Eritrean Highlands: Difference between revisions
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[[Image:Eritrean Highlands.jpg|thumb|[[Teff]] field at the base of a small hill in the Eritrean Highlands.]] |
[[Image:Eritrean Highlands.jpg|thumb|[[Teff]] field at the base of a small hill in the Eritrean Highlands.]] |
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The '''Eritrean Highlands''' are a mountainous region in central Eritrea that are bordered to the south by the Mereb River. The region has seen tremendous [[deforestation]] since the Italian Colonial period which began in the late 19th century. The Highlands are at particular risk of deforestation and associated soil erosion. Furthermore the region, lying south of the [[Sahel]] are at particular risk of desertification and frequent drought. The Highlands experience, as most tropical regions, two seasons; the rainy season (''kremti'') is from June-September while the dry season is from September to June. The average temperature for the Highlands is approximately 16°C. The tallest pointed in [[Eritrea]] is located in the Eritrean Highlands at [[Amba Soira]]. |
The '''Eritrean Highlands''' are a mountainous region in central Eritrea that are bordered to the south by the Mereb River. It is a continuation of the [[Ethiopian Highlands]] to the south. The region has seen tremendous [[deforestation]] since the Italian Colonial period which began in the late 19th century. The Highlands are at particular risk of deforestation and associated soil erosion. Furthermore the region, lying south of the [[Sahel]] are at particular risk of desertification and frequent drought. The Highlands experience, as most tropical regions, two seasons; the rainy season (''kremti'') is from June-September while the dry season is from September to June. The average temperature for the Highlands is approximately 16°C. The tallest pointed in [[Eritrea]] is located in the Eritrean Highlands at [[Amba Soira]]. |
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The Eritrean Highlands are drained by four major rivers towards [[Sudan]] and by several smaller rivers into the [[Red Sea]] coast of [[Eritrea]]. Flowing towards Sudan and the [[Nile River]] are the [[Gash River|Gash]] and [[Setit River|Setit]] Rivers while towards Sudan without reaching the Nile are the [[Barka River|Barka]] and [[Anseba River|Anseba]] Rivers. The Eastern Escarpment of Eritrea is drained by numerous small streams. |
The Eritrean Highlands are drained by four major rivers towards [[Sudan]] and by several smaller rivers into the [[Red Sea]] coast of [[Eritrea]]. Flowing towards Sudan and the [[Nile River]] are the [[Gash River|Gash]] and [[Setit River|Setit]] Rivers while towards Sudan without reaching the Nile are the [[Barka River|Barka]] and [[Anseba River|Anseba]] Rivers. The Eastern Escarpment of Eritrea is drained by numerous small streams. |
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Many believe that forest cover in the Eritrean Highlands was as high 30% but has since declined to 1%,<ref>{{cite paper | author = Boerma, Pauline | title =Assessing Forest Cover Change in Eritrea — A Historical Perspective | publisher =Mountain Research and Development | url =http://www.mrd-journal.org/pdf/Boerma_MRED26_1_pp41-47.pdf | format =PDF | accessdate =2007-01-17}} {{Dead link|date=October 2010|bot=H3llBot}}</ref> however, others including Louise Latt have suggested that there has never been such a dramatic decline in forest cover.<ref>{{cite paper | author = Louise Latt | title = Eritrea Re-photographed: Landscape Changes in the Eritrean Highlands 1890-2004 | format = PDF | url = http://www.cde.unibe.ch/University/pdf/TTD/Laett_Eritrea.pdf | accessdate = 2006-09-26}}</ref> |
Many believe that forest cover in the Eritrean Highlands was as high as 30% but has since declined to 1%,<ref>{{cite paper | author = Boerma, Pauline | title =Assessing Forest Cover Change in Eritrea — A Historical Perspective | publisher =Mountain Research and Development | url =http://www.mrd-journal.org/pdf/Boerma_MRED26_1_pp41-47.pdf | format =PDF | accessdate =2007-01-17}} {{Dead link|date=October 2010|bot=H3llBot}}</ref> however, others including Louise Latt have suggested that there has never been such a dramatic decline in forest cover.<ref>{{cite paper | author = Louise Latt | title = Eritrea Re-photographed: Landscape Changes in the Eritrean Highlands 1890-2004 | format = PDF | url = http://www.cde.unibe.ch/University/pdf/TTD/Laett_Eritrea.pdf | accessdate = 2006-09-26}}</ref> |
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[[Image:Eritrean Baboon.jpg|thumb|[[Baboon]] crossing a road in the Eritrean Highlands.]] |
[[Image:Eritrean Baboon.jpg|thumb|[[Baboon]] crossing a road in the Eritrean Highlands.]] |
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The eastern edge of the Highlands falls off dramatically towards the [[Red Sea]] which causes two climatic systems to overlap. This region is oft noted for its perennial forest cover. This is also the region that Eritrea's Merara coffee is grown. |
The eastern edge of the Highlands falls off dramatically towards the [[Red Sea]] which causes two climatic systems to overlap. This region is oft noted for its perennial forest cover. This is also the region that Eritrea's Merara coffee is grown. |
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Revision as of 00:44, 4 April 2013
The Eritrean Highlands are a mountainous region in central Eritrea that are bordered to the south by the Mereb River. It is a continuation of the Ethiopian Highlands to the south. The region has seen tremendous deforestation since the Italian Colonial period which began in the late 19th century. The Highlands are at particular risk of deforestation and associated soil erosion. Furthermore the region, lying south of the Sahel are at particular risk of desertification and frequent drought. The Highlands experience, as most tropical regions, two seasons; the rainy season (kremti) is from June-September while the dry season is from September to June. The average temperature for the Highlands is approximately 16°C. The tallest pointed in Eritrea is located in the Eritrean Highlands at Amba Soira.
The Eritrean Highlands are drained by four major rivers towards Sudan and by several smaller rivers into the Red Sea coast of Eritrea. Flowing towards Sudan and the Nile River are the Gash and Setit Rivers while towards Sudan without reaching the Nile are the Barka and Anseba Rivers. The Eastern Escarpment of Eritrea is drained by numerous small streams.
Many believe that forest cover in the Eritrean Highlands was as high as 30% but has since declined to 1%,[1] however, others including Louise Latt have suggested that there has never been such a dramatic decline in forest cover.[2]
The eastern edge of the Highlands falls off dramatically towards the Red Sea which causes two climatic systems to overlap. This region is oft noted for its perennial forest cover. This is also the region that Eritrea's Merara coffee is grown.
The soil conditions in the Eritrean Highlands is also quite complex. The predominant soils are chromic, eutric, and calsic cambisols of strong red colour. Other soils found in the highlands are lithosols, xerosols and fluvisols.[3]
See also
References
- ^ Boerma, Pauline. "Assessing Forest Cover Change in Eritrea — A Historical Perspective" (PDF). Mountain Research and Development. Retrieved 2007-01-17.
{{cite journal}}: Cite journal requires|journal=(help) [dead link] - ^ Louise Latt. "Eritrea Re-photographed: Landscape Changes in the Eritrean Highlands 1890-2004" (PDF). Retrieved 2006-09-26.
{{cite journal}}: Cite journal requires|journal=(help) - ^ "FOSA Country Report". Retrieved 2007-01-17.
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