#area_ Soil Slide3 matching against Ita117309 Total Score: 184,950.00
Properties:
Values:
Score:
Descendants Score:


All   Match   In-Focus   Target
       
Model (In-Focus) Instance (Target) Results

#area_ Soil Slide3:
Property, Value, Freq

Ita117309:
Property, Value, Freq

Match Type

Score

#area_ Soil Slide3's Comment

Ita117309's Comment

Deposit

deposit

present

Deposit

deposit

present

has Bed Rock

clastic sediment

always

has Bed Rock

diamicton

present

exact_exact_ppt - exact_AKO_val

10000

Clastic sediments are a weak lithology

Depositi glaciali. Calcari e dolomie,Depositi glaciali. Calcari e dolomie,Depositi glaciali

has Bed Rock

generic sandstone

always

unmatched

-10

Sandstones is a weak lithology

has Bed Rock

metamorphic rock

always

unmatched

-10

Metamorphic foliated rocks have usually weak geotechnical properties. Basin underlain by these weak rocks are likely to experience more landslides compared to basin underlain by stronger lithologies (Bovis and Jakob 1999).

has Been Logged Within Years

>20

sometimes

unmatched

-10

By 20 year since logging, trees have regrown and the roots are anchoring the soil again (Jackson 2019)

has Been Logged Within Years

0-5

usually

unmatched

-10

Landslides are likely by 0 to 5 years after tree harvesting as the trees are dead but some roots are still providing anchoring effect on the slope (Jackson 2019)

has Been Logged Within Years

10-20

usually

unmatched

-10

Landslides are likely by 10 to 20 years after tree harvesting as new trees are starting to provide anchoring effect with their roots on the slope (Jackson 2019)

has Been Logged Within Years

5-10

always

unmatched

-10

Landslides are extremely likely by 5 to 10 years after tree harvesting. Most of tree roots have died, and new trees are too small to provide anchoring effect with their roots on the slope (Jackson 2019)

has Fault

Any Fault

always

unmatched

-10

The presence of fault is an important factor to determine landslide susceptibility (Reichenbach et al., 2018)

has Fire Within Years

>20

sometimes

has Fire Within Years

>20

present

exact_exact_ppt - exact_exact_val

1000

After 20 year since a wildfire, trees have regrown and the wildfire effects on slope stability have diminished (Jackson 2019)

> 20. 1987.0,1981.0,1990.0

has Fire Within Years

0-2

always

unmatched

-10

Landslides are very likely for 2 years after a wildfire. Water cannot infiltrate, runoff and erosion increase as the soil becomes water repellent and loses cohesion because of the fire heat (Jackson 2019).

has Fire Within Years

10-20

sometimes

unmatched

-10

Landslides are likely between 10 to 20 years after a wildfire. The roots have lost anchoring effect and the new trees are still too small to support the slope (Jakson 2019).

has Fire Within Years

3-5

usually

unmatched

-10

Landslides are likely between 3 to 5 years after a wildfire. The water-repellent soil horizon degrades but the roots of dead trees are starting to rot and they do not support the slope with their anchoring effect anymore (Jackson 2019).

has Fire Within Years

5-10

always

unmatched

-10

Landslides are very likely between 5 to 10 years after a wildfire. Roots of dead trees decay, and they are not supporting the soil anymore as for the case of clear cut logging (Jackson 2019).

has Geomorph Process

ErosionalProcess

always

has Geomorph Process

Gully Erosion

present

exact_exact_ppt - exact_AKO_val

10000

Active erosional processes are possible indicator of landslide activity, as landslides occur where landslides have occurred before.

gully erosion. rock fall,gully erosion, erosional process,karst. rock fall,gully erosion, erosional process,karst

has Geomorph Process

MassMovement

always

has Geomorph Process

Rockfall

present

exact_exact_ppt - exact_AKO_val

10000

Active erosional processes are possible indicator of landslide activity, as landslides occur where landslides have occurred before.

rock fall. rock fall,gully erosion, erosional process,karst. rock fall,gully erosion, erosional process,karst

has Land Use

Alpine

rarely

unmatched

-10

Soil slides rarely occur in the Alpine zone, because usually there is not much soil there.

has Land Use

SubAlpineAvalancheChutes

usually

unmatched

-10

Soil slides can occur in the gullies that are also avalanche tracks.

has Landslide Type

Any Landslide

always

unmatched

-10

Landslides are more likely to occur on slopes or valleys that have experienced landslides before (Guzzetti et al., 2012)

has Landslide Type

Flows in rock

sometimes

unmatched

-10

Where there is rock, it is less likely that there will be soil slides rather than landslides in rock. But landslides in rock ARE a sign of an unstable slope, and therefore are not explicitly negatively correlated to soil slides

has Landslide Type

Flows in soil

usually

has Landslide Type

Debris Flow

present

exact_exact_ppt - exact_AKO_val

27000

Landslides are more likely to occur on slopes or valleys that have experienced landslides before (Guzzetti et al., 2012)

Debris flow. Colamento rapido,Scivolamento rotazionale/traslativo. Colamento rapido,Scivolamento rotazionale/traslativo. Debris flow. Colamento rapido,Aree soggette a frane superficiali diffuse,DGPV,Scivolamento rotazionale/traslativo. Colamento rapido,Aree soggette a frane superficiali diffuse,DGPV,Scivolamento rotazionale/traslativo

has Landslide Type

Rock Fall

sometimes

unmatched

-10

Where there is rock, it is less likely that there will be soil slides rather than landslides in rock. But landslides in rock ARE a sign of an unstable slope, and therefore are not explicitly negatively correlated to soil slides

has Landslide Type

Rock Slope Spread

sometimes

unmatched

-10

Where there is rock, it is less likely that there will be soil slides rather than landslides in rock. But landslides in rock ARE a sign of an unstable slope, and therefore are not explicitly negatively correlated to soil slides

has Landslide Type

Rock topples

sometimes

unmatched

-10

Where there is rock, it is less likely that there will be soil slides rather than landslides in rock. But landslides in rock ARE a sign of an unstable slope, and therefore are not explicitly negatively correlated to soil slides

has Landslide Type

Slides in rock

sometimes

has Landslide Type

Slide

present

exact_exact_ppt - AKO_exact_val

1500

Where there is rock, it is less likely that there will be soil slides rather than landslides in rock. But landslides in rock ARE a sign of an unstable slope, and therefore are not explicitly negatively correlated to soil slides

Slides. Colamento rapido,Scivolamento rotazionale/traslativo. Colamento rapido,Scivolamento rotazionale/traslativo. Slides. Colamento rapido,Aree soggette a frane superficiali diffuse,DGPV,Scivolamento rotazionale/traslativo. Colamento rapido,Aree soggette a frane superficiali diffuse,DGPV,Scivolamento rotazionale/traslativo

has Landslide Type

Slides in soil

always

has Landslide Type

Slides in soil

present

exact_exact_ppt - exact_exact_val

30000

Landslides are more likely to occur on slopes or valleys that have experienced landslides before.

Soil Slide. Colamento rapido,Aree soggette a frane superficiali diffuse,DGPV,Scivolamento rotazionale/traslativo. Colamento rapido,Aree soggette a frane superficiali diffuse,DGPV,Scivolamento rotazionale/traslativo

has Landslide Type

Slope deformation in rock

sometimes

has Landslide Type

Mountain Slope Deformation

present

exact_exact_ppt - exact_AKO_val

3000

Where there is rock, it is less likely that there will be soil slides rather than landslides in rock. But landslides in rock ARE a sign of an unstable slope, and therefore are not explicitly negatively correlated to soil slides

Mountain slope deformation. Colamento rapido,Aree soggette a frane superficiali diffuse,DGPV,Scivolamento rotazionale/traslativo. Colamento rapido,Aree soggette a frane superficiali diffuse,DGPV,Scivolamento rotazionale/traslativo

has Landslide Type

Slope deformation in soil

usually

unmatched

-10

Landslides are more likely to occur on slopes or valleys that have experienced landslides before (Guzzetti et al., 2012)

has Landslide Type

Soil Fall

usually

unmatched

-10

Landslides are more likely to occur on slopes or valleys that have experienced landslides before (Guzzetti et al., 2012)

has Landslide Type

Soil topple

usually

unmatched

-10

Landslides are more likely to occur on slopes or valleys that have experienced landslides before (Guzzetti et al., 2012)

has Landslide Type

Spread in soil

usually

unmatched

-10

Landslides are more likely to occur on slopes or valleys that have experienced landslides before (Guzzetti et al., 2012)

has Rainfall

Extreme Rainfall

always

unmatched

-10

Landslides can be triggered by intense rainfall (Segoni et al., 2018). Rainfall threshold for this study are derived from Friele (2012).

has Rainfall

Mild Rainfall

rarely

unmatched

-10

Landslides can be triggered by intense rainfall (Segoni et al., 2018). Rainfall threshold for this study are derived from Friele (2012).

has Rainfall

Moderate Rainfall

sometimes

unmatched

-10

Landslides can be triggered by intense rainfall (Segoni et al., 2018). Rainfall threshold for this study are derived from Friele (2012).

has Rainfall

Severe Rainfall

usually

unmatched

-10

Landslides can be triggered by intense rainfall (Segoni et al., 2018). Rainfall threshold for this study are derived from Friele (2012).

has Slope

Gentle

rarely

has Slope

Gentle

present

exact_exact_ppt - exact_exact_val

200

Soil slides rarely occur on gentle slopes.

35,3,45,15,25,90

has Slope

Moderate

usually

has Slope

Moderate

present

exact_exact_ppt - exact_exact_val

18000

Soil slides usually occur on moderate slopes.

35,3,45,15,25,90

has Slope

Moderately Steep

usually

has Slope

Moderately Steep

present

exact_exact_ppt - exact_exact_val

18000

Soil slides usually occur on moderate steep slopes.

35,3,45,15,25,90

has Slope

Plain

rarely

has Slope

Plain

present

exact_exact_ppt - exact_exact_val

200

Soil slides rarely occur on plain slopes.

35,3,45,15,25,90

has Slope

Steep

rarely

has Slope

Steep

present

exact_exact_ppt - exact_exact_val

200

Soil slides rarely occur on steep slopes, because usually there is not much soil on steep slopes.

35,3,45,15,25,90

has Slope

Very Steep

rarely

has Slope

Very Steep

present

exact_exact_ppt - exact_exact_val

200

Soil slides rarely occur on steep slopes, because usually there is not much soil on steep slopes.

35,3,45,15,25,90

has Stream Order

1

always

has Stream Order

1 - Headwater stream, with no tributaries.

present

exact_exact_ppt - exact_exact_val

10000

Stream erosion can cause soil slides

4.0. VAL DI PEZZA,N.D. VAL DI PEZZA,N.D.

has Stream Order

2

always

unmatched

-10

Stream erosion can cause soil slides

has Stream Order

3

usually

unmatched

-10

Stream erosion can cause soil slides

has Stream Order

4

usually

unmatched

-10

Stream erosion can cause soil slides

has Stream Order

5

sometimes

unmatched

-10

Large stream erosion may cause soil slides

has Surficial Material

Bedrock

sometimes

has Surficial Material

Bedrock

present

exact_exact_ppt - exact_exact_val

1000

There may be some soil even when 'bedrock' has been mapped as principal surficial material

bedrock. Falde detritiche di rocce carbonatiche prevalentemente stabilizzate dalla vegetazione,Pianori modellati prevalentemente dall?erosione glaciale o connessi a particolari strutture tettoniche, con superfici debolmente ondulate utilizzate a pascolo, localmen. Falde detritiche di rocce carbonatiche prevalentemente stabilizzate dalla vegetazione,Pianori modellati prevalentemente dall?erosione glaciale o connessi a particolari strutture tettoniche, con superfici debolmente ondulate utilizzate a pascolo, localmen

has Surficial Material

Colluvium

always

has Surficial Material

Colluvium

present

exact_exact_ppt - exact_exact_val

10000

Soil slides can be generated when colluvium has been mapped as principal surficial material

colluvium. Falde detritiche di rocce carbonatiche prevalentemente stabilizzate dalla vegetazione,Pianori modellati prevalentemente dall?erosione glaciale o connessi a particolari strutture tettoniche, con superfici debolmente ondulate utilizzate a pascolo, localmen. Falde detritiche di rocce carbonatiche prevalentemente stabilizzate dalla vegetazione,Pianori modellati prevalentemente dall?erosione glaciale o connessi a particolari strutture tettoniche, con superfici debolmente ondulate utilizzate a pascolo, localmen. colluvium. Falde detritiche di rocce carbonatiche prevalentemente stabilizzate dalla vegetazione,Pianori modellati prevalentemente dall?erosione glaciale o connessi a particolari strutture tettoniche, con superfici debolmente ondulate utilizzate a pascolo, localmen. Falde detritiche di rocce carbonatiche prevalentemente stabilizzate dalla vegetazione,Pianori modellati prevalentemente dall?erosione glaciale o connessi a particolari strutture tettoniche, con superfici debolmente ondulate utilizzate a pascolo, localmen. colluvium. Falde detritiche di rocce carbonatiche prevalentemente stabilizzate dalla vegetazione,Pianori modellati prevalentemente dall?erosione glaciale o connessi a particolari strutture tettoniche, con superfici debolmente ondulate utilizzate a pascolo, localmen. Falde detritiche di rocce carbonatiche prevalentemente stabilizzate dalla vegetazione,Pianori modellati prevalentemente dall?erosione glaciale o connessi a particolari strutture tettoniche, con superfici debolmente ondulate utilizzate a pascolo, localmen

has Surficial Material

Morainal Material (Till)

always

has Surficial Material

Morainal Material (Till)

present

exact_exact_ppt - exact_exact_val

10000

Soil slides can be generated when morainal material fails from a slope

morainal material. Falde detritiche di rocce carbonatiche prevalentemente stabilizzate dalla vegetazione,Pianori modellati prevalentemente dall?erosione glaciale o connessi a particolari strutture tettoniche, con superfici debolmente ondulate utilizzate a pascolo, localmen. Falde detritiche di rocce carbonatiche prevalentemente stabilizzate dalla vegetazione,Pianori modellati prevalentemente dall?erosione glaciale o connessi a particolari strutture tettoniche, con superfici debolmente ondulate utilizzate a pascolo, localmen. morainal material. Falde detritiche di rocce carbonatiche prevalentemente stabilizzate dalla vegetazione,Pianori modellati prevalentemente dall?erosione glaciale o connessi a particolari strutture tettoniche, con superfici debolmente ondulate utilizzate a pascolo, localmen. Falde detritiche di rocce carbonatiche prevalentemente stabilizzate dalla vegetazione,Pianori modellati prevalentemente dall?erosione glaciale o connessi a particolari strutture tettoniche, con superfici debolmente ondulate utilizzate a pascolo, localmen

has Texture

blocks

always

has Texture

blocks

present

exact_exact_ppt - exact_exact_val

10000

The presence of block can be indicator of landslide processes

rubble, blocks. rubble, blocks

has Texture

rubble

always

has Texture

rubble

present

exact_exact_ppt - exact_exact_val

10000

The presence of rubble is an indicator of landslide processes.

rubble, blocks. rubble, blocks

has Transport Line

Highway

rarely

unmatched

-10

Roads are aggravating factor for landslide activity as compared to undisturbed slopes (Jackson 2019).

has Transport Line

Road Recreation Demographic

sometimes

unmatched

-10

Roads are a aggravating factor for landslide activity as compared to undisturbed slopes (Jackson 2019)

has Transport Line

Road Resource

always

has Transport Line

Road

present

exact_exact_ppt - AKO_exact_val

5000

Logging roads are the greatest aggravating factor for landslide activity as compared to undisturbed slopes (Jackson 2019).

1. 1.0,7.0

has Transport Line

Road Unclassified Or Unknown

always

unmatched

-10

Roads are aggravating factor for landslide activity as compared to undisturbed slopes (Jackson 2019).

has Transport Line

Trail

sometimes

unmatched

-10

Trails are a aggravating factor for landslide activity as compared to undisturbed slopes (Jackson 2019)

has Transport Line

Trail Skid

always

unmatched

-10

Trail skid are aggravating factor for landslide activity as compared to undisturbed slopes (Jackson 2019).

has Geomorph Process

Erosional Process

present

unmatched

erosional process. rock fall,gully erosion, erosional process,karst. rock fall,gully erosion, erosional process,karst

has Surficial Form

Cliff

present

unmatched

cliff. Falde detritiche di rocce carbonatiche prevalentemente stabilizzate dalla vegetazione,Pianori modellati prevalentemente dall?erosione glaciale o connessi a particolari strutture tettoniche, con superfici debolmente ondulate utilizzate a pascolo, localmen. Falde detritiche di rocce carbonatiche prevalentemente stabilizzate dalla vegetazione,Pianori modellati prevalentemente dall?erosione glaciale o connessi a particolari strutture tettoniche, con superfici debolmente ondulate utilizzate a pascolo, localmen

has Railway

Any Railway

present

unmatched

1

has Bed Rock

limestone

present

unmatched

Calcari e dolomie. Calcari e dolomie,Depositi glaciali. Calcari e dolomie,Depositi glaciali

has Bed Rock

dolomite

present

unmatched

Calcari e dolomie. Calcari e dolomie,Depositi glaciali. Calcari e dolomie,Depositi glaciali

has Geomorph Process

Karst Processes

present

unmatched

karst. rock fall,gully erosion, erosional process,karst. rock fall,gully erosion, erosional process,karst

has Surficial Material

Fluvial Material

present

unmatched

fluvial material. Falde detritiche di rocce carbonatiche prevalentemente stabilizzate dalla vegetazione,Pianori modellati prevalentemente dall?erosione glaciale o connessi a particolari strutture tettoniche, con superfici debolmente ondulate utilizzate a pascolo, localmen. Falde detritiche di rocce carbonatiche prevalentemente stabilizzate dalla vegetazione,Pianori modellati prevalentemente dall?erosione glaciale o connessi a particolari strutture tettoniche, con superfici debolmente ondulate utilizzate a pascolo, localmen

has Water

Lake

present

unmatched

1. Lago di Santa Croce

 

 

 

 

 

 

 

 

 

 

4:05:39 PM - March 7, 2021

MineMatch® Online ©2017-2021 Minerva Intelligence Inc.