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Agerbi'a
Lim’at is a '' tabia'' in the Dogu'a Tembien district of the Tigray Region of Ethiopia. The ''tabia'' centre is in Maygwa village, located approximately 8 km to the southwest of the ''woreda'' town Hagere Selam. Geography The ''tabia'' stretches down from the Tsatsen plateau (2810 m a.s.l.), across the main road towards Zeleqwa (Upper Tanqwa) river (2270 m a.s.l.). Geology From the higher to the lower locations, the following geological formations are present: * Upper basalt * Interbedded lacustrine deposits * Lower basalt * Amba Aradam Formation * Antalo Limestone * Quaternary alluvium and freshwater tufa Geomorphology and soils The main geomorphic unit is the Hagere Selam Highlands. Corresponding soil types are: * Associated soil types ** shallow soils with high stone contents (Skeletic Cambisol, Leptic Cambisol, Skeletic Regosol) ** moderately deep dark stony clays with good natural fertility (Vertic Cambisol) ** deep, dark cracking clays, tempora ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ethiopia
Ethiopia, , om, Itiyoophiyaa, so, Itoobiya, ti, ኢትዮጵያ, Ítiyop'iya, aa, Itiyoppiya officially the Federal Democratic Republic of Ethiopia, is a landlocked country in the Horn of Africa. It shares borders with Eritrea to the north, Djibouti to the northeast, Somalia to the east and northeast, Kenya to the south, South Sudan to the west, and Sudan to the northwest. Ethiopia has a total area of . As of 2022, it is home to around 113.5 million inhabitants, making it the 13th-most populous country in the world and the 2nd-most populous in Africa after Nigeria. The national capital and largest city, Addis Ababa, lies several kilometres west of the East African Rift that splits the country into the African and Somali tectonic plates. Anatomically modern humans emerged from modern-day Ethiopia and set out to the Near East and elsewhere in the Middle Paleolithic period. Southwestern Ethiopia has been proposed as a possible homeland of the Afroasiatic langua ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Regosol
A Regosol in the World Reference Base for Soil Resources (WRB) is very weakly developed mineral soil in unconsolidated materials. Regosols are extensive in eroding lands, in particular in arid and semi-arid areas and in mountain regions. Internationally, Regosols correlate with soil taxa that are marked by incipient soil formation such as Entisols in the USDA soil taxonomy or Rudosols and possibly some Tenosols in the Australian Soil Classification. The group of Regosols is a taxonomic rest group containing all soils that could not be accommodated in any of the other groups. Excluded from the Regosols are weakly developed soils that classify as Leptosols (very shallow soils), Arenosols (sandy soils) or Fluvisols (in recent alluvial deposits). These soils have AC- profiles. Profile development is minimal as a consequence of young age and/or slow soil formation. Land use and management of Regosols vary widely. Some Regosols are used for capital-intensive irrigated farming but th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Degol Woyane
Degol Woyane is a ''tabia'' or municipality in the Dogu'a Tembien district of the Tigray Region of Ethiopia. It includes Dabba Selama, the oldest monastery of Ethiopia, and the most inaccessible in the world. The ''tabia'' centre is in Zala village, located approximately 10 km to the west of the ''woreda'' town Hagere Selam. Geography The ''tabia'' stretches down west of Melfa, along the westernmost ridge of Dogu'a Tembien. The highest peak is T'afa (2580 m a.s.l.) and the lowest place Addi Welo (1990 m a.s.l.). Geology From the higher to the lower locations, the following geological formations are present: * Lower basalt * Amba Aradam Formation * Adigrat Sandstone Springs As there are no permanent rivers, the presence of springs is of utmost importance for the local people. The following are the springs in the tabia: * May Dara in Zala * Addi Welo Livelihood The population lives essentially from crop farming, supplemented with off-season work in nearby towns. T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aregen
Aregen is a ''tabia'' or municipality in the Dogu'a Tembien district of the Tigray Region of Ethiopia. The ''tabia'' centre is in Addi Gotet village, located approximately to the west-southwest of the ''woreda'' town Hagere Selam. Geography The ''tabia'' occupies an elongated ridge between the gorges of Upper Tanqwa and Tsech'i Rivers. The highest peak is near Aregen village ( a.s.l.) and the lowest place at the confluence of the two rivers ( a.s.l.). Geology From the higher to the lower locations, the following geological formations are present: * Lower basalt * Amba Aradam Formation * Antalo Limestone * Adigrat Sandstone Geomorphology and soils The main geomorphic units, with corresponding soil types are: * Hagere Selam Highlands, along the central basalt and sandstone ridge ** Associated soil types *** shallow soils with high stone contents (Skeletic Cambisol, Leptic Cambisol, Skeletic Regosol) *** moderately deep dark stony clays with good natural fertility (Ver ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Melfa (Dogu'a Tembien)
Dogu'a Tembien Melfa is a ''tabiya'' or municipality in the Dogu'a Tembien district of the Tigray Region of Ethiopia and ancient capital of Tembien. The ''tabia'' centre is Melfa village itself, located approximately 3 km to the west of the ''woreda'' town Hagere Selam. Geography The ''tabia'' stretches down from the ridge at 2700 m a.s.l. towards Zelekwa/Ruba Dirho River (2150 m a.s.l.). Geology From the higher to the lower locations, the following geological formations are present: * Upper basalt * Interbedded lacustrine deposits * Lower basalt * Amba Aradam Formation * Antalo Limestone Geomorphology and soils The main geomorphic unit is the Hagere Selam Highlands. Corresponding soil types are: * Associated soil types ** shallow soils with high stone contents (Skeletic Cambisol, Leptic Cambisol, Skeletic Regosol) ** moderately deep dark stony clays with good natural fertility (Vertic Cambisol) ** deep, dark cracking clays, temporarily waterlogged during th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drainage System (geomorphology)
In geomorphology, drainage systems, also known as river systems, are the patterns formed by the streams, rivers, and lakes in a particular drainage basin. They are governed by the topography of land, whether a particular region is dominated by hard or soft rocks, and the gradient of the land. Geomorphologists and hydrologists often view streams as part of drainage basins (and sub-basins). This is the topographic region from which a stream receives runoff, throughflow, and its saturated equivalent, groundwater flow. The number, size, and shape of the drainage basins varies and the larger and more detailed the topographic map, the more information is available. Drainage patterns Per the lie of channels, drainage systems can fall into one of several categories, known as drainage patterns. These depend on the topography and geology of the land. All forms of transitions can occur between parallel, dendritic, and trellis patterns. Accordant versus discordant drainage patterns A drai ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nile
The Nile, , Bohairic , lg, Kiira , Nobiin language, Nobiin: Áman Dawū is a major north-flowing river in northeastern Africa. It flows into the Mediterranean Sea. The Nile is the longest river in Africa and has historically been considered the List of rivers by length, longest river in the world, though this has been contested by research suggesting that the Amazon River is slightly longer.Amazon Longer Than Nile River, Scientists Say Of the world's major rivers, the Nile is one of the smallest, as measured by annual flow in cubic metres of water. About long, its drainage basin covers eleven countries: the Democratic Republic of the Congo, Tanzania, Burundi, Rwanda, Uganda, Kenya, Ethiopia, Erit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tekezé River
The Tekezé or Täkkäze River ( amh, ተከዜ, ti, ተከዘ; originally meaning "river" in Ge’ez, ), also spelled Takkaze, is a major river of Ethiopia. For part of its course it forms a section of the westernmost border of Ethiopia and Eritrea. The river is also known as the Setit () in Eritrea, western Ethiopia, and eastern Sudan. According to materials published by the Ethiopian Central Statistical Agency, the Tekezé River is long. The canyon which it has created is the deepest in Africa and one of the deepest in the world, at some points having a depth of over 2000 meters (6,562 feet). Course The Tekezé River rises in the central Ethiopian Highlands near Mount Qachen within Lasta, from where it flows west, north, then west again, forming the westernmost border of Ethiopia and Eritrea from the confluence of the Tomsa with the Tekezé at to the tripoint between the two countries and Sudan at . After entering northeastern Sudan at the tripoint it joins the Atbarah ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Luvisol
Luvisols are a group of soils, comprising one of the 32 Reference Soil Groups in the international system of soil classification, the World Reference Base for Soil Resources The World Reference Base for Soil Resources (WRB) is an international soil classification system for naming soils and creating legends for soil maps. The currently valid version is the fourth edition 2022. It is edited by a working group of the Inte ... (WRB). They are widespread, especially in temperate climates, and are generally fertile. Luvisols are widely used for agriculture. Distribution Luvisols cover 500–600 million ha of land area, mainly in the temperate zones. They form on a wide variety of mineral parent materials. In Mediterranean regions, the formation of hematite can produce red-coloured Chromic Luvisols. Description and formation The main characteristic of Luvisols is an argic horizon, a subsurface zone with higher clay content than the material above it. This typically arises as clay is was ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loam
Loam (in geology and soil science) is soil composed mostly of sand (particle size > ), silt (particle size > ), and a smaller amount of clay (particle size < ). By weight, its mineral composition is about 40–40–20% concentration of sand–silt–clay, respectively. These proportions can vary to a degree, however, and result in different types of loam soils: sandy loam, silty loam, clay loam, sandy clay loam, silty clay loam, and loam. In the , textural classification triangle, the only soil that is not predominantly sand, silt, or clay is called "loam". Loam soils generally contain more nutrients, moisture, and |
Leptosol
A Leptosol in the World Reference Base for Soil Resources (WRB) is a very shallow soil over hard rock or a deeper soil that is extremely gravelly and/or stony. Leptosols cover approximately 1.7 billion hectares of the Earth's surface. They are found from the tropics to the cold polar regions and from sea level to the highest peaks. Leptosols are particularly widespread in mountain areas, notably in Asia, South America, northern Canada and Alaska; and in the Saharan and Arabian deserts. Elsewhere, Leptosols can be found on hard rocks or where erosion has kept pace with soil formation or removed the top of the soil. In the FAO soil classification for the UNESCO Soil Map of the World (1974) the Leptosols on calcareous rock were called Rendzinas, those on acid rock were Rankers. The very shallow, less than 10 cm deep, ''Lithic Leptosols'' in mountain regions are the most extensive Leptosols on Earth. Leptosols are unattractive soils for rainfed agriculture because of their inab ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
