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 ), Masai lion ( Panthera leo nubica ), 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 North Mediterranean Gibraltar Arc Greater Middle East MENA Middle East Maghreb Barbary Coast Barbara Ancient Libya Atlas Mountains ( Middle Atlas ) Sahara Western Sahara Sahel Eastern Mediterranean Egypt Upper Egypt Middle Egypt Lower Egypt Cataracts of the Nile Bashmur Nubia Lower Nubia Nile Valley Nile Delta Darfur Gulf of Aqaba Sub-Saharan East Aethiopia Swahili coast East African Rift Great Rift Valley Afar Triangle Danakil Desert Danakil Alps Albertine Rift Virunga Mountains Gregory Rift Valley Southern Rift Valley Rift Valley lakes African Great Lakes Mittelafrika Horn of Africa Ethiopian Highlands Gulf of Aden Gulf of Tadjoura Sudan ( region ) Sudanian Savanna East African montane forests Sub-Saharan Central Negroland Guinea region Gulf of Guinea Cape Lopez Mayombe Igboland Mbaise Maputaland Pool Malebo Congo Basin Chad Basin Congolese rainforests Ouaddaï highlands Ennedi Plateau Sub-Saharan West Pepper Coast Gold Coast Slave Coast Ivory Coast Cape Palmas Cape Mesurado Negroland Guinea region Gulf of Guinea Sudanian Savanna Niger Basin Guinean Forests of West Africa Sudan ( region ) Niger Delta Inner Niger Delta Sub-Saharan South 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 Sub-Saharan Anglophone Africa Francophone Africa Lusophone Africa Arabophone Africa Sub-Saharan Africa Tropical Africa Islands Regions of North America Canada Eastern Canada Western Canada Canadian Prairies Central Canada Northern Canada Atlantic Canada The Maritimes French Canada English Canada Acadia Acadian Peninsula Quebec City -- Windsor Corridor Peace River Country Cypress Hills Palliser 's Triangle Canadian Shield Interior Alaska - 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Manchurian grassland Wild Fields Yedisan Muravsky Trail Ural Ural Mountains Volga region Idel - Ural Kolyma Transbaikal Pryazovia Bjarmaland Kuban Zalesye Ingria Novorossiya Gornaya Shoriya Tulgas Iranian Plateau Altai Mountains Pamir Mountains Tian Shan Badakhshan Wakhan Corridor Wakhjir Pass Mount Imeon Mongolian Plateau Western Regions Taklamakan Desert Karakoram Trans - Karakoram Tract Siachen Glacier North Inner Asia Northeast Far East Russian Far East Okhotsk - Manchurian taiga Extreme North Siberia Baikalia ( Lake Baikal ) Transbaikal Khatanga Gulf Baraba steppe Kamchatka Peninsula Amur Basin Yenisei Gulf Yenisei Basin Beringia Sikhote - Alin East Japanese archipelago Northeastern Japan Arc Sakhalin Island Arc Korean Peninsula Gobi Desert Taklamakan Desert Greater Khingan Mongolian Plateau Inner Asia Inner Mongolia Outer Mongolia China proper Manchuria Outer Manchuria Inner Manchuria Northeast China Plain Mongolian - Manchurian grassland North China Plain Yan_Mountains Kunlun Mountains Liaodong Peninsula Himalayas Tibetan Plateau Tibet Tarim Basin Northern Silk Road Hexi Corridor Nanzhong Lingnan Liangguang Jiangnan Jianghuai Guanzhong Huizhou Wu Jiaozhou Zhongyuan Shaannan Ordos Loop Loess Plateau Shaanbei Hamgyong Mountains Central Mountain Range Japanese Alps Suzuka Mountains Leizhou Peninsula Gulf of Tonkin Yangtze River Delta Pearl River Delta Yenisei Basin Altai Mountains Wakhan Corridor Wakhjir Pass West Greater Middle East MENA Middle East Red Sea Caspian Sea Mediterranean Sea Zagros Mountains Persian Gulf Pirate Coast Strait of Hormuz Greater and Lesser Tunbs Al - Faw Peninsula Gulf of Oman Gulf of Aqaba Gulf of Aden Balochistan Arabian Peninsula Najd Hejaz Tihamah Eastern Arabia South Arabia Hadhramaut Arabian Peninsula coastal fog desert Tigris -- Euphrates Mesopotamia Upper Mesopotamia Lower Mesopotamia Sawad Nineveh plains Akkad ( region ) Babylonia Canaan Aram Eber - Nari Suhum Eastern Mediterranean Mashriq Kurdistan Levant Southern Levant Transjordan Jordan Rift Valley Levantine Sea Golan Heights Hula Valley Gaza Strip West Bank Galilee Gilead Judea Samaria Arabah Anti-Lebanon Mountains Sinai Peninsula Arabian Desert Syrian Desert Fertile Crescent Azerbaijan Syria Palestine Iranian Plateau Armenian Highlands Caucasus Caucasus Mountains Greater Caucasus Lesser Caucasus North Caucasus South Caucasus Kur - Araz Lowland Lankaran Lowland Alborz Absheron Peninsula Anatolia Cilicia Cappadocia Alpide belt South Greater India Indian subcontinent Himalayas Hindu Kush Western Ghats Eastern Ghats Ganges Basin Ganges Delta Pashtunistan Punjab Balochistan Kashmir Kashmir Valley Pir Panjal Range Thar Desert Indus Valley Indus River Delta Indus Valley Desert Indo - Gangetic Plain Eastern coastal plains Western Coastal Plains Meghalaya subtropical forests Lower Gangetic plains moist deciduous forests Northwestern Himalayan alpine shrub and meadows Doab Bagar tract Great Rann of Kutch Little Rann of Kutch Deccan Plateau Coromandel Coast Konkan False Divi Point Hindi Belt Ladakh Aksai Chin Gilgit - Baltistan Baltistan Shigar Valley Karakoram Saltoro Mountains Siachen Glacier Bay of Bengal Gulf of Khambhat Gulf of Kutch Gulf of Mannar Trans - Karakoram Tract Wakhan Corridor Wakhjir Pass Lakshadweep Andaman and Nicobar Islands Andaman Islands Nicobar Islands Maldive Islands Alpide belt Southeast Mainland Indochina Malay Peninsula Maritime Peninsular Malaysia Sunda Islands Greater Sunda Islands Lesser Sunda Islands Indonesian Archipelago Timor New Guinea Bonis Peninsula Papuan Peninsula Huon Peninsula Huon Gulf Bird 's Head Peninsula Gazelle Peninsula Philippine Archipelago Luzon Visayas Mindanao Leyte Gulf Gulf of Thailand East Indies Nanyang Alpide belt Asia - 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Larsen Sea Ross Sea Scotia Sea Somov Sea Weddell Sea Endorheic basins Aral Sea Caspian Sea Dead Sea Sea of Galilee 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=802476528 '' 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 26 September 2017, at 11 : 34. 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Question: where is ethiopian highlands located on a map
Answer: central and northern Ethiopia, and its northernmost portion reaches into Eritrea