[GRASS-SVN] r62233 - grass-addons/grass7/raster/r.droka

Fri Oct 10 03:42:19 PDT 2014

Author: kikapu
Date: 2014-10-10 03:42:19 -0700 (Fri, 10 Oct 2014)
New Revision: 62233

Modified:
   grass-addons/grass7/raster/r.droka/r.droka.html
Log:
r.droka: update

Modified: grass-addons/grass7/raster/r.droka/r.droka.html
===================================================================

--- grass-addons/grass7/raster/r.droka/r.droka.html	2014-10-10 10:17:02 UTC (rev 62232)
+++ grass-addons/grass7/raster/r.droka/r.droka.html	2014-10-10 10:42:19 UTC (rev 62233)
@@ -1,6 +1,4 @@
-<!DOCTYPE html>
 <h1>NAME</h1>
-<meta charset="UTF-8">
 <div><strong>r.droka</strong>- <strong>D</strong>raft <strong>Ro</strong>c<strong>k</strong>fall <strong>A</strong>nalysis – An empirical method that identifies the maximum area of invasion of a rockfall.</div>
 <h1>DESCRIPTION</h1>
 <div><p>The intersection between the topographic profile and the line starting from the point of detachment with a certain angle to the horizontal line defines the point of maximum propagation (Evans and Hungr, 1993; Jaboyedoff and Labiouse, 2003). The angle of inclination (φp) and the line of propagation are defined as zenith angle and shadow zone. This script defines rockfall zones from a digital elevation model (DEM) and vector layer containing starting point or points.</p>
@@ -50,4 +48,3 @@
 <p>JABOYEDOFF M., LABIOUSE V. (2003) - Preliminary assessment of rockfall hazard based on GIS Data. Proceeding of the 10th ISRM Congress, South African Inst. Min. Met., Johannesburg, pp: 575-578</p>
 <p>EVANS, S.G., HUNGR O. (1993). The assessment of rock fall hazard at the base of the talus slope. Can. Geotech. J., 30: 620-636. DOI: 10.1139/t93-054 | © 1993 </p>
 </div>
-</html>

