commit e022ce02cb8c4c106b9a9a2752ec785d122d79ec
parent 2bf98ea43e81f5e8f16b011ca93caf89accb9720
Author: Anders Damsgaard <anders@adamsgaard.dk>
Date: Fri, 12 Apr 2019 09:36:01 +0200
Fix table formatting
Diffstat:
1 file changed, 5 insertions(+), 7 deletions(-)
diff --git a/README.md b/README.md
@@ -29,13 +29,11 @@ probably be improved further.
The rheology is of Bingham type, where no deformation occurs beneath the Mohr-Coulomb yield limit. Above it, deformation is highly non-linearly viscous. The model has a parameter *b* for rate dependence beyond yield. Glass beads have *b* = 0.94.
-| Subglacial till | Continuum Model |
-| --------------------------------------- | --------------- |
-| Upstream-B (Kamb 1991) | |
+| Real material (laboratory of field study) | Continuum Model |
+| ----------------------------------------- | --------------- |
+| Upstream-B (Kamb 1991) | |
|  |  |
-| --------------------------------------- | --------------- |
-| Various subglacial tills (Iverson 2010) | |
+| Various subglacial tills (Iverson 2010): | |
|  |  |
-| --------------------------------------- | --------------- |
-| Whillans Ice Plain (Tulaczyk 2006) | |
+| Whillans Ice Plain (Tulaczyk 2006): | |
|  |  |