Difference between revisions of "Tectonic-Geomorphic-Climatic Interaction (NSF-EAR-1324637, 1323137)"

Latest revision as of 14:21, 13 April 2018

Click the text links below to explore the different sections of this project:

Subduction Zone Dynamics in the Mantle and at the Earth's Surface	The role of surface displacement in landscape evolution	The role of rock mass strength in landscape evolution

Connections between rock mass strength and grain size in alluvium	The combined influence of rock damage and surface displacement in landscape evolution	educational tools

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-Tectonic-Geomorphic-Climatic Interaction (NSF-EAR-1324637, 1323137)
+<div style="font-size:110%">
+'''Click the text links below to explore the different sections of this project:'''
-    a) [[The role of surface displacement in landscape evolution]]
+{| class="wikitable"
+|-
-    b) [[The role of rock mass strength in landscape evolution]]
+! style="width:400px" | [[Subduction Zone Dynamics in the Mantle and at the Earth's Surface]]
+! style="width:400px" | [[The role of surface displacement in landscape evolution]]
-    c) [[Connections between rock mass strength and grain size in alluvium]]
+! style="width:400px" | [[The role of rock mass strength in landscape evolution]]
+|-
-    d) [[the combined influence of rock damage and surface displacement in landscape evolution]]
+| [[File:mantle_hook.jpg|400px]]
+| [[File:kin_crop.jpg|400px]]
+| [[File:faultero_crop.jpg|400px]]
+|-
+! style="width:400px" | [[Connections between rock mass strength and grain size in alluvium]]
+! style="width:400px" | [[The combined influence of rock damage and surface displacement in landscape evolution]]
+! style="width:400px" | [[educational tools]]
+|-
+| [[File:tx_crop.jpg|400px]]
+| [[File:dyn_crop.jpg|400px]]
+| [[File:ed_crop.jpg|400px]]
+|}
+</div>