Ethiopian Highlands - wikipedia Ethiopian Highlands Ethiopian Highlands The Semien Mountains with the tallest peak Ras Dashen ( 4,550 m ) in the Ethiopian Highlands are a World Heritage Site and include the Semien Mountains National Park Highest point Elevation 4,550 m ( 14,930 ft ) Parent peak Mount Tullu Demtu Geography Topographic map Location Ethiopia Geology Age of rock 75 million years Mountain type Mountain range The Ethiopian Highlands is a rugged mass of mountains in Ethiopia, situated in the Horn region in Northeast Africa. It forms the largest continuous area of its altitude in the continent, with little of its surface falling below 1500 m ( 4,921 ft ), while the summits reach heights of up to 4550 m ( 14,928 ft ). It is sometimes called the Roof of Africa due to its height and large area. Most of the Ethiopian Highlands are part of central and northern Ethiopia, and its northernmost portion reaches into Eritrea. Contents 1 History 2 Physical geography 3 Geology 4 Climate 5 Ecology 6 Fauna 7 See also 8 References 9 External links History A coffee cup from the era of the Kaffa Kingdom In the southern parts of the Ethiopian Highlands once was located the Kingdom of Kaffa, a medieval early modern state, whence the coffee plant was exported to the Arabian peninsula. The land of the former kingdom is mountainous with stretches of forest. The land is very fertile, capable of three harvests a year. The term `` coffee '' derives from the Arabic qahwah ( قهوة ) and is traced to Kaffa. Physical geography The Highlands are divided into northwestern and southeastern portions by the Main Ethiopian Rift, which contains a number of salt lakes. The northwestern portion, which covers the Tigray and Amhara Regions, includes the Semien Mountains, part of which has been designated the Semien Mountains National Park. Its summit, Ras Dashan ( 4550 m ), is the highest peak in Ethiopia. Lake Tana, the source of the Blue Nile, also lies in the northwestern portion of the Ethiopian Highlands. The southeastern portion 's highest peaks are located in the Bale Zone of Ethiopia 's Oromia Region. The Bale Mountains, also designated a national park, are nearly as high as those of Semien. The range includes peaks of over 4000 m. Among these are Mount Tullu Demtu ( 4337 m ), which is the second - highest peak in Ethiopia, and Mount Batu ( 4307 m ). Most of the country 's major cities are located at elevations of around 2,000 -- 2,500 m ( 6,562 -- 8,202 ft ) above sea level, including historic capitals such as Gondar and Axum. Geology Dendi Caldera, a collapsed volcano in the mountain region The Ethiopian Highlands began to rise 75 million years ago, as magma from the Earth 's mantle uplifted a broad dome of the ancient rocks of the Arabian - Nubian Shield. The opening of the Great Rift Valley split the dome of the Ethiopian Highlands into three parts ; the mountains of the southern Arabian Peninsula are geologically part of the ancient Ethiopian Highlands, separated by the rifting which created the Red Sea and Gulf of Aden and separated Africa from Arabia. Around 30 million years ago, a flood basalt plateau began to form, piling layers upon layers of voluminous fissure - fed basaltic lava flows. Most of the flows were tholeiitic, save for a thin layer of alkali basalts and minor amounts of felsic ( high - silica ) volcanic rocks, such as rhyolite. In the waning stages of the flood basalt episode, large explosive caldera - forming eruptions also occurred. The Ethiopian Highlands were eventually bisected by the Great Rift Valley as the African continental crust pulled apart. This rifting gave rise to large alkaline basalt shield volcanoes beginning about 30 -- 31 million years ago. Climate Main article : Climate of Ethiopia The predominant climate type of the Ethiopian Highlands is tropical monsoon, and have a climate which is generally considerably cooler than other regions at similar proximity to the Equator. Ecology Ethiopian Highlands with Ras Dashan in the background Because the highlands elevate Ethiopia, located close to the equator, this has resulted in giving this country an unexpectedly temperate climate. Further, these mountains catch the precipitation of the monsoon winds of the Indian Ocean, resulting in a rainy season that lasts from June until mid-September. These heavy rains cause the Nile to flood in the summer, a phenomenon that puzzled the ancient Greeks, as the summer is the driest season in the Mediterranean climate that they knew. The Ethiopian Highlands share a similar flora and fauna of other mountainous regions of Africa ; this distinctive flora and fauna is known as Afromontane but from the time of the last Ice Age has been populated with some Eurasian ( palearctic ) flora. The habitats are somewhat different on either side of the Great Rift Valley that splits the highlands. At lower elevations, the highlands are surrounded by tropical savannas and grasslands, including the Sahelian Acacia savanna to the northwest, the East Sudanian Savanna to the west, and the Somali Acacia - Commiphora bushlands and thickets to the northeast, east, south, and through the Rift Valley. The highlands themselves are divided into three distinct ecoregions, distinguished by elevation. The Ethiopian montane forests lie between 1,100 and 1,800 meters elevation, above the lowland grasslands and savannas and extends to areas of similar habitat in Eritrea, Sudan, and Djibouti. This woodland belt has several natural plant communities, but has mostly been heavily grazed and converted to agricultural use now. Kolla, is an open woodland found at lower elevations, and dominated by species of Terminalia, Commiphora, Boswellia, and Acacia. Weyna dega is a woodland found in moister and higher locations, dominated by the conifers Afrocarpus gracilior and Juniperus procera. The lower portion of the Harenna Forest is a distinct woodland community, with an open canopy of Warburgia ugandensis, Croton macrostachyus, and Syzygium guineese, and Afrocarpus gracilior, with wild coffee ( Coffea arabica ) as the dominant understory shrub. The southwesterly winds bring rainfall from May to October with moisture from the Red Sea coming in from the east year round. Fauna at these elevations includes the endemic Harwood 's francolin ( Francolinus harwoodi ), Prince Ruspoli 's turaco ( Tauraco ruspolii ) and yellow - throated seedeater ( Serinus flavigula ), along with the Djibouti francolin ( Francolinus ochropectus ) in the Djibouti hills that are in the same general ecoregion. The Ethiopian montane grasslands and woodlands is the largest of the highland ecoregions, occupying the area between 1800 and 3000 meters elevations. The natural vegetation was closed - canopy forest in moister areas, and grassland, bushland, and thicket in drier areas. However these hillsides have good fertile soil and are heavily populated, largely by farming communities so most of the region has been converted to agriculture with a few areas of natural vegetation remaining. Urban areas in this ecoregion include : Ethiopia 's capital city and Africa 's fourth largest city Addis Ababa, the Amhara Region capital Bahir Dar with its island monasteries on Lake Tana, the old walled city of Harar, the spa town of Ambo, Asella in the Arsi Zone, the trekking center of Dodola, the lakeside Debre Zeyit, the largest city in the southwest Jimma, the market town of Nekemte, and the capital of the Tigray Region, Mek'ele. Awash National Park is a site for birdwatching. Remaining woodland in the drier areas contains much endemic flora and primarily consists of Podocarpus conifers and Juniperus procera, often with Hagenia abyssinica. In the Harenna Forest, pockets of moist, closed - canopy forest with Pouteria and Olea are draped with lianas and epiphytes, while above 2400 metres, a shrubby zone is home to Hagenia, Schefflera, and giant lobelias ( Lobelia gibberroa ), species which can be found on the East African mountains further south. The evergreen broadleaved forest of the Semien Mountains, between 2,300 and 2,700 meters elevation, is dominated by Syzygium guineense, Juniperus procera, and Olea africana. As the lower slopes of the mountains are so heavily populated even the high altitude moorlands are affected by human interference, such as the grazing of livestock and even farming. There are two protected areas of high moorland : Bale Mountains National Park in the southern highlands, accessible from Dinsho ; and Semien Mountains National Park, accessible from Gondar, which includes Ras Dashen. However even these parks are losing habitat to livestock grazing, while the lower elevation parks ( Harar Wildlife Sanctuary, Awash National Park, Omo National Park, and Nechisar National Park ) are even less secure. Fauna These slopes are home to a number of endemic reptiles, birds and animals including the endangered walia ibex ( Capra walie ) and the gelada baboon, whose thick fur allows it to thrive in the cooler climates of the mountains. These two species are only found on the northern side of the valley while another rare endemic the mountain nyala ( Tragelaphus buxtoni ) is restricted to the southern side, and now survives at higher altitudes than its original habitat as the lower slopes are heavily farmed. More widespread mammals found here include the mantled guereza ( Colobus guereza ), which is also threatened as its habitat disappears as is that of many other mammals of the highlands such as olive baboon ( Papio anubis ), Egyptian wolf ( Canis aureus lupaster ), African leopard ( Panthera pardus pardus ), East African lion ( Panthera leo melanochaita ), spotted hyena ( Crocuta crocuta ), caracal ( Caracal caracal ), serval ( Felis serval ), common duiker ( Sylvicapra grimmia ) and red river hog ( Potamochoerus porcus ). Birds include Rueppell 's chat, the finch Ankober serin ( Serinus ankoberensis ), white - winged flufftail ( Sarothrura ayresi ), and blue - winged goose. The farmland is home to many butterflies, especially Papilio, Charaxinae, Pieridae and Lycaenidae. Above 3000 meters elevation lie the high Ethiopian montane moorlands, the largest afroalpine region in Africa. The montane moorlands lie above the tree line, and consist of grassland and moorland with abundant herbs and some shrubs that have adapted to the high mountain conditions. There are several endemic animal species one of which, the Ethiopian wolf ( Canis simensis ), is critically endangered. Other endemics include the big - headed mole - rat ( Tachyoryctes macrocephalus ) which is common on the Sanetti Plateau in the Bale Mountains. The mountain nyala finds its way up to the high moorlands although it is more common at lower elevations. Wintering birds include wigeon ( Anas penelope ), shoveler ( Anas clypeata ), ruff ( Philomachus pugnax ) and greenshank ( Tringa nebularia ). Other fauna in the area also includes aardvark, eagle, Ethiopian wolf, Egyptian wolf, gelada, secretary bird, Nubian ibex, and marabou stork and Ethiopian endemic species such as the shrew, Crocidura harenna and the narrow - footed woodland mouse ( Grammomys minnae ) and Menelik 's bushbuck ( Tragelaphus scriptus meneliki ), which is a subspecies with long, dark fur. See also Geography of Ethiopia Wildlife of Ethiopia References Jump up ^ Paul B. Henze, Layers of Time ( New York : Palgrave, 2000 ), p. 2. ^ Jump up to : Oxford English Dictionary, 1st ed. `` coffee, n. '' Oxford University Press ( Oxford ), 1891. Jump up ^ Weinberg & Bealer 2001, p. 25 Jump up ^ January 2005 : The Ethiopian Large Igneous Province Jump up ^ An explanation of this unusual rain pattern can be found at Ethiopia : Drought intensifies during corn and sorghum harvest ( ReliefWeb ) Jump up ^ http://worldwildlife.org/ecoregions/at0112 External links `` Ethiopian montane forests ''. Terrestrial Ecoregions. World Wildlife Fund. `` Ethiopian montane grasslands and woodlands ''. Terrestrial Ecoregions. World Wildlife Fund. `` Ethiopian montane moorlands ''. Terrestrial Ecoregions. World Wildlife Fund. Ethiopian Wolf Conservation Programme List of ecoregions in Africa Sovereign states Algeria Angola Benin Botswana Burkina Faso Burundi Cameroon Cape Verde ( Cabo Verde ) Central African Republic Chad Comoros Democratic Republic of the Congo Republic of the Congo Djibouti Egypt Equatorial Guinea Eritrea Ethiopia Gabon The Gambia Ghana Guinea Guinea - Bissau Ivory Coast ( Côte d'Ivoire ) Kenya Lesotho Liberia Libya Madagascar Malawi Mali Mauritania Mauritius Morocco Mozambique Namibia Niger Nigeria Rwanda São Tomé and Príncipe Senegal Seychelles Sierra Leone Somalia South Africa South Sudan Sudan Swaziland Tanzania Togo Tunisia Uganda Zambia Zimbabwe States with limited recognition Sahrawi Arab Democratic Republic Somaliland Dependencies and other territories Canary Islands / Ceuta / Melilla / ( see also plazas de soberanía ) ( Spain ) Madeira ( Portugal ) Mayotte / Réunion ( France ) Saint Helena / Ascension Island / Tristan da Cunha ( United Kingdom ) Western Sahara Major African geological formations Plates African Plate Somali Plate Madagascar Plate Seychelles Plate Cratons and shields Arabian - Nubian Shield Congo Craton Kaapvaal Craton Kalahari Craton Saharan Metacraton Tanzania Craton Tuareg Shield West African Craton Zimbabwe Craton Shear zones Aswa Dislocation Broodkop Shear Zone Central African Shear Zone Chuan Shear Zones Foumban Shear Zone Kandi Fault Zone Mwembeshi Shear Zone Todi Shear Zone Western Meseta Shear Zone Orogens Alpide Orogen Cape Fold Belt Damara Orogen East African Orogen Eburnean Orogen Gondwanide Orogen Kibaran Orogen Kuunga Orogen Mauritanide Belt Pan-African orogens Terra Australis Orogen Rifts Afar Triangle Anza trough Bahr el Arab rift Benue Trough Blue Nile rift East African Rift Gulf of Suez Rift Lamu Embayment Melut Basin Muglad Basin Red Sea Rift Sangha Aulacogen Atbara rift White Nile rift Sedimentary basins Angola Basin Aoukar Blue Nile Basin Chad Basin Congo Basin Douala Basin El Djouf Foreland Karoo Basin Gabon Basin Iullemmeden Basin Kufra Basin Murzuq Basin Niger Delta Basin Ogaden Basin Orange River basin Ouled Abdoun Basin Owambo Basin Reggane Basin Rio del Rey Basin Sirte Basin Somali Coastal Basin Taoudeni basin Tanzania Coastal Basin Tindouf Basin Turkana Basin Mountain ranges Aïr Mountains Atlas Mountains Aurès Mountains Bambouk Mountains Blue Mountains Cameroon line Central Pangean Mountains Chaillu Mountains Drakensberg Ethiopian Highlands East African mountains Great Escarpment Great Karas Mountains Guinée forestière Imatong Mountains Jebel Uweinat Loma Mountains Mandara Mountains Marrah Mountains Mitumba Mountains Nuba Mountains Rif Mountains Rwenzori Mountains Sankwala Mountains Serra da Leba Serra da Chela Teffedest Mountains Tibesti Mountains Large igneous provinces Agulhas Plateau ( Northeast Georgia Rise, Maud Rise ) Brazilian Highlands Caribbean Central Atlantic Circum - Superior Columbia River Deccan Emeishan Ethiopian and Yemen Highlands Franklin ( Franklin dike swarm ) High Arctic ( Sverdrup Basin ) Karoo - Ferrar Kerguelen ( Broken Ridge ) Marathon Keweenawan Long Range Mackenzie ( Coppermine River Mackenzie dike swarm ) Matachewan Mistassini North Atlantic Ontong Java - Manihiki - Hikurangi Panjal Paraná and Etendeka Shatsky Siberian Skagerrak Ungava Winagami Regions of the world Regions of Africa Central Africa Guinea region Gulf of Guinea Cape Lopez Mayombe Igboland Mbaise Maputaland Pool Malebo Congo Basin Chad Basin Congolese rainforests Ouaddaï highlands Ennedi Plateau East Africa African Great Lakes Albertine Rift East African Rift Great Rift Valley Gregory Rift Rift Valley lakes Swahili coast Virunga Mountains Zanj Horn of Africa Afar Triangle Al - Habash Barbara Danakil Alps Danakil Desert Ethiopian Highlands Gulf of Aden Gulf of Tadjoura Indian Ocean islands Comoros Islands North Africa Maghreb Barbary Coast Bashmur Ancient Libya Atlas Mountains Nile Valley Cataracts of the Nile Darfur Gulf of Aqaba Lower Egypt Lower Nubia Middle Egypt Nile Delta Nuba Mountains Nubia The Sudans Upper Egypt Western Sahara West Africa Pepper Coast Gold Coast Slave Coast Ivory Coast Cape Palmas Cape Mesurado Guinea region Gulf of Guinea Niger Basin Guinean Forests of West Africa Niger Delta Inner Niger Delta Southern Africa Madagascar Central Highlands ( Madagascar ) Northern Highlands Rhodesia North South Thembuland Succulent Karoo Nama Karoo Bushveld Highveld Fynbos Cape Floristic Region Kalahari Desert Okavango Delta False Bay Hydra Bay Macro-regions Aethiopia Arab world Commonwealth realm East African montane forests Eastern Desert Equatorial Africa Françafrique Gibraltar Arc Greater Middle East Islands of Africa List of countries where Arabic is an official language Mediterranean Basin MENA Middle East Mittelafrika Negroland Northeast Africa Portuguese - 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Larsen Sea Ross Sea Scotia Sea Somov Sea Weddell Sea Landlocked seas Aral Sea Caspian Sea Dead Sea Salton Sea Book Coordinates : 12 ° 32 ′ 00 '' N 41 ° 23 ′ 8 '' E ﻿ / ﻿ 12.53333 ° N 41.38556 ° E ﻿ / 12.53333 ; 41.38556 Retrieved from `` https://en.wikipedia.org/w/index.php?title=Ethiopian_Highlands&oldid=809345040 '' Categories : Ethiopian Highlands Regions of Africa Mountain ranges of Ethiopia Geography of Ethiopia Forests of Ethiopia Afromontane ecoregions Ecoregions of Ethiopia Ecoregions of Sudan Amhara Region Geography of Oromia Region Tigray Region Large igneous provinces Oligocene volcanism Oligocene Africa Ecoregions of Africa Plateaus of Africa Highlands Hidden categories : All articles with unsourced statements Articles with unsourced statements from January 2014 Coordinates on Wikidata Talk Contents About Wikipedia Asturianu Беларуская Български Català Cebuano Čeština Deutsch Eesti Ελληνικά Español Esperanto Euskara فارسی Français 한국어 Հայերեն हिन्दी Hrvatski Bahasa Indonesia Italiano עברית ქართული Қазақша Lietuvių Magyar Македонски Nederlands 日本 語 Norsk Norsk nynorsk Polski Português Русский Slovenčina Српски / srpski Srpskohrvatski / српскохрватски Suomi Türkçe Українська اردو 粵語 中文 Edit links This page was last edited on 8 November 2017, at 15 : 09. 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Question: where is the ethiopian highlands located on a map
Answer: central and northern Ethiopia, and its northernmost portion reaches into Eritrea