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Golis Mountains
The Golis Mountains are a mountain range in Somaliland. Also known as ''Qar Golis'', they cut through the Togdheer region, and end near the Gan Libah. Jerato Pass This range has a mountain pass known as the "Jerrato Pass". See also * Cal Madow Cal Madow (also Calmadow, Al Madow, Al Medu, or Al Mado; so, Buuraha Calmadow; ar, عَلَمْدُو, ʿAlamdū) is a mountain range in Somaliland. It stretches across an area between the east of Erigavo, Somaliland, to the Bari region of So ... References External links * Mountain ranges Mountain ranges of Africa Mountain ranges of Somaliland Togdheer {{Somaliland-geo-stub ...
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Togdheer
Togdheer ( so, Togdheer, ar, تُوْجْدَيْر, Tūjdayr) is an administrative region ('' gobol'') in central Somaliland. Togdheer is bordered by Maroodi Jeex to the west, Saaxil to the north, Sanaag to the northeast, Sool to the east and Ethiopia to the south. Its capital is Burao. Overview Togdheer is bordered by Maroodi Jeex from the west, Sahil to the north, Ethiopia to the south, and Sanaag & Sool to the east. With its capital at Burao (Burco), the region's name is derived from the Togdheer River, which means "Long River" in Somali. The region has an approximate population of 350,000 people. Under British Somaliland, the Togdheer region was formerly the Burao district which was one of three districts that comprised the Burao region. The other two regions were Las Anod and Erigavo districts. Sanaag was carved out of Togdheer region and was established as a separate region on June 23, 1973, comprising the three districts of Erigavo, Las Qorey and Garadag. As ...
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Mountain Range
A mountain range or hill range is a series of mountains or hills arranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form, structure, and alignment that have arisen from the same cause, usually an orogeny. Mountain ranges are formed by a variety of geological processes, but most of the significant ones on Earth are the result of plate tectonics. Mountain ranges are also found on many planetary mass objects in the Solar System and are likely a feature of most terrestrial planets. Mountain ranges are usually segmented by highlands or mountain passes and valleys. Individual mountains within the same mountain range do not necessarily have the same geologic structure or petrology. They may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, and volcanic landforms resulting in a variety of rock types. Major ranges Most geolo ...
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Somaliland
Somaliland,; ar, صوماليلاند ', ' officially the Republic of Somaliland,, ar, جمهورية صوماليلاند, link=no ''Jumhūrīyat Ṣūmālīlānd'' is a ''de facto'' sovereign state in the Horn of Africa, still considered internationally to be part of Somalia. Somaliland lies in the Horn of Africa, on the southern coast of the Gulf of Aden. It is bordered by Djibouti to the northwest, Ethiopia to the south and west, and Somalia to the east.Encyclopædia Britannica, ''The New Encyclopædia Britannica'', (Encyclopædia Britannica: 2002), p.835 Its claimed territory has an area of , with approximately 5.7 million residents as of 2021. The capital and largest city is Hargeisa. The government of Somaliland regards itself as the successor state to British Somaliland, which, as the briefly independent State of Somaliland, united in 1960 with the Trust Territory of Somaliland (the former Italian Somaliland) to form the Somali Republic.''The New Encyclopæ ...
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Gaanlibah
Gaanlibah or Ga'an Libah ( so, Gacan Libaax) is mountain range, archaeological site, and national park located in the Maroodi Jeex region of Somaliland. Nearby are the Golis Mountains. Its upper slopes are the source of the seasonal Togdheer river that flows through the city of Burao into the Nugaal Valley. Overview Gaanlibah is not far from Laas Geel and around east of the provincial capital Hargeisa. It is in the western part of the northern mountains, which extend east and west parallel to the northern coast of the Horn of Africa. Flora and fauna The natural vegetation includes evergreen and semi-evergreen bushland and thicket at lower elevations, dominated by the shrub '' Buxus hildebrandtii'', which cover approximately 20,000 ha. Woodlands of African juniper (''Juniperus procera'') and other Afromontane plant communities occur at higher elevations, and cover about 30,000 ha.BirdLife International (2022) Important Bird Areas factsheet: Gacan Libaax. Downloaded from http:/ ...
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John Murray (publishing House)
John Murray is a British publisher, known for the authors it has published in its long history including, Jane Austen, Sir Arthur Conan Doyle, Lord Byron, Charles Lyell, Johann Wolfgang von Goethe, Herman Melville, Edward Whymper, Thomas Malthus, David Ricardo, and Charles Darwin. Since 2004, it has been owned by conglomerate Lagardère under the Hachette UK brand. Business publisher Nicholas Brealey became an imprint of John Murray in 2015. History The business was founded in London in 1768 by John Murray (1737–1793), an Edinburgh-born Royal Marines officer, who built up a list of authors including Isaac D'Israeli and published the ''English Review''. John Murray the elder was one of the founding sponsors of the London evening newspaper ''The Star'' in 1788. He was succeeded by his son John Murray II, who made the publishing house important and influential. He was a friend of many leading writers of the day and launched the '' Quarterly Review'' in 1809. He was the ...
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Mountain Pass
A mountain pass is a navigable route through a mountain range or over a ridge. Since many of the world's mountain ranges have presented formidable barriers to travel, passes have played a key role in trade, war, and both human and animal migration throughout history. At lower elevations it may be called a hill pass. A mountain pass is typically formed between two volcanic peaks or created by erosion from water or wind. Overview Mountain passes make use of a gap, saddle, col or notch. A topographic saddle is analogous to the mathematical concept of a saddle surface, with a saddle point marking the highest point between two valleys and the lowest point along a ridge. On a topographic map, passes are characterized by contour lines with an hourglass shape, which indicates a low spot between two higher points. In the high mountains, a difference of between the summit and the mountain is defined as a mountain pass. Passes are often found just above the source of a river ...
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Cal Madow
Cal Madow (also Calmadow, Al Madow, Al Medu, or Al Mado; so, Buuraha Calmadow; ar, عَلَمْدُو, ʿAlamdū) is a mountain range in Somaliland. It stretches across an area between the east of Erigavo, Somaliland, to the Bari region of Somalia. Its peak sits at almost in Shimbiris, northwest of Erigavo. Cal Madow was a tourist destination in the late 1980s. The local population of the Sanaag region is primarily responsible for preserving the habitat, which continues to face the risk of deforestation. Ecology The dense mountain forest sits at an altitude of between above sea level, and has a mean annual rainfall of . In addition to rainfall, Cal Madow receives additional precipitation in the form of fog and winter rains, which sustain isolated forests of '' Juniperus procera, Buxus hildebrandtii'', and others. Mist also appears to be important in the distribution of juniperus (''dayib''), one of the species locals use for timber. For timber production, the buxus (''d ...
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Mountain Ranges
A mountain range or hill range is a series of mountains or hills arranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form, structure, and alignment that have arisen from the same cause, usually an orogeny. Mountain ranges are formed by a variety of geological processes, but most of the significant ones on Earth are the result of plate tectonics. Mountain ranges are also found on many planetary mass objects in the Solar System and are likely a feature of most terrestrial planets. Mountain ranges are usually segmented by highlands or mountain passes and valleys. Individual mountains within the same mountain range do not necessarily have the same geologic structure or petrology. They may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, and volcanic landforms resulting in a variety of rock types. Major ranges Most geologically ...
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Mountain Ranges Of Africa
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ...
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Mountain Ranges Of Somaliland
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ...
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