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Geologic Process Identification through Landform Analysis
Ian Thomsen
Topographic Position Index
From Jenness 2006
Inherently Scalable Adjusts to capture features of different scales
• Quickly
• Easily
• Repeatable
Jenness, 2006
• Comparing elevation of each cell to the mean of all cells in an annulus of radius 100 cells (3000 meters) around it.
• Only interested in large, regional-scale features
Raster Calculator
Slope Tool
TPI < -6 = Canyon bottom
-4 < TPI < 3 , Slope < 12° = Gentle Slope
-4 < TPI < 3 ; Slope > 12° = Steep Slope
3 < TPI < 6 = Steep Slope
6 < TPI = Ridge top
Raster Calculator
Focal Statistics Operations
Areas of statistical operation can be customized to the scale of interest
For example: • 4500m square window
discards signal from smaller features
• 19500m window only captures largest features
Identify all points which are classed as Steep Slope or Ridge Top at 4500x4500m scale but only class as Shallow Slope at 19500x19500m scale • Filters out all features too large to be fault generated • Removes smaller topographic relief
Raster Calculator
Pamir
Results
• Method successfully marks landforms which match characteristics of fault scarp structures
• Successfully removes other topography from consideration
But…
• Issues of scale
Results
• Defines SOME topographic relief as fault related, but not all
• MORE problems of scale
Results Obvious problems:
• Where are the faults?! They SHOULD be around here!
Two possibilities:
• There is no fault here
Or
• The scale of features of interest is lost in more recent features
Problems identifying fault features with TPI
Extremely scale dependent
Scale must be uniform
Difficult to detect topography of interest within other geologic/erosional features
Implications of work
Check the accuracy of map data
Identify sites where fault-generated features are more and less likely to be found
Can be applied to any geological features whose scale can be isolated from “background” topography
Future work
Develop statistical methods to quickly combine
TPI
Lithologic changes
Seismic activity
Test method accuracy in the field
Refine algorithm
Apply TPI analysis to other geologic mapping projects