| ITHACA-PS-GIR.1 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS103 |
Rocchino-Castrovillari |
ExposureDescription |
|
sequence of cemented conglomerate and alluvium and colluvium deposits |
FaultCode_160117 |
ExposureOrientation |
NE-SW |
|
|
1:6000 |
Cal113 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 3 m; ExposureLength: 13 m |
|
|
|
|
|
|
|
TR |
|
|
|
|
|
|
|
|
It corresponds to F1 Rocchino site Cinti et al.,2015 |
F. Iezzi |
PS103 |
|
|
|
| ITHACA-PS-GIR.2 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS106 |
Torre di Giorgio T3 |
ExposureDescription |
|
alluvial fan deposits |
FaultCode_160100 |
ExposureOrientation |
NE-SW |
|
|
1:90000 |
Cal015 |
|
|
|
|
|
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|
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|
TR |
|
|
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|
|
It corresponds to T3 Torre di Giorgio Cinti et al.,2002 |
F. Iezzi |
PS106 |
|
|
|
| ITHACA-PS-GIR.3 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS107 |
Torre di Giorgio T4 |
ExposureDescription |
|
alluvial fan deposits |
FaultCode_160101 |
ExposureOrientation |
NE-SW |
|
|
1:90000 |
Cal015 |
|
|
|
|
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|
TR |
|
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|
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|
|
It corresponds to T4 Torre di Giorgio Cinti et al.,2002 |
F. Iezzi |
PS107 |
|
|
|
| ITHACA-PS-GIR.4 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS108 |
Masseria Quercia Marina T1 |
ExposureDescription |
|
colluvial deposits |
FaultCode_160615 |
ExposureOrientation |
NE-SW |
|
|
1:90000 |
Cal067 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
|
|
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|
|
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|
TR |
|
|
|
|
|
|
|
|
It corresponds to T1 of Michetti et al.,1997 |
F. Iezzi |
PS108 |
|
|
|
| ITHACA-PS-GIR.5 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS109 |
Masseria Quercia Marina T2 |
ExposureDescription |
|
carbonatic sediments |
FaultCode_160614 |
ExposureOrientation |
NE-SW |
|
|
1:90000 |
Cal067 |
|
|
|
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|
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|
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TR |
|
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|
|
It corresponds to T2 of Michetti et al.,1997 |
F. Iezzi |
PS109 |
|
|
|
| ITHACA-PS-GIR.6 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS105 |
Cava D'Atri |
ExposureDescription |
|
Alluvial fan deposits |
FaultCode_160115 |
|
|
|
|
1:90000 |
Cal114 |
|
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QF |
|
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|
|
It corresponds to Cava D'atri Ferelli et al.,1994 |
F. Iezzi |
PS105 |
|
|
|
| ITHACA-PS-GIR.7 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS110 |
Viggiano |
ExposureDescription |
|
Limestone |
FaultCode_30425 |
ExposureOrientation |
NE-SW |
|
|
1:1 |
Bas043 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
|
|
|
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|
OUT |
|
|
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|
|
|
It corresponds to Viggiano of Giano et al.,2000 |
F. Iezzi |
PS110 |
|
|
|
| ITHACA-PS-GIR.8 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS111 |
Galaino |
ExposureDescription |
|
Paleosoils made of red clay |
FaultCode_30412 |
ExposureOrientation |
NE-SW |
|
|
1:1 |
Bas043 |
|
|
|
|
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|
OUT |
|
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|
|
It correaponds to Galaino of Giano et al.,2000 |
F. Iezzi |
PS111 |
|
|
|
| ITHACA-PS-GIR.9 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS112 |
Pergola |
ExposureDescription |
|
Carbonate gravel, sand, red clay |
FaultCode_31410 |
ExposureOrientation |
NE-SW |
|
|
1:1 |
Bas043 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 12-15 m; ExposureLength: 10 m |
|
|
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|
|
OUT |
|
|
|
|
|
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|
|
It corresponds to Pergola of Giano et al.,2000 |
F. Iezzi |
PS112 |
|
|
|
| ITHACA-PS-GIR.10 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS114 |
Casabianca |
ExposureDescription |
|
fractures and soft terrain,distorsions and horizontal rotations |
FaultCode_36901 |
|
|
|
|
1:1 |
Cal011 |
|
|
|
|
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|
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|
HE |
|
|
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|
|
It Corresponds to Casabianca of Cinti et al., 2015 SRL |
F. Iezzi |
PS114 |
|
|
|
| ITHACA-PS-GIR.11 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS115 |
Parco del cavallo |
ExposureDescription |
|
oriented fractures and horizontal rotation of walls |
FaultCode_36901 |
|
|
|
|
1:1 |
Cal011 |
|
|
|
|
|
|
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|
HE |
|
|
|
|
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|
|
|
it corresponds to Parco del Cavallo of Cinti et al.,2015 SRL |
F. Iezzi |
PS115 |
|
|
|
| ITHACA-PS-GIR.12 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS116 |
Covoni |
ExposureDescription |
|
fine sediments
with small lenses of pebble sized subangular clasts |
FaultCode_30828 |
ExposureOrientation |
NE-SW |
|
|
1:1 |
Bas046 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
TR |
|
|
|
|
|
|
|
|
It corresponds to Covoni of Improta et al.,2010 |
F. Iezzi |
PS116 |
|
|
|
| ITHACA-PS-GIR.13 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS117 |
Trincea |
ExposureDescription |
|
fine colluvial and slope deposits
with fine sized subangular calcareous mudstone clasts |
FaultCode_30828 |
ExposureOrientation |
WNW-ESE |
|
|
|
Bas046 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
TR |
|
|
|
|
|
|
|
|
it corresponds to Trincea of Improta et al.,2010 |
F. Iezzi |
PS117 |
|
|
|
| ITHACA-PS-GIR.14 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS118 |
Timpa del Vento T1 |
ExposureDescription |
|
footwall composed of white powdery cataclasite |
FaultCode_50505 |
ExposureOrientation |
NE-SW |
|
|
1:200.000 |
Cam166 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
TR |
|
|
|
|
|
|
|
|
It corresponds to Trench 1 of Galli et al.,2006 |
F. Iezzi |
PS118 |
|
|
|
| ITHACA-PS-GIR.15 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS119 |
Timpa del Vento T2 |
ExposureDescription |
|
light-grayish clay packed
between the dolomite and the slope succession |
FaultCode_50505 |
ExposureOrientation |
NE-SW |
|
|
1:200.000 |
Cam166 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
TR |
|
|
|
|
|
|
|
|
It corresponds to Trench 2 of Galli et al. (2006). Paleoevents are derived correlating results of Trench 1, Trench 2 and Trench 3 of Galli et al. (2006) |
F. Iezzi |
PS119 |
|
|
|
| ITHACA-PS-GIR.16 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS120 |
Timpa del Vento T3 |
ExposureDescription |
|
alluvial fan deposits |
FaultCode_50505 |
ExposureOrientation |
NE-SW |
|
|
1:200.000 |
Cam166 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
TR |
|
|
|
|
|
|
|
|
It corresponds to Trench 3 of Galli et al.,2006 |
F. Iezzi |
PS120 |
|
|
|
| ITHACA-PS-GIR.17 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS87 |
Patalecchia |
ExposureDescription |
|
Late Pleistocene slope-debris deposits with volcanic tephra layers |
FaultCode_120113 |
ExposureOrientation |
SW-NE |
|
|
1:150.000 |
Cam167 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
OUT |
|
|
|
|
|
|
|
|
It corresponds to PAT-02 of Galli et al. (2017) |
F. Iezzi |
PS87 |
|
|
|
| ITHACA-PS-GIR.18 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS88 |
Hercules sanctuary |
ExposureDescription |
|
Slope deposits |
FaultCode_120148 |
ExposureOrientation |
NNW-SSE |
|
|
1:150.000 |
Cam167 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2 m; ExposureLength: 3 m |
|
|
|
|
|
|
|
(handmade exavation) |
|
|
|
|
C:\Users\franc\OneDrive - Universitàdi Napoli Federico II\PROGETTI PNRR\PNRR GEOSCIENCES\DATABASE PALEOSISMOLOGIA\PROGETTO QGIS\photos_sketches_logs\101120147\2.jpg |
|
|
|
Description of the paleoevents is from Galli and Galadini (2003). The site location is from Fig. 2 of Galli et al. (2017). Evidence of faulting in archeological site. |
F. Iezzi |
PS88 |
|
|
|
| ITHACA-PS-GIR.19 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS89 |
Hercules Sanctuary 2 |
ExposureDescription |
|
Slope deposits |
FaultCode_120148 |
ExposureOrientation |
NNE-SSW |
|
|
1:150.000 |
Cam167 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 3 m; ExposureLength: 8 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\franc\OneDrive - Universitàdi Napoli Federico II\PROGETTI PNRR\PNRR GEOSCIENCES\DATABASE PALEOSISMOLOGIA\PROGETTO QGIS\photos_sketches_logs\102120148\1.jpg |
C:\Users\franc\OneDrive - Universitàdi Napoli Federico II\PROGETTI PNRR\PNRR GEOSCIENCES\DATABASE PALEOSISMOLOGIA\PROGETTO QGIS\photos_sketches_logs\102120148\2.jpg |
|
|
|
it corresponds to T2 of Galli et al. (2017) |
F. Iezzi |
PS89 |
|
|
|
| ITHACA-PS-GIR.20 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS90 |
Aquae Iuliae fault T3 |
ExposureDescription |
|
Colluvial and slope deposits |
FaultCode_50100 |
ExposureOrientation |
NE-SW |
|
|
1:110.000 |
Mol019 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 4 m; ExposureLength: 8 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\franc\OneDrive - Universitàdi Napoli Federico II\PROGETTI PNRR\PNRR GEOSCIENCES\DATABASE PALEOSISMOLOGIA\PROGETTO QGIS\photos_sketches_logs\10350100\1.jpg |
C:\Users\franc\OneDrive - Universitàdi Napoli Federico II\PROGETTI PNRR\PNRR GEOSCIENCES\DATABASE PALEOSISMOLOGIA\PROGETTO QGIS\photos_sketches_logs\10350100\2.jpg |
|
|
|
It corresponds to Trench 1 of Galli and Naso (2009) |
F. Iezzi |
PS90 |
|
|
|
| ITHACA-PS-GIR.21 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS91 |
Aquae Iuliae fault T2 |
ExposureDescription |
|
Colluvial and slope deposits |
FaultCode_50102 |
ExposureOrientation |
NE-SW |
|
|
1:110.000 |
Mol019 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2 m; ExposureLength: 4 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\franc\OneDrive - Universitàdi Napoli Federico II\PROGETTI PNRR\PNRR GEOSCIENCES\DATABASE PALEOSISMOLOGIA\PROGETTO QGIS\photos_sketches_logs\10450100\1.jpg |
|
|
|
|
It corresponds to Trench 2 of Galli and Naso (2009). |
F. Iezzi |
PS91 |
|
|
|
| ITHACA-PS-GIR.22 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS92 |
Aquae Iuliae fault T1 |
ExposureDescription |
|
Colluvial and slope deposits |
FaultCode_50102 |
ExposureOrientation |
NE-SW |
|
|
1:110.000 |
Mol019 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2 m; ExposureLength: 3 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\franc\OneDrive - Universitàdi Napoli Federico II\PROGETTI PNRR\PNRR GEOSCIENCES\DATABASE PALEOSISMOLOGIA\PROGETTO QGIS\photos_sketches_logs\10550100\1.jpg |
C:\Users\franc\OneDrive - Universitàdi Napoli Federico II\PROGETTI PNRR\PNRR GEOSCIENCES\DATABASE PALEOSISMOLOGIA\PROGETTO QGIS\photos_sketches_logs\10550100\2.jpg |
|
|
|
It corresponds to Trench 3 of Galli and Naso (2009) |
F. Iezzi |
PS92 |
|
|
|
| ITHACA-PS-GIR.23 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS93 |
S. Angelo Alife |
ExposureDescription |
|
Slope deposits with volcanic tuffs |
FaultCode_52808 |
ExposureOrientation |
NNE-SSW |
|
|
1:1 |
Cam057 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 1 m; ExposureLength: 3 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\franc\OneDrive - Universitàdi Napoli Federico II\PROGETTI PNRR\PNRR GEOSCIENCES\DATABASE PALEOSISMOLOGIA\PROGETTO QGIS\photos_sketches_logs\10652808\1.jpg |
|
|
|
|
|
F. Iezzi |
PS93 |
|
|
|
| ITHACA-PS-GIR.24 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS94 |
Gioia Sannitica FZ1 |
ExposureDescription |
|
Alluvial and colluvial deposits |
FaultCode_52814 |
ExposureOrientation |
NE-SW |
|
|
1:1 |
Cam057 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
ROC |
|
|
|
C:\Users\franc\OneDrive - Universitàdi Napoli Federico II\PROGETTI PNRR\PNRR GEOSCIENCES\DATABASE PALEOSISMOLOGIA\PROGETTO QGIS\photos_sketches_logs\10752814\1.jpg |
|
|
|
|
|
F. Iezzi |
PS94 |
|
|
|
| ITHACA-PS-GIR.25 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS95 |
Gioia Sannitica FZ2 |
ExposureDescription |
|
Alluvial and colluvial deposits |
FaultCode_52814 |
ExposureOrientation |
NE-SW |
|
|
1:1 |
Cam057 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
ROC |
|
|
|
C:\Users\franc\OneDrive - Universitàdi Napoli Federico II\PROGETTI PNRR\PNRR GEOSCIENCES\DATABASE PALEOSISMOLOGIA\PROGETTO QGIS\photos_sketches_logs\10852814\1.jpg |
|
|
|
|
|
F.Iezzi |
PS95 |
|
|
|
| ITHACA-PS-GIR.26 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS96 |
Monte Ramatico-Castelpagno T7 |
ExposureDescription |
|
Stone masonry |
FaultCode_51401 |
ExposureOrientation |
NE-SW |
|
|
1:285.000 |
Cam164 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
TR |
|
|
|
|
C:\Users\franc\OneDrive - Universitàdi Napoli Federico II\PROGETTI PNRR\PNRR GEOSCIENCES\DATABASE PALEOSISMOLOGIA\PROGETTO QGIS\photos_sketches_logs\10951401\2.jpg |
|
|
|
faulting of a wall |
F. Iezzi |
PS96 |
|
|
|
| ITHACA-PS-GIR.27 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS97 |
Monte Oppido T6 |
ExposureDescription |
|
Slope deposits |
FaultCode_51403 |
ExposureOrientation |
NE-SW |
|
|
1:285.000 |
Cam164 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\franc\OneDrive - Universitàdi Napoli Federico II\PROGETTI PNRR\PNRR GEOSCIENCES\DATABASE PALEOSISMOLOGIA\PROGETTO QGIS\photos_sketches_logs\11051403\1.jpg |
|
|
|
|
|
F. Iezzi |
PS97 |
|
|
|
| ITHACA-PS-GIR.28 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS101 |
Monte Cucuzzone-San GregorioT5 |
ExposureDescription |
|
Slope deposits |
FaultCode_51515 |
ExposureOrientation |
NE-SW |
|
|
1:285.000 |
Cam164 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\franc\OneDrive - Universitàdi Napoli Federico II\PROGETTI PNRR\PNRR GEOSCIENCES\DATABASE PALEOSISMOLOGIA\PROGETTO QGIS\photos_sketches_logs\11451515\1.jpg |
|
|
|
|
|
F. Iezzi |
PS101 |
|
|
|
| ITHACA-PS-GIR.29 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS99 |
Monte delle Rose-Sette Cuponi T3 |
ExposureDescription |
|
Slope deposits |
FaultCode_51502 |
ExposureOrientation |
NE-SW |
|
|
1:285.000 |
Cam164 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\franc\OneDrive - Universitàdi Napoli Federico II\PROGETTI PNRR\PNRR GEOSCIENCES\DATABASE PALEOSISMOLOGIA\PROGETTO QGIS\photos_sketches_logs\11251502\1.jpg |
|
|
|
|
|
F. Iezzi |
PS99 |
|
|
|
| ITHACA-PS-GIR.30 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS100 |
Serra del Dardano–Piano il Parco T4 |
ExposureDescription |
|
Slope deposits |
FaultCode_51512 |
ExposureOrientation |
NE-SW |
|
|
1:285.000 |
Cam164 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2 m; ExposureLength: 4 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\franc\OneDrive - Universitàdi Napoli Federico II\PROGETTI PNRR\PNRR GEOSCIENCES\DATABASE PALEOSISMOLOGIA\PROGETTO QGIS\photos_sketches_logs\11351512\1.jpg |
|
|
|
|
|
F. Iezzi |
PS100 |
|
|
|
| ITHACA-PS-GIR.31 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS102 |
Piano di Pecore |
ExposureDescription |
|
sequence of lacustrine and colluvial deposits. Volcanic pumice, sand, and ash are commonly the main components of sediments. |
FaultCode_51503 |
ExposureOrientation |
N-S |
|
|
1:1 |
Cam225 |
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|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 4 m; ExposureLength: 33 m |
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TR |
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|
C:\Users\franc\OneDrive - Universitàdi Napoli Federico II\PROGETTI PNRR\PNRR GEOSCIENCES\DATABASE PALEOSISMOLOGIA\PROGETTO QGIS\photos_sketches_logs\11551503\1.jpg |
C:\Users\franc\OneDrive - Universitàdi Napoli Federico II\PROGETTI PNRR\PNRR GEOSCIENCES\DATABASE PALEOSISMOLOGIA\PROGETTO QGIS\photos_sketches_logs\11551503\2.jpg |
|
|
|
It corresponds to Trench 1 of Pantosti et al. (1993) |
F. Iezzi |
PS102 |
|
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|
| ITHACA-PS-GIR.32 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS104 |
Fonte Bellusci |
ExposureDescription |
|
Sequence of fan-delta, lacustrine, alluvial deposits
and paleosols |
FaultCode_160118 |
ExposureOrientation |
NW-SE |
|
|
1:90000 |
Cal012 |
|
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|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
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TR |
|
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|
It corresponds to T2 Fonte Bellusci Cinti et al.,2002 |
F. Iezzi |
PS104 |
|
|
|
| ITHACA-PS-GIR.33 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS113 |
S.Angelo |
ExposureDescription |
|
alluvial fan deposits |
FaultCode_53308 |
|
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|
1:1 |
Cam262 |
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QF |
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|
It corresponds to Villani et al.,2010 |
F. Iezzi |
PS113 |
|
|
|
| ITHACA-PS-GIR.34 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS37 |
Egna |
ExposureDescription |
|
alternation of alluvial fan deposits and alluvial plains deposits, on which a Roma building was built. |
FaultCode_100605 |
|
|
|
|
1:100.000 |
Taa014 |
|
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|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
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TR |
|
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|
It corresponds to the seven trenches described in Galadini and Galli (1999) |
D.Maceroni |
PS37 |
|
|
|
| ITHACA-PS-GIR.35 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS45 |
Moscarello |
ExposureDescription |
|
Alluvial fan deposits, unconsolidated sandy conglomerate, colluvial deposits |
FaultCode_11700 |
ExposureOrientation |
W-E |
|
|
1:16.500 |
sicilia002 |
|
|
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|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 7-8 m; ExposureLength: 15 m |
|
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|
|
TR |
|
|
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|
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|
|
It corresponds to Trench A of Azzaro et al. (2000) |
D.Maceroni |
PS45 |
|
|
|
| ITHACA-PS-GIR.36 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS46 |
Piana di Campoli 3 |
ExposureDescription |
|
Alternating coarse alluvial and mainly fine colluvial deposits and paleosols, which overlie bedrock. |
FaultCode_20711 |
ExposureOrientation |
NNE-SSW |
|
|
1:150.000 |
Abz027 |
|
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|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 4 m; ExposureLength: 10 m |
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TR |
|
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|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\4620711\1.jpg |
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|
D.Maceroni |
PS46 |
|
|
|
| ITHACA-PS-GIR.37 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS48 |
Campotosto |
ExposureDescription |
|
Succession of colluvial, alluvial and debris deposits |
FaultCode_22000 |
ExposureOrientation |
WSW-ENE |
|
|
1:30.000 |
Ita638 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2,5 m; ExposureLength: 32 m |
|
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|
TR |
|
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|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\4822000\1.jpg |
|
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|
It corresponds to the site 3 of Galadini and Galli (2003). The site location refers to Fig. 3 of Galadini and Galli (2003). |
D. Maceroni |
PS48 |
|
|
|
| ITHACA-PS-GIR.38 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS49 |
Pescasseroli |
|
|
|
FaultCode_22405 |
|
|
|
|
1:50.000 |
Abz015 |
|
|
|
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|
TR |
|
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|
It corresponds to point P of Galadini et al. (1998), where the contact between Flysch and alluvial deposits was detected. |
D. Maceroni |
PS49 |
|
|
|
| ITHACA-PS-GIR.39 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS54 |
Piano di Castelluccio |
ExposureDescription |
|
Succession of alluvial and colluvial deposits |
FaultCode_141207 |
ExposureOrientation |
NE-SW |
|
|
1:25.000 |
Ita638 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 1-1,5 m; ExposureLength: 5 m |
|
|
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|
|
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|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\5423829\1.jpg |
|
|
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|
Midpoint between trenches 1, 2 and 3. The location of the site refers to Fig.4 of Galadini and Galli (2003). |
D. Maceroni |
PS54 |
|
|
|
| ITHACA-PS-GIR.40 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS55 |
Campo Imperatore-Monte Mutri |
ExposureDescription |
|
Sequence of alluvial and colluvial deposits |
FaultCode_25315 |
ExposureOrientation |
NNE-SSW |
|
|
1:60.000 |
Abz016 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2 m; ExposureLength: 10 m |
|
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|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\5525315\1.jpg |
|
|
|
|
It corresponds to Trench 3 and 4 of Galli et al. (2002). The site location refers to Fig. 2 of Galli et al. (2002) Necessita di aggiungere nuove faglie per match |
D. Maceroni |
PS55 |
|
|
|
| ITHACA-PS-GIR.41 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS56 |
Campo Imperatore-Monte Mutri |
ExposureDescription |
|
Sequence of alluvial and colluvial deposits |
FaultCode_25316 |
ExposureOrientation |
NNE-SSW |
|
|
1:60.000 |
Abz016 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2 m; ExposureLength: 6 m |
|
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|
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|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\5625316\1.jpg |
|
|
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|
It corresponds to Trench 2 of Galli et al. (2002). The site location refers to Fig. 2 of Galli et al. (2002) Necessit? di aggiungere nuove faglie per match |
D. Maceroni |
PS56 |
|
|
|
| ITHACA-PS-GIR.42 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS38 |
La Casetta |
|
|
|
FaultCode_21010 |
|
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|
|
1:200.000 |
Laz041 |
|
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TR |
|
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|
D. Maceroni |
PS38 |
|
|
|
| ITHACA-PS-GIR.43 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS39 |
Pie di Colle |
|
|
|
FaultCode_21006 |
|
|
|
|
1:200.000 |
Laz041 |
|
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TR |
|
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|
D. Maceroni |
PS39 |
|
|
|
| ITHACA-PS-GIR.44 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS40 |
Caporio |
|
|
|
FaultCode_21002 |
|
|
|
|
1:200.000 |
Laz041 |
|
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TR |
|
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|
D. Maceroni |
PS40 |
|
|
|
| ITHACA-PS-GIR.45 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS44 |
Sant'Angelo ruderi |
ExposureDescription |
|
Surface faulting in alluvial-colluvial deposits |
FaultCode_20024 |
ExposureOrientation |
NW-SE |
|
|
1:25.000 |
Ita636 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 4 m; ExposureLength: 8 m |
|
|
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|
|
|
|
QF |
|
|
|
|
|
|
|
|
Occurrence of repeated surface faulting during the Late Pleistocene and particularly one event with about Ms 6.9, that occurred about 29.690 yr ago |
D. Maceroni |
PS44 |
|
|
|
| ITHACA-PS-GIR.46 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS47 |
Norcia site |
ExposureDescription |
|
Slickenside juxtaposes Middle Pleistocene alluvial fan pebbles against Upper Pleistocene to Holocene colluvial deposits |
FaultCode_141913 |
ExposureOrientation |
NE-SW |
|
|
1:110.000 |
Ita636 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2 m; ExposureLength: 5 m |
|
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|
QF |
|
|
|
|
|
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|
|
Coseismic ground effects documented that occurred during 1703 and 1979 Norcia earthquakes. The site location refers to Fig.4 of Blumetti (1995). |
D. Maceroni |
PS47 |
|
|
|
| ITHACA-PS-GIR.47 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS51 |
Piano Aremogna 1 |
ExposureDescription |
|
The stratigraphy exposed includes paleosols and alluvial fan deposits gently dipping towards the plain and capping fluvioglacial fan deposits. |
FaultCode_23402 |
ExposureOrientation |
E-W |
|
|
1:50.000 |
Abz011 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2.5 m; ExposureLength: 50 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\5123402\1.jpg |
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\5123402\2.jpg |
|
|
|
It corresponds to Trench 1 of D'Addezio et al. (2001). The site location refers to Figure 4 of the paper. |
D. Maceroni |
PS51 |
|
|
|
| ITHACA-PS-GIR.48 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS52 |
Cinque Miglia |
ExposureDescription |
|
Sequence of fluvioglacial fan, paleosol and alluvial sediments. |
FaultCode_23404 |
ExposureOrientation |
NE-SW |
|
|
1:50.000 |
Abz011 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 3.5 m; ExposureLength: 10 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\5223404\1.jpg |
|
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|
|
It corresponds to Trench 3 of D'Addezio et al. (2001). The site location refers to Figure 3 of the paper. |
D. Maceroni |
PS52 |
|
|
|
| ITHACA-PS-GIR.49 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS53 |
Rivisondoli |
|
|
|
FaultCode_23400 |
|
|
|
|
1:1 |
Abz029 |
|
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|
|
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|
OUT |
|
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|
D. Maceroni |
PS53 |
|
|
|
| ITHACA-PS-GIR.50 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS57 |
Pantano San Gregorio |
ExposureDescription |
|
sequence of lacustrine and colluvial deposits, partly resulting from remobilization and volcanites |
FaultCode_51522 |
ExposureOrientation |
NE-SW |
|
|
1:50.000 |
Cam129 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 5-6m; ExposureLength: 30m |
|
|
|
|
|
|
|
TR |
|
|
|
|
|
|
|
|
It corresponds to Trench 3 and 4 of D'Addezio et al. (1991) |
D. Maceroni |
PS57 |
|
|
|
| ITHACA-PS-GIR.51 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS41 |
Valle del Venacquaro nord |
ExposureDescription |
|
Succession of till, alluvial fan and alluvial-colluvial-palustrine deposits. |
FaultCode_25201 |
ExposureOrientation |
N-S |
|
|
1:10.000 |
Abz019 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 3 m; ExposureLength: 5 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\4125201\1.jpg |
|
|
|
|
The site location refers to Fig. 4 of Giraudi and Frezzotti (1995). The authors stated that the fault plane was not reached for excavation safety reasons. Therefore, the several paleoevents for this site are not available. |
D. Maceroni |
PS41 |
|
|
|
| ITHACA-PS-GIR.52 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS42 |
Valle del Venacquaro sud |
ExposureDescription |
|
Succession of till, alluvial fan and alluvial-colluvial-palustrine deposits. |
FaultCode_25202 |
ExposureOrientation |
NNE-SSW |
|
|
1:10.000 |
Abz019 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 3 m; ExposureLength: 10 m |
|
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|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\4225202\1.jpg |
|
|
|
|
The site location refers to Fig. 4 of Giraudi and Frezzotti (1995). |
D. Maceroni |
PS42 |
|
|
|
| ITHACA-PS-GIR.53 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS43 |
Val Maone |
ExposureDescription |
|
Fault scarps that affect postglacial valley bottom sediments and linked to faults that dislocate the carbonate bedrock. |
FaultCode_25206 |
|
|
|
|
1:10.000 |
Abz019 |
|
|
|
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|
|
|
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|
OUT |
|
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|
In this site three fault activity phases are identified. The cronological constraints, based on morpho-litho-stratigraphic consideration, appear very similar to 41 and 42 paleosites located in Venaquaro valley. |
D. Maceroni |
PS43 |
|
|
|
| ITHACA-PS-GIR.54 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS04 |
SS Marsicana |
ExposureDescription |
|
lacustrine deposits, colluvial sediments, erosion surfaces |
FaultCode_20503 |
ExposureOrientation |
NE-SW |
|
|
1:165.000 |
Abz012 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 3 m; ExposureLength: ND |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\420503\1.jpg |
|
|
|
|
It corresponds to the site 1 of Galadini and Galli (1999). The site location refers to Fig. 2 of Galadini and Galli (1999). |
D. Maceroni |
PS04 |
|
|
|
| ITHACA-PS-GIR.55 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS05 |
Colle delle Cerese |
ExposureDescription |
|
lacustrine-coastline sediments and slope-colluvial deposits |
FaultCode_25507 |
ExposureOrientation |
NE-SW |
|
|
1:165.000 |
Abz012 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 6,5 m; ExposureLength: 10 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\525507\1.jpg |
|
|
|
|
It corresponds to the site 3 of Galadini and Galli (1999) and to the site 2 of Galadini et al. (1997). The site location refers to Fig. 1 of Galli et al. (2016). |
D. Maceroni |
PS05 |
|
|
|
| ITHACA-PS-GIR.56 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS06 |
Colle Cerese Cave |
ExposureDescription |
|
lacustrine sediments |
FaultCode_25507 |
ExposureOrientation |
NE-SW |
|
|
1:165.000 |
Abz012 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2 m; ExposureLength: 3 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\625507\1.jpg |
|
|
|
|
It corresponds to the site 4 of Galadini and Galli (1999) and to the site 3 of Galadini et al. (1997). The site location refers to Fig. 1 of Galli et al. (2016). |
D. Maceroni |
PS06 |
|
|
|
| ITHACA-PS-GIR.57 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS07 |
Molini di Venere |
ExposureDescription |
|
lacustrine sediments |
FaultCode_20401 |
ExposureOrientation |
NE-SW |
|
|
1:165.000 |
Abz012 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 4 m; ExposureLength: 13 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\720401\1.jpg |
|
|
|
|
It corresponds to the site 5 of Galadini and Galli (1999). The site location refers to Fig. 1 of Galli et al. (2016). |
D. Maceroni |
PS07 |
|
|
|
| ITHACA-PS-GIR.58 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS08 |
Casali D'Aschi |
ExposureDescription |
|
sequence of slope-colluvial deposits, limestone breccias, carbonate bedrock |
FaultCode_20401 |
ExposureOrientation |
NE-SW |
|
|
1:165.000 |
Abz012 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 20 m; ExposureLength: 40 m |
|
|
|
|
|
|
|
QF |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\820401\1.jpg |
|
|
|
|
It corresponds to the site 6 of Galadini and Galli (1999) and to the site 5 of Galadini et al. (1997). The site location refers to Fig. 2 of Galadini and Galli (1999). |
D. Maceroni |
PS08 |
|
|
|
| ITHACA-PS-GIR.59 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS09 |
Trasacco Strada 37 |
ExposureDescription |
|
lacustrine deposits |
FaultCode_22200 |
ExposureOrientation |
NE-SW |
|
|
1:50.000 |
Abz012 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 4 m; ExposureLength: 5 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\922200\1.jpg |
|
|
|
|
It corresponds to the 8 of Galadini and Galli (1999) and to the site 7 of Galadini et al. (1997).The site location refers to Fig. 3 of Galadini and Galli (1999) |
D. Maceroni |
PS09 |
|
|
|
| ITHACA-PS-GIR.60 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS12 |
Trasacco Fosso 41 |
ExposureDescription |
|
lacustrine deposits |
FaultCode_22200 |
ExposureOrientation |
NE-SW |
|
|
1:50.000 |
Abz012 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 3 m; ExposureLength: 3 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\1222200\1.jpg |
|
|
|
|
it corresponds to the site 7 of Galadini and Galli (1999) and to the site 6 of Galadini et al. (1997). The site location refers to Fig. 3 of Galadini and Galli (1999) |
D. Maceroni |
PS12 |
|
|
|
| ITHACA-PS-GIR.61 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS13 |
Trasacco Strada 38 |
ExposureDescription |
|
lacustrine deposits, vulcanic levels, surface faulting |
FaultCode_22200 |
ExposureOrientation |
NE-SW |
|
|
1:50.000 |
Abz012 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 3 m; ExposureLength: ND |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\1322200\1.jpg |
|
|
|
|
It corresponds to the site 9 of Galadini and Galli (1999) and to the site 8 of Galadini et al. (1997). The site location refers to Fig. 3 of Galadini and Galli (1999) |
D. Maceroni |
PS13 |
|
|
|
| ITHACA-PS-GIR.62 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS14 |
Trasacco Strada 10 |
ExposureDescription |
|
lacustrine deposits, vulcanic levels |
FaultCode_22200 |
ExposureOrientation |
NE-SW |
|
|
1:50.000 |
Abz012 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: ND; ExposureLength: ND |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\1422200\1.jpg |
|
|
|
|
It corresponds to the site 11 of Galadini and Galli (1999) end to the site 9 of Galadini et al. (1997). The site location refers to Fig. 3 of Galadini and Galli (1999). |
D. Maceroni |
PS14 |
|
|
|
| ITHACA-PS-GIR.63 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS15 |
Luco Strada 42 |
ExposureDescription |
|
Series of 3 m deep soundings exposing a sedimentary sequence characterized by lacustrine deposits (Complex 1 and Complex 4). Dislocation of historical ground surface of about 0.10 m related to 1915 surface faulting event. |
FaultCode_20200 |
ExposureOrientation |
ND |
|
|
1:165.000 |
Abz012 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: ND; ExposureLength: ND |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\1520200\1.jpg |
|
|
|
|
It corresponds to the site 12 Galadini and Galli (1999) and to the site 10 of Galadini et al. (1997). The site location refers to Fig. 1 of Galli et al. (2016). |
D. Maceroni |
PS15 |
|
|
|
| ITHACA-PS-GIR.64 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS16 |
Luco Strada 45 |
ExposureDescription |
|
colluvial and shore lacustrine deposits |
FaultCode_20200 |
ExposureOrientation |
E-W |
|
|
1:165.000 |
Abz012 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2,5 m; ExposureLength: 8,5 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\1620200\1.jpg |
|
|
|
|
It corresponds to the site 13 of Galadini and Galli (1999) and to the 11 of Galadini et al. (1997). The site location refers to Fig. 1 of Galli et al. (2016). |
D. Maceroni |
PS16 |
|
|
|
| ITHACA-PS-GIR.65 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS17 |
San Benedetto 1 |
ExposureDescription |
|
Succession of latest Pleistocene to historical fluvio-lacustrine deposits |
FaultCode_20401 |
ExposureOrientation |
NE-SW |
|
|
1:16.000 |
Abz024 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 3 m; ExposureLength: 20 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\1720401\1.jpg |
|
|
|
|
It corresponds to Trench 1 of Michetti et al. (1996). The site location refers to Fig. 4 of Michetti et al. (1996). |
D. Maceroni |
PS17 |
|
|
|
| ITHACA-PS-GIR.66 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS18 |
Piano di Pezza |
ExposureDescription |
|
Sedimentary sequence formed mainly of paleosols and alluvial fan graveldipping gently toward the plain |
FaultCode_20300 |
ExposureOrientation |
NE-SW |
|
|
1:25.000 |
Abz026 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 3 m; ExposureLength: 11 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\1820300\1.jpg |
|
|
|
|
It corresponds to Trench 1 of Pantosti et al. (1996). The site location refers to Fig. 2 of Pantosti et al. (1996) |
D. Maceroni |
PS18 |
|
|
|
| ITHACA-PS-GIR.67 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS19 |
Vado di Pezza |
ExposureDescription |
|
Sequence of lacustrine deposits interbedded with sand, gravel, paleosols and slope deposits |
FaultCode_20300 |
ExposureOrientation |
NE-SW |
|
|
1:25.000 |
Abz026 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 4 m; ExposureLength: 30 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\1920300\1.jpg |
|
|
|
|
It corresponds to Trench 3 of Pantosti et al. (1996). The site location refers to Fig. 2 of Pantosti et al. (1996). |
D. Maceroni |
PS19 |
|
|
|
| ITHACA-PS-GIR.68 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS20 |
Campo Porcaro |
ExposureDescription |
|
Stratigraphic sequence of last deglaciation slope and alluvial deposits and paleosoil |
FaultCode_20300 |
ExposureOrientation |
NE-SW |
|
|
1:2.500 |
Abz026 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
TR |
|
|
|
|
|
|
|
|
It corresponds to Trench 4 of Pantosti et al. (1996). The site location refers to Fig. 5 of Pantosti et al. (1996) |
D. Maceroni |
PS20 |
|
|
|
| ITHACA-PS-GIR.69 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS21 |
Trasacco Roman |
ExposureDescription |
|
lacustrine deposits |
FaultCode_22200 |
ExposureOrientation |
NE-SW |
|
|
1:50.000 |
Abz012 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: ND; ExposureLength: ND |
|
|
|
|
|
|
|
TR |
|
|
|
|
|
|
|
|
It corresponds to site 10 of Galadini and Galli (1999). The site location refers to Fig. 3 of Galadini and Galli (1999). |
D. Maceroni |
PS21 |
|
|
|
| ITHACA-PS-GIR.70 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS22 |
SS Marsicana-Celano |
ExposureDescription |
|
lacustrine deposits, colluvial sediments, erosion surfaces |
FaultCode_20500 |
ExposureOrientation |
ND |
|
|
1:165.000 |
Abz012 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: ND; ExposureLength: ND |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\2220500\1.jpg |
|
|
|
|
It corresponds to the site 2 of Galadini and Galli (1999). The site location refers to Fig. 2 of Galadini and Galli (1999). |
D. Maceroni |
PS22 |
|
|
|
| ITHACA-PS-GIR.71 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS23 |
Bacinetto |
ExposureDescription |
|
Surface faulting during 1915 earthquake. |
FaultCode_25402 |
ExposureOrientation |
ND |
|
|
1:165.000 |
Abz012 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: ND; ExposureLength: ND |
|
|
|
|
|
|
|
TR |
|
|
|
|
|
|
|
|
It corresponds to site 14 in Galadini and Galli (1999), but its description is not provided in the paper. The site location refers to Fig. 2 of Galadini and Galli (1999) |
D. Maceroni |
PS23 |
|
|
|
| ITHACA-PS-GIR.72 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS24 |
Pescina-fotovoltaico |
ExposureDescription |
|
Sequence of white-grey lacustrine clayey silt, colluvial and alluvial deposits containing abundant archaeological remains. |
FaultCode_20500 |
ExposureOrientation |
NE-SW |
|
|
1:10.000 |
Abz020 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 1,5 - 2 m; ExposureLength: 2 - 5 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\2420500\1.jpg |
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\2420500\2.jpg |
|
|
|
It corresponds to trenches (1 to 5) of Gori et al. (2017), drugged along a synthetic splay of the faul 20500. The site location refers to Fig. 4 of Gori et al. (2017) |
D. Maceroni |
PS24 |
|
|
|
| ITHACA-PS-GIR.73 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS25 |
Cava di Venere 2 |
ExposureDescription |
|
Tectonic contact between carbonate bedrock and latest quaternary slope deposits and recent colluvial units. |
FaultCode_20401 |
ExposureOrientation |
NNE-SSW |
|
|
1:50.000 |
Abz023 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 3 m; ExposureLength: 10 m |
|
|
|
|
|
|
|
QF |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\2520401\1.jpg |
|
|
|
|
It corresponds to the site 2 of Saroli et al. (2008). The site location refers to Fig. 2 of Saroli et al. (2008) |
D. Maceroni |
PS25 |
|
|
|
| ITHACA-PS-GIR.74 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS36 |
Cava di Venere 1 |
ExposureDescription |
|
Tectonic contact between carbonate bedrock and latest quaternary alluvial-lacustrine and colluvial deposits. |
FaultCode_20401 |
ExposureOrientation |
NE-SW |
|
|
1:50.000 |
Abz023 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 8 m; ExposureLength: 10 m |
|
|
|
|
|
|
|
QF |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\3620401\1.jpg |
|
|
|
|
It corresponds to the site 1 of Saroli et al. (2008). The site location refers to Fig. 2 of Saroli et al. (2008) |
D. Maceroni |
PS36 |
|
|
|
| ITHACA-PS-GIR.75 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS26 |
Forme |
ExposureDescription |
|
Sequence of slope deposits cut by the fault |
FaultCode_20600 |
ExposureOrientation |
NNE-SSW |
|
|
1:80.000 |
Abz018 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2,5 m; ExposureLength: 3 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\2620600\1.jpg |
|
|
|
|
The site location refers to Fig. 5 of Galli et al. (2012). |
D. Maceroni |
PS26 |
|
|
|
| ITHACA-PS-GIR.76 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS27 |
Molini di Venere 1 |
ExposureDescription |
|
post Latest Glacial Maximum lacustrine deposits cut by the fault |
FaultCode_20401 |
ExposureOrientation |
NE-SW |
|
|
1:1 |
Abz017 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 3 m; ExposureLength: 10 |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\2720401\1.jpg |
|
|
|
|
Geographic coordinates provided in Galli et al. (2016). |
D. Maceroni |
PS27 |
|
|
|
| ITHACA-PS-GIR.77 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS28 |
San Benedetto |
ExposureDescription |
|
Sequence of fluvio-lacustrine deposits |
FaultCode_20401 |
ExposureOrientation |
NE-SW |
|
|
1:500.000 |
Abz029 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 4 m; ExposureLength: 24 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\2820401\1.jpg |
|
|
|
|
It corresponds to one of 3 trenches, drugged by Brunamonte et al. (1991). Only one site was located, because the authors reports only a summary diagram of the observations and not specific logs of 3 trenches. The site location refers to Fig. 1. |
D. Maceroni |
PS28 |
|
|
|
| ITHACA-PS-GIR.78 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS29 |
Paganica TA |
ExposureDescription |
|
continental units, roman cultural unit, surface faulting events |
FaultCode_20087 |
ExposureOrientation |
NE-SW |
|
|
1:10.000 |
Abz025 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
|
|
|
|
|
|
|
|
TR |
|
|
|
|
|
|
|
|
|
D. Maceroni |
PS29 |
|
|
|
| ITHACA-PS-GIR.79 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS30 |
Paganica TB |
ExposureDescription |
|
continental units, surface faulting events |
FaultCode_20087 |
ExposureOrientation |
NE-SW |
|
|
1:10.000 |
Abz025 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
|
|
|
|
|
|
|
|
TR |
|
|
|
|
|
|
|
|
|
D. Maceroni |
PS30 |
|
|
|
| ITHACA-PS-GIR.80 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS31 |
Paganica TC |
ExposureDescription |
|
continental units, antithetic fault, surface faulting event |
FaultCode_20087 |
ExposureOrientation |
NE-SW |
|
|
1:10.000 |
Abz025 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
|
|
|
|
|
|
|
|
TR |
|
|
|
|
|
|
|
|
|
D. Maceroni |
PS31 |
|
|
|
| ITHACA-PS-GIR.81 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS32 |
Bagno Piccolo |
ExposureDescription |
|
deformed miocenic bedrock, slope deposits, anthropic unit |
FaultCode_20095 |
ExposureOrientation |
WNW-ESE |
|
|
1:1 |
Abz022 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2 m; ExposureLength: 2 - 3 m |
|
|
|
|
|
|
|
OUT |
|
|
|
|
|
|
|
|
|
D.Maceroni |
PS32 |
|
|
|
| ITHACA-PS-GIR.82 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS33 |
Le Chieie |
ExposureDescription |
|
deformed carbonate bedrock, colluvial deposits |
FaultCode_27100 |
ExposureOrientation |
ESE-WNW |
|
|
1:1 |
Abz021 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 1 m; ExposureLength: 3 m |
|
|
|
|
|
|
|
HE |
|
|
|
|
|
|
|
|
|
D. Maceroni |
PS33 |
|
|
|
| ITHACA-PS-GIR.83 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS34 |
Grotta di San Bartolomeo |
ExposureDescription |
|
deformed carbonate bedrock, colluvial deposits |
FaultCode_27101 |
ExposureOrientation |
NE-SW |
|
|
1:1 |
Abz021 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 3 m; ExposureLength: 3-4 m |
|
|
|
|
|
|
|
HE |
|
|
|
|
|
|
|
|
|
D.Maceroni |
PS34 |
|
|
|
| ITHACA-PS-GIR.84 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS35 |
San Benedetto 2 |
ExposureDescription |
|
Succession of latest Pleistocene to historical fluvio-lacustrine deposits |
FaultCode_20401 |
ExposureOrientation |
NE-SW |
|
|
1:16.000 |
Abz024 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 3 m; ExposureLength: 20 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\3520401\1.jpg |
|
|
|
|
It corresponds to Trench 2 of Michetti et al. (1996). The site location refers to Fig. 4 of Michetti et al. (1996). |
D. Maceroni |
PS35 |
|
|
|
| ITHACA-PS-GIR.85 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS10 |
Campo Porcaro antithetic |
ExposureDescription |
|
Stratigraphic sequence composed of late deglaciation and alluvium deposits and paleosoil |
FaultCode_20300 |
ExposureOrientation |
NE-SW |
|
|
1:2.500 |
Abz026 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2 m; ExposureLength: 14 m |
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|
|
TR |
|
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|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\1020300\1.jpg |
|
|
|
|
It corresponds to Trench 7 of Pantosti et al. (1996). The site location refers to Fig. 5 of Pantosti et al. (1996) |
D. Maceroni |
PS10 |
|
|
|
| ITHACA-PS-GIR.86 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS11 |
Piano di Pezza antithetic |
ExposureDescription |
|
Stratigraphic sequence composed of outwash, alluvial fan gravel and paleosol that can be correlated to those of Trench 1 |
FaultCode_20300 |
ExposureOrientation |
NE-SW |
|
|
1:25.000 |
Abz026 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 4 m; ExposureLength: 12 m |
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|
TR |
|
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|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA\PNRR Geosciences\Photos_Sketches_Log\1120300\1.jpg |
|
|
|
|
It corresponds to Trench 2 of Pantosti et al. (1996). The site location refers to Fig. 2 of Pantosti et al. (1996) |
D. Maceroni |
PS11 |
|
|
|
| ITHACA-PS-GIR.87 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS59 |
Piana di Campoli 1 |
ExposureDescription |
|
Alternating coarse alluvial and mainly fine colluvial deposits and paleosols, which overlie bedrock. |
FaultCode_20711 |
ExposureOrientation |
NE-SW |
|
|
1:150.000 |
Abz027 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 3 m; ExposureLength: 15 m |
|
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|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\5920711\1.jpg |
|
|
|
|
It corresponds to the Trench A of Salvi et al. (2003). The site location referes to the Figure 2 of the paper |
D.Maceroni |
PS59 |
|
|
|
| ITHACA-PS-GIR.88 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS60 |
Piana di Campoli 2 |
ExposureDescription |
|
Alternating coarse alluvial and mainly fine colluvial deposits and paleosols, which overlie bedrock. |
FaultCode_20711 |
ExposureOrientation |
NE-SW |
|
|
1:150.000 |
Abz027 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 5 m; ExposureLength: 9 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\6020711\1.jpg |
|
|
|
|
It corresponds to the Trench B of Salvi et al. (2003). The site location referes to the Figure 2 of the paper. |
D.Maceroni |
PS60 |
|
|
|
| ITHACA-PS-GIR.89 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS61 |
Fosso Cerasitto 1 |
ExposureDescription |
|
Sequence of alluvial and colluvial deposits |
FaultCode_20711 |
ExposureOrientation |
NE-SW |
|
|
1:150.000 |
Abz027 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 3 m; ExposureLength: 8 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\6120711\1.jpg |
|
|
|
|
It corresponds to the Trench D of Salvi et al. (2003). The site location referes to the Figure 2 of the paper |
D.Maceroni |
PS61 |
|
|
|
| ITHACA-PS-GIR.90 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS62 |
Fosso Cerasitto 2 |
ExposureDescription |
|
Sequence of alluvial and colluvial deposits. |
FaultCode_20711 |
ExposureOrientation |
NNE-SSW |
|
|
1:150.000 |
Abz027 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 3 m; ExposureLength: 8 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\6220711\1.jpg |
|
|
|
|
It corresponds to the Trench E of Salvi et al. (2003). The site location referes to the Figure 2 of the paper |
D.Maceroni |
PS62 |
|
|
|
| ITHACA-PS-GIR.91 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS63 |
Piano Aremogna 2 |
ExposureDescription |
|
Sequence of fluvioglacial fan deposits, capped by organic rich lacustrine and alluvial sediments and paleosols. The trench intersects three sub-parallel antithetic scarps. |
FaultCode_23402 |
ExposureOrientation |
W-E |
|
|
1:50.000 |
Abz011 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2.5 m; ExposureLength: 50 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\6323402\1.jpg |
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\6323402\2.jpg |
|
|
|
It corresponds to Trench 2 of D'Addezio et al. (2001). The site location refers to Figure 4 of the paper. |
D.Maceroni |
PS63 |
|
|
|
| ITHACA-PS-GIR.92 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS64 |
Norcia T10 |
ExposureDescription |
|
The exposed deposits can be referred to the Late Pleistocene Patino fan activity and to Holocene-Present colluvia. |
FaultCode_141917 |
ExposureOrientation |
NE-SW |
|
|
1:5000 |
Umb015 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 3 m; ExposureLength: 10 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\64141917\2.jpg |
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\64141917\1.jpg |
|
|
|
It corresponds to the trench (T10) of Galli et al. (2018). The site location is derived from Accordo di Collaborazione Scientifica tra il Commissario Straordinario per la Ricostruzione e INGV (2022) - Lotto Norcia. |
D.Maceroni |
PS64 |
|
|
|
| ITHACA-PS-GIR.93 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS65 |
Norcia T9 |
ExposureDescription |
|
The trench exposed Patino gravels which are faulted against LGM fan gravels and orange, silty colluvia. |
FaultCode_141915 |
ExposureOrientation |
NE-SW |
|
|
1:5000 |
Umb009 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 5 m; ExposureLength: 20 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\65141915\1.jpg |
|
|
|
|
It corresponds to the trench (T9) of Galli et al. (2018). The site location is derived from Accordo di Collaborazione Scientifica tra il Commissario Straordinario per la Ricostruzione e INGV (2022) - Lotto Norcia. |
D.Maceroni |
PS65 |
|
|
|
| ITHACA-PS-GIR.94 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS67 |
Norcia T6 |
ExposureDescription |
|
The trench exposed a 3-m-wide fault zone, where different levels of the Patino fan succession were juxtaposed |
FaultCode_141913 |
ExposureOrientation |
NE-SW |
|
|
1:5000 |
Umb015 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 3 m; ExposureLength: 20 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\67141913\1.jpg |
|
|
|
|
It correspondss to the trench (T6) of Galli et al. (2018). The site location is derived from Accordo di Collaborazione Scientifica tra il Commissario Straordinario per la Ricostruzione e INGV (2022) - Lotto Norcia. |
D.Maceroni |
PS67 |
|
|
|
| ITHACA-PS-GIR.95 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS68 |
Norcia T5 |
ExposureDescription |
|
The trench exposed the upper Patin fan succession faulted against massive, fine gravels in silty orange matrix |
FaultCode_141916 |
ExposureOrientation |
NE-SW |
|
|
1:5000 |
Umb009 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 4 m; ExposureLength: 20 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\68141916\1.jpg |
|
|
|
|
It corresponds to the trench (T5) of Galli et al. (2018). The site location is derived from Accordo di Collaborazione Scientifica tra il Commissario Straordinario per la Ricostruzione e INGV (2022) - Lotto Norcia. |
D.Maceroni |
PS68 |
|
|
|
| ITHACA-PS-GIR.96 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS70 |
Norcia T3 |
ExposureDescription |
|
Trenches dragged along antitethic fault. The footwall sequence is composed by gravels of the Patino alluvial fan, conversely, all the units in the hangingwall are of colluvial nature. |
FaultCode_141916 |
ExposureOrientation |
NE-SW |
|
|
1:5000 |
Umb013 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 6 m; ExposureLength: 15 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\70141916\1.jpg |
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\70141916\2.jpg |
|
|
|
It corresponds to the trench (T3) of Galli et al. (2005). The site location is derived from Accordo di Collaborazione Scientifica tra il Commissario Straordinario per la Ricostruzione e INGV (2022) - Lotto Norcia. |
D.Maceroni |
PS70 |
|
|
|
| ITHACA-PS-GIR.97 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS71 |
Norcia T1-T2 |
ExposureDescription |
|
Trenches dragged along antitethic fault. The footwall sequence is composed by gravels of the Patino alluvial fan, conversely, all the units in the hangingwall are of colluvial nature. |
FaultCode_141916 |
ExposureOrientation |
NE-SW |
|
|
1:5000 |
Umb013 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 6 m; ExposureLength: 15 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\71141916\1.jpg |
|
|
|
|
It corresponds to the trenches (T1 and T2) of Galli et al. (2005). The site location is derived from Accordo di Collaborazione Scientifica tra il Commissario Straordinario per la Ricostruzione e INGV (2022) - Lotto Norcia. |
D.Maceroni |
PS71 |
|
|
|
| ITHACA-PS-GIR.98 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS72 |
Norcia synthetic splay |
ExposureDescription |
|
The trench exposed the tectonic contact between faintly stratified carbonate gravels and gravelly colluvia in the abundant, sandy, reddish |
FaultCode_141913 |
ExposureOrientation |
NE-SW |
|
|
1:5000 |
Umb015 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 4 m; ExposureLength: 50 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\72141913\1.jpg |
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\72141913\2.jpg |
|
|
|
It corresponds to the Trench 11 of Galli et al. (2023). The site location refers to trench T01 deriving from Accordo di Collaborazione Scientifica tra Commissario per la Ricostruzione e INGV (2022) - Lotto Norcia |
D.Maceroni |
PS72 |
|
|
|
| ITHACA-PS-GIR.99 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS73 |
Norcia antithetic splay |
ExposureDescription |
|
The trench exposed mainly the well-stratified gravels of the Patino alluvial fan. |
FaultCode_141916 |
ExposureOrientation |
NE-SW |
|
|
1:5000 |
Umb015 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 3 m; ExposureLength: 40 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\73141916\1.jpg |
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\73141916\2.jpg |
|
|
|
It corresponds to the Trench 13 of Galli et al. (2023). The site location refers to T02 deriving from Accordo di Collaborazione Scientifica tra il Commissario Straordinario per la Ricostruzione e INGV (2022) - Lotto Norcia |
D.Maceroni |
PS73 |
|
|
|
| ITHACA-PS-GIR.100 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS75 |
Norcia T7 |
ExposureDescription |
|
The trench exposed the Patino fan gravels in the footwall faulted against sandy gravel colluvial in the hanging wall. |
FaultCode_141913 |
ExposureOrientation |
NE-SW |
|
|
1:5000 |
Umb009 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2 m; ExposureLength: 4 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\75141913\1.jpg |
|
|
|
|
It corresponds to the trench (T7) of Galli et al. (2018). The site location is derived from Accordo di Collaborazione Scientifica tra il Commissario Straordinario per la Ricostruzione e INGV (2022) - Lotto Norcia. |
D.Maceroni |
PS75 |
|
|
|
| ITHACA-PS-GIR.101 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS76 |
Norcia T8 |
ExposureDescription |
|
The trench exposed a complex fault zone, made by dozens of splays accomodating a general warping of the succession and of the erosional top of the Patino fan gravels |
FaultCode_141915 |
ExposureOrientation |
NE-SW |
|
|
1:5000 |
Umb009 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 3.5 m; ExposureLength: 22 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\76141915\1.jpg |
|
|
|
|
It corresponds to the trench (T8) of Galli et al. (2018). The site location is derived from Accordo di Collaborazione Scientifica tra il Commissario Straordinario per la Ricostruzione e INGV (2022) - Lotto Norcia. |
D.Maceroni |
PS76 |
|
|
|
| ITHACA-PS-GIR.102 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS77 |
Norcia T4 |
ExposureDescription |
|
The trench exposed the upper Patino fan succession faulted against massive, fine gravels in silty orange matrix |
FaultCode_141916 |
ExposureOrientation |
NE-SW |
|
|
1:5000 |
Umb009 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 5 m; ExposureLength: 8 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\77141916\1.jpg |
|
|
|
|
It corresponds to the trench (T4) of Galli et al. (2018). The site location is derived from Accordo di Collaborazione Scientifica tra il Commissario Straordinario per la Ricostruzione e INGV (2022) - Lotto Norcia. |
D.Maceroni |
PS77 |
|
|
|
| ITHACA-PS-GIR.103 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS66 |
Capo del Colle |
ExposureDescription |
|
The trench exumed the foundation of the wall of a house, which shows evidence of ductile and brittle deformation as well as caesuras, restorations and reconstructions. |
FaultCode_141904 |
ExposureOrientation |
NE-SW |
|
|
1:5000 |
Umb015 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 1-2 m; ExposureLength: 6-7 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\66141904\1.jpg |
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\66141904\2.jpg |
|
|
|
It corresponds to the Trench 14 of Galli et al. (2023). The site location is derived from Accordo di Collaborazione Scientifica tra il Commissario Straordinario per la Ricostruzione e INGV (2022) - Lotto Norcia. |
D.Maceroni |
PS66 |
|
|
|
| ITHACA-PS-GIR.104 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS69 |
Campi-Capo del Colle |
ExposureDescription |
|
The trench exposed a homogeneous succession of fine, alluvial fan gravels, weel-stratified, invert-graded, subangular and reworked upward by agricultural processes. Any certain element of either brittle or ductile deformation was observed. |
FaultCode_141905 |
ExposureOrientation |
NE-SW |
|
|
1:5000 |
Umb015 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 3 m; ExposureLength: 45 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\69141905\1.jpg |
|
|
|
|
It corresponds to the Trench 15 of Galli et al. (2023). The site location is derived from Accordo di Collaborazione Scientifica tra il Commissario Straordinario per la Ricostruzione e INGV (2022) - Lotto Norcia. |
D.Maceroni |
PS69 |
|
|
|
| ITHACA-PS-GIR.105 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS74 |
Campi basso |
ExposureDescription |
|
The trench exposed a homogeneous succession of faintly stratified, medium-to-fine alluvial fan gravels, with angular clasts, alternating with discontinuous, massive course horizons in a brown sandy-silty matrix. |
FaultCode_141906 |
ExposureOrientation |
NE-SW |
|
|
1:5000 |
Umb015 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2-3 m; ExposureLength: 65 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\74141906\1.jpg |
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\74141906\2.jpg |
|
|
|
It corresponds to the Trench 16 of Galli et al. (2023). The site location is derived from Accordo di Collaborazione Scientifica tra il Commissario Straordinario per la Ricostruzione e INGV (2022) - Lotto Norcia. |
D.Maceroni |
PS74 |
|
|
|
| ITHACA-PS-GIR.106 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS78 |
Pielarocca |
|
|
|
FaultCode_141902 |
ExposureOrientation |
NE-SW |
|
|
1:1 |
Umb015 |
|
|
|
|
|
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OUT |
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C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\78141902\1.jpg |
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|
Cemented slope debris faulted and dragged along the carbonate slickenside. |
D.Maceroni |
PS78 |
|
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|
| ITHACA-PS-GIR.107 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS80 |
Borgo Incile |
ExposureDescription |
|
The excavated walls exposed prevalently fluvial and lacustrine sediments, wich we have subdivided into seven different units. |
FaultCode_20200 |
ExposureOrientation |
NE-SW |
|
|
1:500.000 |
Abz028 |
|
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|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2-3 m; ExposureLength: 44 |
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TR |
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C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\8020200\1.jpg |
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\8020200\2.jpg |
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|
There is no evidence of faulting or fractures at least for the last 20 kyrs. Evidence of paleoliquefaction has been observed. The site location refers to the Figure 3(a) of Iezzi et al. (2023) |
D.Maceroni |
PS80 |
|
|
|
| ITHACA-PS-GIR.108 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS81 |
Perrella site_01 |
ExposureDescription |
|
Stratigraphic record made of colluvial and alluvial sediments interbedded with pedogenetic horizons. |
FaultCode_20200 |
ExposureOrientation |
NE-SW |
|
|
1:100 |
Abz028 |
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|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2.5-3 m; ExposureLength: 83 m |
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TR |
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C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\8120200\1.jpg |
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\8120200\2.jpg |
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|
There is no evidence of faulting. Evidence of paleoliquefaction has been observed in the eastern termination, at distance 73-75 m. The site location refers to Figure 7(a) of Iezzi et al. (2023) |
D.Maceroni |
PS81 |
|
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|
| ITHACA-PS-GIR.109 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS82 |
Perrella site_02 |
ExposureDescription |
|
Stratigraphic record made of colluvial and alluvial sediments interbedded with pedogenetic horizons. |
FaultCode_20200 |
ExposureOrientation |
E-W |
|
|
1:100 |
Abz028 |
|
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|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2.5-3 m; ExposureLength: 8 m |
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TR |
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C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\8220200\1.jpg |
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\8220200\2.jpg |
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|
There is no evidence of faulting. The site location refers to Figure 7(a) of Iezzi et al. (2023) |
D.Maceroni |
PS82 |
|
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|
| ITHACA-PS-GIR.110 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS83 |
Perrella site_03 |
ExposureDescription |
|
Stratigraphic record made of colluvial and alluvial sediments interbedded with pedogenetic horizons. |
FaultCode_20200 |
ExposureOrientation |
WNW-ESE |
|
|
1:100 |
Abz028 |
|
|
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|
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|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2.5-3 m; ExposureLength: 23 m |
|
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|
TR |
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|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\8320200\1.jpg |
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\8320200\2.jpg |
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|
There is no evidence of faulting. The site location refers to Figure 7(a) of Iezzi et al. (2023) |
D.Maceroni |
PS83 |
|
|
|
| ITHACA-PS-GIR.111 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS84 |
Perrella site_04 |
ExposureDescription |
|
Stratigraphic record made of colluvial and alluvial sediments interbedded with pedogenetic horizons. |
FaultCode_20200 |
ExposureOrientation |
E-W |
|
|
1:100 |
Abz028 |
|
|
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|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2.5-3 m; ExposureLength: 27 m |
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TR |
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|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\8420200\1.jpg |
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|
There is no evidence of faulting. The site location refers to Figure 7(a) of Iezzi et al. (2023) |
D.Maceroni |
PS84 |
|
|
|
| ITHACA-PS-GIR.112 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS85 |
Manigi quarry |
ExposureDescription |
|
Late Pleistocene slope deposits faulted against Mesozoic limestone along a N304 antithetic splay. However, the trace of this fault is not provided in Galli et al. (2020). |
FaultCode_140302 |
ExposureOrientation |
W-E/NW-SE/NE-SW |
|
|
1:1 |
Umb012 |
|
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QF |
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|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\85140302\1.jpg |
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\85140302\2.jpg |
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|
The location of the quarry is easily observed on DEM and Google base maps. |
D. Maceroni |
PS85 |
|
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|
| ITHACA-PS-GIR.113 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS86 |
Mt.Alvagnano site |
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|
FaultCode_141931 |
ExposureOrientation |
NW-SE |
|
|
1:1 |
Umb012 |
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OUT |
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C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\86141931\1.jpg |
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|
The location of the outcrop is easily observed on DEM and Google base maps. |
D. Maceroni |
PS86 |
|
|
|
| ITHACA-PS-GIR.114 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS121 |
Vallicella_A |
ExposureDescription |
|
Alluvial and colluvial deposits. The upper part of these deposits is referable to the Holocene, while a few metres down in the trench, alluvial deposits referable to the Upper Pleistocene can be identified. |
FaultCode_20000 |
ExposureOrientation |
NNE-WWS |
|
|
1:5000 |
Abz001 |
|
|
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|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2.5 m; ExposureLength: 158 m |
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|
TR |
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|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\10020001\1.jpg |
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\10020001\2.jpg |
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|
The Vallicella trench has a total length of 150 m and revealed the presence of three faults. For the description of the recognised seismic events, it was necessary to split the trench into three points (A,B,C) located along the faults. |
D. Maceroni |
PS121 |
|
|
|
| ITHACA-PS-GIR.115 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS122 |
Vallicella_B |
ExposureDescription |
|
Alluvial and colluvial deposits. The upper part of these deposits is referable to the Holocene, while a few metres down in the trench, alluvial deposits referable to the Upper Pleistocene can be identified. |
FaultCode_20002 |
ExposureOrientation |
NNE-WWS |
|
|
1:5000 |
Abz001 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2.5 m; ExposureLength: 158 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\10120002\1.jpg |
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\10120002\2.jpg |
|
|
|
The Vallicella trench has a total length of 150 m and revealed the presence of three faults. For the description of the recognised seismic events, it was necessary to split the trench into three points (A,B,C) located along the faults. |
D. Maceroni |
PS122 |
|
|
|
| ITHACA-PS-GIR.116 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS123 |
Vallicella_C |
ExposureDescription |
|
Alluvial and colluvial deposits. The upper part of these deposits is referable to the Holocene, while a few metres down in the trench, alluvial deposits referable to the Upper Pleistocene can be identified. |
FaultCode_20003 |
ExposureOrientation |
NNE-WWS |
|
|
1:5000 |
Abz001 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2.5 m; ExposureLength: 158 m |
|
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|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\10220003\1.jpg |
|
|
|
|
The Vallicella trench has a total length of 150 m and revealed the presence of three faults. For the description of the recognised seismic events, it was necessary to split the trench into three points (A,B,C) located along the faults. |
D. Maceroni |
PS123 |
|
|
|
| ITHACA-PS-GIR.117 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS126 |
Collemusino_A |
ExposureDescription |
|
Holocenic alluvial fan deposits |
FaultCode_20018 |
ExposureOrientation |
NE-SE |
|
|
1:5000 |
Abz002 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2,5 m; ExposureLength: 19 m |
|
|
|
|
|
|
|
TR |
|
|
|
|
|
|
|
|
|
D. Maceroni |
PS126 |
|
|
|
| ITHACA-PS-GIR.118 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS127 |
Collemusino_B |
ExposureDescription |
|
Holocenic alluvial fan deposits |
FaultCode_20019 |
ExposureOrientation |
NE-SW |
|
|
1:5000 |
Abz002 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2,5 m; ExposureLength: 13 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\106Collemusino\1.jpg |
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\106Collemusino\2.jpg |
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|
D. Maceroni |
PS127 |
|
|
|
| ITHACA-PS-GIR.119 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS128 |
Pizzoli |
ExposureDescription |
|
Sequence of alluvial fan, colluvial and slope deposits |
FaultCode_20003 |
ExposureOrientation |
NE |
|
|
1:10.000 |
Abz003 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2 m; ExposureLength: 28 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\10720003\1.jpg |
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\10720003\2.jpg |
|
|
|
|
D. Maceroni |
PS128 |
|
|
|
| ITHACA-PS-GIR.120 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS129 |
Pizzoli_1 |
ExposureDescription |
|
Colluvial and alluvial deposits of the Upper Pleistocene, as well as a couple of palaeosols, all of which were displaced by four faults. |
FaultCode_20003 |
ExposureOrientation |
NE-SW |
|
|
1:30.000 |
Abz004 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 3 m; ExposureLength: 30 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\12920003\1.jpg |
|
|
|
|
This trench was opened by Moro et al. (2002) but Galli et al. (2011) improved the previous paleoseismological data through new radiocarbon dating samples. |
D. Maceroni |
PS129 |
|
|
|
| ITHACA-PS-GIR.121 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS130 |
Arischia |
ExposureDescription |
|
Mainly fine, well-stratifiedm alluvial fan gravels capped by a dark-brown palaeosol. |
FaultCode_20026 |
ExposureOrientation |
NE-SW |
|
|
1:30.000 |
Abz004 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2-2.5 m; ExposureLength: 10 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\130Arischia\1.jpg |
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|
|
|
D. Maceroni |
PS130 |
|
|
|
| ITHACA-PS-GIR.122 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS131 |
Mt. Marine_A |
ExposureDescription |
|
The excavations walls exposed evidence for faulting and displacement of the exposed colluvial, organic rich and cultural sediments, and paleosols. |
FaultCode_20003 |
ExposureOrientation |
NE-SW |
|
|
1:50.000 |
Abz006 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2 m; ExposureLength: 5 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\13120003\1.jpg |
|
|
|
|
|
D. Maceroni |
PS131 |
|
|
|
| ITHACA-PS-GIR.123 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS132 |
Mt. Marine_B |
ExposureDescription |
|
The excavations walls exposed evidence for faulting and displacement of the exposed colluvial, organic rich and cultural sediments, and paleosols. |
FaultCode_20001 |
ExposureOrientation |
NW-SE |
|
|
1:50.000 |
Abz006 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2 m; ExposureLength: 4 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\13220001\1.jpg |
|
|
|
|
|
D. Maceroni |
PS132 |
|
|
|
| ITHACA-PS-GIR.124 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS133 |
Mt. Pettino |
ExposureDescription |
|
It exposed mainly slope angular fine gravels, that are faintly stratified and mantled by a dark-brown palaeosol with sparse carbonate clasts, which is truncated upwards by other layered slope debris deposits. |
FaultCode_20084 |
ExposureOrientation |
NE-SW |
|
|
1:30.000 |
Abz004 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 5 m; ExposureLength: 15 m |
|
|
|
|
|
|
|
TR |
|
|
|
|
|
|
|
|
|
D. Maceroni |
PS133 |
|
|
|
| ITHACA-PS-GIR.125 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS02 |
SG2 |
ExposureDescription |
|
The trench exibits the depositional, erosional and deformational history of the site in the last 30 ka. |
FaultCode_20118 |
ExposureOrientation |
NNE-SSW |
|
|
1:1250 |
Abz033 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2.5 m; ExposureLength: 60 m |
|
|
|
|
|
|
|
TR |
|
|
|
|
|
|
|
|
|
D.Maceroni |
PS02 |
|
|
|
| ITHACA-PS-GIR.126 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS134 |
SG_Quarry site |
ExposureDescription |
|
Complex NW-SE trending fault zone, cutting both the bedrock, the paleosols and the alluvial and debris deposits. |
FaultCode_20114 |
ExposureOrientation |
NNE-SSW |
|
|
1:1250 |
Abz033 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 25 m; ExposureLength: 4 m |
|
|
|
|
|
|
|
QF |
|
|
|
|
|
|
|
|
The dicrete events horizons of surface faulting are not identified. Nevertheless, the structural setting, the intense deformation of the stratigraphy and the chronological context point to repeated tectonic activity in the Late Pleistocene. |
D.Maceroni |
PS134 |
|
|
|
| ITHACA-PS-GIR.127 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS01 |
SG1 |
ExposureDescription |
|
The trench exibits the depositional, erosional and deformational history of the site in the last 30 ka. |
FaultCode_20114 |
ExposureOrientation |
NNE-SSW |
|
|
1:1250 |
Abz033 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 1.5 m; ExposureLength: 5 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\deborah.maceroni\OneDrive - ISPRA\ISPRA - Lavoro\Lavoro\PNRR Geosciences\Progetti GIS\Photos_Sketches_Log\120114\1.jpg |
|
|
|
|
|
D.Maceroni |
PS01 |
|
|
|
| ITHACA-PS-GIR.128 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS135 |
Capanna Ghezzi |
ExposureDescription |
|
The succession was made by both swamp and colluvial deposits, with important pedogenized horizons. |
FaultCode_141217 |
ExposureOrientation |
N-S |
|
|
1:25.000 |
Umb027 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 4 m; ExposureLength: 8 m |
|
|
|
|
|
|
|
TR |
|
|
|
|
|
|
|
|
|
D. Maceroni |
PS135 |
|
|
|
| ITHACA-PS-GIR.129 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS136 |
Portella di Vao |
ExposureDescription |
|
The trench exposed fine sands, silts, and clays, with interbedded thin levels of coarse-to-medium gravels. Sediments are mainly of palustrine-lacustrine origin, partly laminated, and with a primary, subhorizontal layering. |
FaultCode_141214 |
ExposureOrientation |
NE-SW |
|
|
1:25.000 |
Umb027 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 4.5 m; ExposureLength: 18 m |
|
|
|
|
|
|
|
TR |
|
|
|
|
|
|
|
|
|
D. Maceroni |
PS136 |
|
|
|
| ITHACA-PS-GIR.130 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS137 |
Colle Infante site |
ExposureDescription |
|
The trench exposed clinostratigrafied, slope-derived gravels in a silty matrix faulted against coarse gravels and limestone |
FaultCode_141214 |
ExposureOrientation |
SW-NE |
|
|
1:25.000 |
Umb027 |
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|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 3 m; ExposureLength: 12 m |
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TR |
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|
D. Maceroni |
PS137 |
|
|
|
| ITHACA-PS-GIR.131 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS138 |
Capitignano site 1 |
ExposureDescription |
|
Tectonic contact between miocenic bedrock and likely Late Pleistocene-Holocene continental deposits |
FaultCode_21800 |
ExposureOrientation |
NE-SW |
|
|
1:5000 |
Abz036 |
|
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|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2,5 m; ExposureLength: 34 m |
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TR |
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|
D. Maceroni |
PS138 |
|
|
|
| ITHACA-PS-GIR.132 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS58 |
Capitignano site 3 |
ExposureDescription |
|
Fault plane that affects Holocene continental deposits |
FaultCode_21800 |
ExposureOrientation |
NE-SW |
|
|
1:5000 |
Abz036 |
|
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|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2 m; ExposureLength: 10 m |
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TR |
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|
D. Maceroni |
PS58 |
|
|
|
| ITHACA-PS-GIR.133 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS140 |
Capitignano site 4 |
ExposureDescription |
|
Fault plane that affects Holocene continental deposits |
FaultCode_21800 |
ExposureOrientation |
NE-SW |
|
|
1:5000 |
Abz036 |
|
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|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2 m; ExposureLength: 10 m |
|
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TR |
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|
D. Maceroni |
PS140 |
|
|
|
| ITHACA-PS-GIR.134 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS141 |
San Giovanni trench |
|
|
|
FaultCode_20112 |
ExposureOrientation |
NE-SW |
|
|
1:5000 |
Abz036 |
|
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TR |
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|
D. Maceroni |
PS141 |
|
|
|
| ITHACA-PS-GIR.135 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS142 |
Paganica T2 |
ExposureDescription |
|
The trench took advantage of the gorge that opened as a conseguence of the rupture of a joint Gran Sasso watern pipeline. The wall exposed faintly stratified carbonate gravels, which are generally clast-supported or with levels in a coarse sandy matrix |
FaultCode_20087 |
ExposureOrientation |
NE-SW |
|
|
1:65000 |
Abz038 |
|
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TR |
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|
D. Maceroni |
PS142 |
|
|
|
| ITHACA-PS-GIR.136 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS143 |
Paganica T1 |
ExposureDescription |
|
The trench was opened at the apex of an alluvial fan, showing 14 different lithological units. |
FaultCode_20087 |
ExposureOrientation |
NE-SW |
|
|
1:65000 |
Abz038 |
|
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|
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|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 3-6 m; ExposureLength: 25 m |
|
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TR |
|
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|
|
D. Maceroni |
PS143 |
|
|
|
| ITHACA-PS-GIR.137 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS144 |
Paganica T3 |
ExposureDescription |
|
The fault zone visible in the trench showa a graben-like feature that involves almost all of the outcropping deposits |
FaultCode_20087 |
ExposureOrientation |
NE-SW |
|
|
1:65000 |
Abz038 |
|
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TR |
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|
D. Maceroni |
PS144 |
|
|
|
| ITHACA-PS-GIR.138 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS145 |
Paganica T4 |
ExposureDescription |
|
Lower Pleistocene alluvial fan gravel in the footwall that was faulted against alternating Late Pleistocene-Holocene slope debris, colluvia and alluvial fan deposits |
FaultCode_20087 |
ExposureOrientation |
NE-SW |
|
|
1:20.000 |
Abz004 |
|
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|
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|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 3-6 m; ExposureLength: 25 m |
|
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|
TR |
|
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|
|
D. Maceroni |
PS145 |
|
|
|
| ITHACA-PS-GIR.139 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS146 |
Paganica T5 |
ExposureDescription |
|
Faulting of Middle Pleistocene alluvial gravels, capped by Late Pleistocene palaeosol and colluvia, against Holocene slope deposits |
FaultCode_20087 |
ExposureOrientation |
NE-SW |
|
|
1:10.000 |
Abz004 |
|
|
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|
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|
TR |
|
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|
|
The trench matches with the median sector of a long gorge that was opened by the 2009 coseism Gran Sasso aqueduct rupture. |
D. Maceroni |
PS146 |
|
|
|
| ITHACA-PS-GIR.140 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS98 |
Colle Enzano P1 |
ExposureDescription |
|
The exposes a wedge of massive sub-angular clasts, which are rich in an organic, brownish sandy matrix that has been deeply dragged along the rock fault plane. |
FaultCode_20092 |
ExposureOrientation |
NE-SW |
|
|
1:65000 |
Abz038 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
|
|
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|
HE |
|
|
|
|
|
|
|
|
Hand-made pit close to the carbonate fault plane, which was the same plane where surface-faulting phenomena were observed during 2009 earthquake |
D. Maceroni |
PS98 |
|
|
|
| ITHACA-PS-GIR.141 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS147 |
Monte Valva T2 |
ExposureDescription |
|
Slope deposits |
FaultCode_51500 |
ExposureOrientation |
NE-SW |
|
|
1:285.000 |
Cam164 |
|
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|
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|
TR |
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|
C:\Users\franc\OneDrive - Università di Napoli Federico II\PROGETTI PNRR\PNRR GEOSCIENCES\DATABASE PALEOSISMOLOGIA\PROGETTO QGIS\photos_sketches_logs\11151500\1.jpgLL |
|
|
|
|
It corresponds to T2 of Galli and Peronace (2014). Paleoevents are derived combining findings from this site and from T1 of Galli and Peronace (2014) |
F. Iezzi |
PS147 |
|
|
|
| ITHACA-PS-GIR.142 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS148 |
Piano di Pecore T1 |
ExposureDescription |
|
Lacustrine and colluvial deposits |
FaultCode_51503 |
ExposureOrientation |
N-S |
|
|
1:1 |
Cam221 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 4 m; ExposureLength: 33 m |
|
|
|
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|
TR |
|
|
|
C:\Users\franc\OneDrive - Università di Napoli Federico II\PROGETTI PNRR\PNRR GEOSCIENCES\DATABASE PALEOSISMOLOGIA\PROGETTO QGIS\photos_sketches_logs\11551503\1.jpg |
C:\Users\franc\OneDrive - Università di Napoli Federico II\PROGETTI PNRR\PNRR GEOSCIENCES\DATABASE PALEOSISMOLOGIA\PROGETTO QGIS\photos_sketches_logs\11551503\2.jpg |
|
|
|
It corresponds to Trench 1 of Pantosti et al. (1993). Paleoevents are derived combining findings from this site and from Trench 2 of Pantosti et al. (1993) |
F. Iezzi |
PS148 |
|
|
|
| ITHACA-PS-GIR.143 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS149 |
Pantano San Gregorio T4 |
ExposureDescription |
|
Lacustrine and colluvial deposits |
FaultCode_51522 |
ExposureOrientation |
NE-SW |
|
|
1:1 |
Cam129 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 5-6 m; ExposureLength: 30 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\franc\OneDrive - Università di Napoli Federico II\PROGETTI PNRR\PNRR GEOSCIENCES\DATABASE PALEOSISMOLOGIA\PROGETTO QGIS\photos_sketches_logs_UNINA04\11751522\1 |
|
|
|
|
It corresponds to Trench 4 of D'Addezio et al. (1991). Paleoevents are derived combining findings from this site and from Trench 3 of D'Addezio et al. (1991) |
F. Iezzi |
PS149 |
|
|
|
| ITHACA-PS-GIR.144 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS150 |
Patalecchia_Il Lago |
ExposureDescription |
|
Alluvial fan deposits |
FaultCode_120110 |
|
|
|
|
1:1 |
Mol004 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 1.5 m; ExposureLength: 50 m |
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\franc\OneDrive - Università di Napoli Federico II\PROGETTI PNRR\PNRR GEOSCIENCES\DATABASE PALEOSISMOLOGIA\PROGETTO QGIS\photos_sketches_logs_UNINA04\120120110\1 |
C:\Users\franc\OneDrive - Università di Napoli Federico II\PROGETTI PNRR\PNRR GEOSCIENCES\DATABASE PALEOSISMOLOGIA\PROGETTO QGIS\photos_sketches_logs_UNINA04\120120110\2 |
|
|
|
|
F. Iezzi |
PS150 |
|
|
|
| ITHACA-PS-GIR.145 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS151 |
Monte Valva T1 |
ExposureDescription |
|
Slope deposits |
FaultCode_51500 |
ExposureOrientation |
NE-SW |
|
|
1:285.000 |
Cam164 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
TR |
|
|
|
C:\Users\franc\OneDrive - Università di Napoli Federico II\PROGETTI PNRR\PNRR GEOSCIENCES\DATABASE PALEOSISMOLOGIA\PROGETTO QGIS\photos_sketches_logs\12151500\1.jpg |
|
|
|
|
It corresponds to site T1 of Galli and Peronace (2014). Paleoevents are derived combining findings from this site and from T2 of Galli and Peronace (2014) |
F. Iezzi |
PS151 |
|
|
|
| ITHACA-PS-GIR.146 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS152 |
Quarry |
ExposureDescription |
|
Colluvial and slope deposits with paleosols |
FaultCode_31413 |
|
|
|
|
1:1 |
Bas058 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
|
|
|
|
|
|
|
|
QF |
|
|
|
|
C:\Users\franc\OneDrive - Università di Napoli Federico II\PROGETTI PNRR\PNRR GEOSCIENCES\DATABASE PALEOSISMOLOGIA\PROGETTO QGIS\photos_sketches_logs_UNINA04\21831413\2.jpg |
|
|
|
It corresponds to the Quarry site of Moro et al. (2007) |
F. Iezzi |
PS152 |
|
|
|
| ITHACA-PS-GIR.147 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS153 |
S. Angelo Le Fratte |
ExposureDescription |
|
Slope deposits |
FaultCode_31403 |
|
|
|
|
1:111111 |
Bas058 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
OUT |
|
|
|
|
C:\Users\franc\OneDrive - Università di Napoli Federico II\PROGETTI PNRR\PNRR GEOSCIENCES\DATABASE PALEOSISMOLOGIA\PROGETTO QGIS\photos_sketches_logs_UNINA04\21831403\2.jpg |
|
|
|
Faulted slope deposits dated 14924-14171 cal BC (radiocarbon dating, conventional age 13840±50 BP). It corresponds to the S. Angelo Le Fratte site of Moro et al. (2007) |
F. Iezzi |
PS153 |
|
|
|
| ITHACA-PS-GIR.148 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS154 |
Aqueduct site |
ExposureDescription |
|
Middle Pleistocene calcareous conglomerate, Late Pleistocene alluvial braidplain deposits, colluvial, alluvial and slope wash deposits. |
FaultCode_20087 |
ExposureOrientation |
NE-SW |
|
|
1:10.000 |
Abz030 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 4 m; ExposureLength: 80 m |
|
|
|
|
|
|
|
TR |
|
|
|
|
|
|
|
|
at this site, the 2009 ruptures occurred at the base of the scarp on the fields and tarmac road adjacent to the pipeline |
D. Maceroni |
PS154 |
|
|
|
| ITHACA-PS-GIR.149 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS155 |
Zaccagnini site |
ExposureDescription |
|
Late-Middle Pleistocene white alluvial gravel against a thick sequence of alluvial and colluvial deposits. |
FaultCode_20087 |
ExposureOrientation |
NE-SW |
|
|
1:10.000 |
Abz030 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 3 m; ExposureLength: 12 m |
|
|
|
|
|
|
|
TR |
|
|
|
|
|
|
|
|
|
D. Maceroni |
PS155 |
|
|
|
| ITHACA-PS-GIR.150 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS156 |
Mo'Tretteca site |
ExposureDescription |
|
Partially cemented whitish alluvial gravel whithin a yellow sandy matrix buried under a layered colluvial sequence characterized by silty to silty clay deposits with abundant, small, mainly angular, carbonatic clasts |
FaultCode_20087 |
ExposureOrientation |
NE-SW |
|
|
1:10.000 |
Abz030 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 3 m; ExposureLength: 20 m |
|
|
|
|
|
|
|
TR |
|
|
|
|
|
|
|
|
|
D. Maceroni |
PS156 |
|
|
|
| ITHACA-PS-GIR.151 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS157 |
250 K site |
ExposureDescription |
|
Colluvial overying the white Late-Middle Pleistocene alluvial gravel |
FaultCode_20094 |
ExposureOrientation |
NE-SW |
|
|
1:10.000 |
Abz030 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
OUT |
|
|
|
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|
|
|
Cut in building yard located in between the two 2009 rupture splays. |
D. Maceroni |
PS157 |
|
|
|
| ITHACA-PS-GIR.152 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS158 |
Paganica T6 |
ExposureDescription |
|
Coarse alluvial gravels are mantled by a reddish, altered sandy-silty palaeosol and are faulted against loose and chaotic slope deposits, with large boulders along the segment underlined by the fault scarp |
FaultCode_20088 |
ExposureOrientation |
NE-SW |
|
|
1:200.000 |
Abz004 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
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|
TR |
|
|
|
|
|
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|
|
The trench involved one of the breaching faults that crossed the relay zone between Paganica and San Gregorio, where surficial breaks were observed in the 2009 earthquake |
D. Maceroni |
PS158 |
|
|
|
| ITHACA-PS-GIR.153 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS03 |
San Demetrio trench |
ExposureDescription |
|
The tench intersected the Valle dell'Inferno and San Mauro formations, a sequence of colluvial deposits moslty related to the fault activity and slope wash alluvial/colluvial layer made of reworked volcanic sand. |
FaultCode_20711 |
ExposureOrientation |
NE-SW |
|
|
1:10.000 |
Abz052 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2-2.5 m; ExposureLength: 127 m |
|
|
|
|
|
|
|
TR |
|
|
|
|
|
|
|
|
|
D. Maceroni |
PS03 |
|
|
|
| ITHACA-PS-GIR.154 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS159 |
Raccapreturo_A |
ExposureDescription |
|
Sedimentary succession made of slope-derived sediments |
FaultCode_20606 |
ExposureOrientation |
NE-SW |
|
|
1:8000 |
Abz054 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2-2.5 m; ExposureLength: 11 m |
|
|
|
|
|
|
|
TR |
|
|
|
|
|
|
|
|
|
D. Maceroni |
PS159 |
|
|
|
| ITHACA-PS-GIR.155 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS160 |
Roccapreturo_B |
ExposureDescription |
|
Sedimentary succession made of slope-derived sediments |
FaultCode_20606 |
ExposureOrientation |
NE-SW |
|
|
1:8000 |
Abz054 |
|
|
|
|
|
|
|
|
ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2-2.5 m; ExposureLength: 5 m |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
D. Maceroni |
PS160 |
|
|
|
| ITHACA-PS-GIR.156 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS161 |
Roman "Maggiore" temple |
ExposureDescription |
|
Sequence of stratified clast-supported slope debris made of angular-to-subangular carbonate clasts. |
FaultCode_20613 |
ExposureOrientation |
NE-SW |
|
|
1:1 |
Abz054 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
TR |
|
|
|
|
|
|
|
|
The trench was dug on top of a debris cone that mantles the fault scarp. Any tectonic displacement affecting the debris was detected. |
D. Maceroni |
PS161 |
|
|
|
| ITHACA-PS-GIR.157 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS162 |
Roman "Maggiore" temple_1 |
ExposureDescription |
|
Slope derived deposits that are clearly displaced by the fault activity. |
FaultCode_20613 |
ExposureOrientation |
NE-SW |
|
|
1:1 |
Abz054 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
TR |
|
|
|
|
|
|
|
|
|
D. Maceroni |
PS162 |
|
|
|
| ITHACA-PS-GIR.158 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS163 |
|
ExposureDescription |
|
The fault displaces slope deposits-mainly nmade of carbonate gravels in brownish sandy-silty organic-rich matrix, dated at 20401-19484 BC. |
FaultCode_20613 |
|
|
|
|
1:1 |
Abz056 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
QF |
|
|
|
|
|
|
|
|
|
D. Maceroni |
PS163 |
|
|
|
| ITHACA-PS-GIR.159 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS164 |
Castel di Ieri_A |
ExposureDescription |
|
The excavation exposed both "natural" (colluvial, fluvial and organic-rich) and "cultural" sediments which fill small holes and excavations occurred during past centuries. |
FaultCode_20613 |
|
|
|
|
1:1 |
Abz056 |
|
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TR |
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D. Maceroni |
PS164 |
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| ITHACA-PS-GIR.160 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS79 |
Castel di Ieri_B |
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FaultCode_20613 |
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1:1 |
Abz056 |
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TR |
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D. Maceroni |
PS79 |
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| ITHACA-PS-GIR.161 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS124 |
Sulmona_T1 |
ExposureDescription |
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It exposed well stratified alluvial fan and massive debris flow deposits that are offset accros several fault strands against younger, faintly cemented, alluvial sands, as well as slope- and scarp-derived colluvial. |
FaultCode_22800 |
ExposureOrientation |
NE-SW |
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1:5000 |
Abz068 |
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ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: > 4 m; ExposureLength: 30 m |
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TR |
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D. Maceroni |
PS124 |
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| ITHACA-PS-GIR.162 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS125 |
Sulmona_T2 |
ExposureDescription |
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It exposed stratigraphic succession similar to that described in PS166 |
FaultCode_22800 |
ExposureOrientation |
NE-SW |
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1:5000 |
Abz068 |
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ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 1.5 m; ExposureLength: 15 m |
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TR |
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D. Maceroni |
PS125 |
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| ITHACA-PS-GIR.163 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS139 |
Sulmona_T3 |
ExposureDescription |
|
It exposed roughly the same alluvial succession of PS166 and PS167 |
FaultCode_22800 |
ExposureOrientation |
NE-SW |
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1:5000 |
Abz068 |
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ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 2.5 m; ExposureLength: 5 m |
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TR |
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D. Maceroni |
PS139 |
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| ITHACA-PS-GIR.164 |
https://hub.geosciences-ir.it/ITHACA/Paleosites/PS50 |
Sulmona_T4 |
ExposureDescription |
|
It exposed well-organized alluvial fan grabels in the footwall that were faulted against alluvial sands and stratified slope colluvia. |
FaultCode_22800 |
ExposureOrientation |
NE-SW |
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1:5000 |
Abz068 |
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ExposureHeigh; ExposureLength |
ExposureHeigh; ExposureLength |
ExposureHeigh: 4-5 m; ExposureLength: 25 m |
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TR |
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D. Maceroni |
PS50 |
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