[GRASS-SVN] r62235 - grass-addons/grass7/raster/r.droka

[svn_grass at osgeo.org]

Author: kikapu
Date: 2014-10-10 05:03:42 -0700 (Fri, 10 Oct 2014)
New Revision: 62235

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 11:58:16 UTC (rev 62234)
+++ grass-addons/grass7/raster/r.droka/r.droka.html	2014-10-10 12:03:42 UTC (rev 62235)
@@ -1,11 +1,11 @@
-<h1>NAME</h1>
+<h2>NAME</h2>
 <dl>
-<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.
-<h1>DESCRIPTION</h1>
+<dt><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.</dt>
+<h2>DESCRIPTION</h2>
 <dt>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.</dt>
 <dt><a><img src="img.png" width="401" height="227" alt=""><a></dt>
 <dt><strong><span style="font-size: smaller;">Energy line used for the cone method from the top or the bottom of a cliff (shadow angle), according to various authors (Image from Jaboyedoff and Labiouse, 2003)</span></strong></dt>
-<h1>INPUT</h1>
+<h2>INPUT</h2>
 
 
 <dt><strong>Digital Elevation Model</strong> = name </dt>
@@ -26,7 +26,7 @@
     <ul>This value define the radius for randomly generatin boulders starting from starting point. It's in the option dialog window.</ul>
 
 
-<h1>OUTPUT</h1>
+<h2>OUTPUT</h2>
 <dt><strong>r.droka generates 5 raster maps and a vector map.</strong> The names of all output maps start with the prefix defined by the parameter prefix followed by name of map</dt>
 <ul>
     <li><em>prefix</em>_propagation: raster map rapresenting the area of propagation. If are used multiple source points, each pixel show the percentage of passage (%)</li>
@@ -37,15 +37,14 @@
     <li><em>prefix</em>_starting: vector map of starting points</li>
 </ul>
 
+<h2>REFERENCES</h2>
+<dt>FILIPELLO A., GIULIANI A., MANDRONE G. (2010) - Rock Slopes Failure Susceptibility Analysis: From Remote Sensing Measurements to Geographic Information System Raster Modules. American Journal of Environmental Sciences 6 (6): 489-494, 2010 ISSN 1553-345X © 2010 Science Publications.</dt>
+<dt>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</dt>
+<dt>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 </dt>
 
+<h2>SEE ALSO</h2>
 
-<h1>AUTHORS</h1>
+<h2>AUTHORS</h2>
 <dt>Andrea Filipello, University of Turin, Italy - <a href="mailto:andrea.filipello at gmail.com">Email</a> </dt>
 <dt>Daniele Strigaro, University of Milan, Italy -  <a href="mailto:daniele.strigaro at gmail.com">Email</a></dt>
 
-
-<h1>REFERENCES</h1>
-<dt>FILIPELLO A., GIULIANI A., MANDRONE G. (2010) - Rock Slopes Failure Susceptibility Analysis: From Remote Sensing Measurements to Geographic Information System Raster Modules. American Journal of Environmental Sciences 6 (6): 489-494, 2010 ISSN 1553-345X © 2010 Science Publications.</dt>
-<dt>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</dt>
-<dt>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 </dt>
-