AAU-ETD AAU-ETD
 

Addis Ababa University Libraries Electronic Thesis and Dissertations: AAU-ETD! >
Faculty of Science >
Thesis - Earth Sciences >

Please use this identifier to cite or link to this item: http://hdl.handle.net/123456789/2708

Title: GEOLOGICAL FACTORS GOVERNING the VULNERABILITY of LAND to DEGRADATION: - the case of HOSAINA – WERABE AREA, USING REMOTE SENSING and GIS
Authors: MEERAPH, HABTEWOLD
Advisors: Dr Mohammed Umer
Copyright: Jul-2006
Date Added: 6-May-2012
Abstract: Abstract The study area, Hosaina-Werabe, is situated in the western margin of the main Ethiopian rift valley. It is structurally controlled and tectonically active. It is covered by loose ash falls, weak pumice layers, and less welded tuff layers, which are vulnerable to land degradation activities, and are intercalated with relatively stronger ignimbrite layers. Whereas the lithologies and geological structures make the area vulnerable to land degradation, the steep slopes at fault escarpments and volcanic domes accelerate the erosive power of overland flows and /or rivers. The main land degradation process is erosion by water. The land degradation activity in the area is assessed using integrated remote sensing and GIS techniques and field survey. The rate of land degradation, in areal bases, has been estimated using Landsat satellite images of the years 1973, 1984, 2000 G. C. on a small sample site of about 247 sq km. area, which was a subset from the study area. The average rate of land degradation from the year 1984 to 1973 is 0.7 sq. km / year and from the year 1984 to 2000, it is 1.0 sq. km / year. The result shows a general increasing trend of land degradation. The areal extent of degraded land is also increasing over time. In the year 1973, it was 7.3 %, in the year 1984, it rose to 10.4 % and it was extended to 16.7 % in the year 2000 G. C. xiv Cross-tabulation of two year images at a time, indicated that few parts of the formerly degraded areas were seen to be covered by vegetation. However, newly formed degraded lands have shown prominent areal expansion through time. Land degradation vulnerability factor maps were produced from topographic maps, existing maps, Landsat satellite data and SRTM (Shuttle Radar Topographic Mission) data. GIS analyses of distance and area measurements, slope, and reclassification were done for each factor based on their relation with land degradation activity. These layers were standardized and weights were given in a hierarchical order. Finally multi-criteria analysis was done that indicated areas susceptible to land degradation. It was reclassified in order to produce three classes of vulnerability map for the study area. Accordingly, factors that are responsible for making the area vulnerable to land degradation are, in decreasing order of importance: drainage, slope, geological structure, geology (lithology), soil and land use/ land cover.
URI: http://hdl.handle.net/123456789/2708
Appears in:Thesis - Earth Sciences

Files in This Item:

File Description SizeFormat
MEERAPH HABTEWOLD.pdf6.13 MBAdobe PDFView/Open

Items in the AAUL Digital Library are protected by copyright, with all rights reserved, unless otherwise indicated.

 

  Last updated: May 2010. Copyright © Addis Ababa University Libraries - Feedback