en.unionpedia.org

Laterite, the Glossary

Index Laterite

Laterite is a soil type rich in iron and aluminium and is commonly considered to have formed in hot and wet tropical areas.[1]

Table of Contents

  1. 132 relations: Alpine orogeny, Aluminium, Aluminium oxide, Amphibole, Anatase, Angkor Wat, Aquifer, Augite, Australian Shield, Basalt, Basement (geology), Bauxite, Bitumen, Boehmite, Brazil, Burkina Faso, Cadmium, Calcite, Calcium, Capillary action, Cation-exchange capacity, Cementation (geology), Chalcedony, Chromium, Clay, Clay mineral, Cliff Ollier, Climate, Cobalt, Continental collision, Craton, Cretaceous, Diaspore, Dolomite (mineral), Dry season, Duricrust, Feldspar, Ferricrete, Francis Buchanan-Hamilton, French colonial empire, Gabbro, Geografiska Annaler, Gibbsite, Gneiss, Goethite, Granite, Granitoid, Halloysite, Hematite, Hydroxide, ... Expand index (82 more) »

  2. Ore deposits
  3. Regolith
  4. Soil-based building materials
  5. Weathering

Alpine orogeny

The Alpine orogeny or Alpide orogeny is an orogenic phase in the Late Mesozoic (Eoalpine) and the current Cenozoic that has formed the mountain ranges of the Alpide belt.

See Laterite and Alpine orogeny

Aluminium

Aluminium (Aluminum in North American English) is a chemical element; it has symbol Al and atomic number 13.

See Laterite and Aluminium

Aluminium oxide

Aluminium oxide (or aluminium(III) oxide) is a chemical compound of aluminium and oxygen with the chemical formula.

See Laterite and Aluminium oxide

Amphibole

Amphibole is a group of inosilicate minerals, forming prism or needlelike crystals, composed of double chain tetrahedra, linked at the vertices and generally containing ions of iron and/or magnesium in their structures.

See Laterite and Amphibole

Anatase

Anatase is a metastable mineral form of titanium dioxide (TiO2) with a tetragonal crystal structure.

See Laterite and Anatase

Angkor Wat

Angkor Wat (អង្គរវត្ត, "City/Capital of Temples") is a Hindu-Buddhist temple complex in Cambodia.

See Laterite and Angkor Wat

Aquifer

An aquifer is an underground layer of water-bearing material, consisting of permeable or fractured rock, or of unconsolidated materials (gravel, sand, or silt).

See Laterite and Aquifer

Augite

Augite, also known as Augurite, is a common rock-forming pyroxene mineral with formula.

See Laterite and Augite

Australian Shield

The Australian Shield is a geological feature known as a shield that occupies more than half of the continent of Australia.

See Laterite and Australian Shield

Basalt

Basalt is an aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the surface of a rocky planet or moon.

See Laterite and Basalt

Basement (geology)

In geology, basement and crystalline basement are crystalline rocks lying above the mantle and beneath all other rocks and sediments.

See Laterite and Basement (geology)

Bauxite

Bauxite is a sedimentary rock with a relatively high aluminium content. Laterite and Bauxite are aluminium minerals, Regolith and Weathering.

See Laterite and Bauxite

Bitumen

Bitumen is an immensely viscous constituent of petroleum. Laterite and Bitumen are building materials.

See Laterite and Bitumen

Boehmite

Boehmite or böhmite is an aluminium oxide hydroxide (γ-AlO(OH)) mineral, a component of the aluminium ore bauxite. Laterite and Boehmite are aluminium minerals.

See Laterite and Boehmite

Brazil

Brazil, officially the Federative Republic of Brazil, is the largest and easternmost country in South America and Latin America.

See Laterite and Brazil

Burkina Faso

Burkina Faso is a landlocked country in West Africa.

See Laterite and Burkina Faso

Cadmium

Cadmium is a chemical element; it has symbol Cd and atomic number 48.

See Laterite and Cadmium

Calcite

Calcite is a carbonate mineral and the most stable polymorph of calcium carbonate (CaCO3).

See Laterite and Calcite

Calcium

Calcium is a chemical element; it has symbol Ca and atomic number 20.

See Laterite and Calcium

Capillary action

Capillary action (sometimes called capillarity, capillary motion, capillary rise, capillary effect, or wicking) is the process of a liquid flowing in a narrow space in opposition to or at least without the assistance of any external forces like gravity.

See Laterite and Capillary action

Cation-exchange capacity

Cation-exchange capacity (CEC) is a measure of how many cations can be retained on soil particle surfaces.

See Laterite and Cation-exchange capacity

Cementation (geology)

Cementation involves ions carried in groundwater chemically precipitating to form new crystalline material between sedimentary grains. Laterite and Cementation (geology) are Sedimentology.

See Laterite and Cementation (geology)

Chalcedony

Chalcedony is a cryptocrystalline form of silica, composed of very fine intergrowths of quartz and moganite.

See Laterite and Chalcedony

Chromium

Chromium is a chemical element; it has symbol Cr and atomic number 24.

See Laterite and Chromium

Clay

Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolinite, Al2Si2O5(OH)4). Laterite and clay are Sedimentology and soil-based building materials.

See Laterite and Clay

Clay mineral

Clay minerals are hydrous aluminium phyllosilicates (e.g. kaolin, Al2Si2O5(OH)4), sometimes with variable amounts of iron, magnesium, alkali metals, alkaline earths, and other cations found on or near some planetary surfaces.

See Laterite and Clay mineral

Cliff Ollier

Cliff Ollier (born 26 October 1931) is a geologist, geomorphologist, soil scientist, emeritus professor and honorary research fellow, at the School of Earth and Geographical Sciences University of Western Australia.

See Laterite and Cliff Ollier

Climate

Climate is the long-term weather pattern in a region, typically averaged over 30 years.

See Laterite and Climate

Cobalt

Cobalt is a chemical element; it has symbol Co and atomic number 27.

See Laterite and Cobalt

Continental collision

In geology, continental collision is a phenomenon of plate tectonics that occurs at convergent boundaries.

See Laterite and Continental collision

Craton

A craton (or; from κράτος "strength") is an old and stable part of the continental lithosphere, which consists of Earth's two topmost layers, the crust and the uppermost mantle.

See Laterite and Craton

Cretaceous

The Cretaceous is a geological period that lasted from about 145 to 66 million years ago (Mya).

See Laterite and Cretaceous

Diaspore

Diasporealso called diasporite, empholite, kayserite, or tanatariteis an aluminium hydroxide oxide mineral, α-AlO(OH), crystallizing in the orthorhombic system and isomorphous with goethite. Laterite and diaspore are aluminium minerals.

See Laterite and Diaspore

Dolomite (mineral)

Dolomite is an anhydrous carbonate mineral composed of calcium magnesium carbonate, ideally The term is also used for a sedimentary carbonate rock composed mostly of the mineral dolomite (see Dolomite (rock)).

See Laterite and Dolomite (mineral)

Dry season

The dry season was a yearly period of low rainfall, especially in the tropics.

See Laterite and Dry season

Duricrust

Duricrust is a hard layer on or near the surface of soil.

See Laterite and Duricrust

Feldspar

Feldspar (sometimes spelled felspar) is a group of rock-forming aluminium tectosilicate minerals, also containing other cations such as sodium, calcium, potassium, or barium.

See Laterite and Feldspar

Ferricrete

Ferricrete is a hard, erosion-resistant layer of sedimentary rock, usually conglomerate or breccia, that has been cemented into a duricrust by iron oxides. Laterite and Ferricrete are pedology.

See Laterite and Ferricrete

Francis Buchanan-Hamilton

Francis Buchanan (15 February 1762 – 15 June 1829), later known as Francis Hamilton but often referred to as Francis Buchanan-Hamilton, was a Scottish surgeon, surveyor and botanist who made significant contributions as a geographer and zoologist while living in India.

See Laterite and Francis Buchanan-Hamilton

French colonial empire

The French colonial empire comprised the overseas colonies, protectorates, and mandate territories that came under French rule from the 16th century onward.

See Laterite and French colonial empire

Gabbro

Gabbro is a phaneritic (coarse-grained), mafic intrusive igneous rock formed from the slow cooling of magnesium-rich and iron-rich magma into a holocrystalline mass deep beneath the Earth's surface.

See Laterite and Gabbro

Geografiska Annaler

Geografiska Annaler is a scientific journal published by the Swedish Society for Anthropology and Geography in Stockholm, Sweden.

See Laterite and Geografiska Annaler

Gibbsite

Gibbsite, Al(OH)3, is one of the mineral forms of aluminium hydroxide. Laterite and Gibbsite are aluminium minerals.

See Laterite and Gibbsite

Gneiss

Gneiss is a common and widely distributed type of metamorphic rock.

See Laterite and Gneiss

Goethite

Goethite is a mineral of the diaspore group, consisting of iron(III) oxide-hydroxide, specifically the α-polymorph.

See Laterite and Goethite

Granite

Granite is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase.

See Laterite and Granite

Granitoid

A granitoid is a generic term for a diverse category of coarse-grained igneous rocks that consist predominantly of quartz, plagioclase, and alkali feldspar.

See Laterite and Granitoid

Halloysite

Halloysite is an aluminosilicate clay mineral with the empirical formula Al2Si2O5(OH)4. Laterite and Halloysite are aluminium minerals.

See Laterite and Halloysite

Hematite

Hematite, also spelled as haematite, is a common iron oxide compound with the formula, Fe2O3 and is widely found in rocks and soils.

See Laterite and Hematite

Hydroxide

Hydroxide is a diatomic anion with chemical formula OH−.

See Laterite and Hydroxide

Igneous rock

Igneous rock, or magmatic rock, is one of the three main rock types, the others being sedimentary and metamorphic.

See Laterite and Igneous rock

India

India, officially the Republic of India (ISO), is a country in South Asia.

See Laterite and India

International Crops Research Institute for the Semi-Arid Tropics

The International Crops Research Institute for the Semi-Arid Tropics (ICRISAT) is an international organisation which conducts agricultural research for rural development, headquartered in Patancheru, Hyderabad, Telangana, India, with several regional centres (Bamako (Mali), Nairobi (Kenya)) and research stations (Niamey (Niger), Kano (Nigeria), Lilongwe (Malawi), Addis Ababa (Ethiopia), Bulawayo (Zimbabwe)).

See Laterite and International Crops Research Institute for the Semi-Arid Tropics

Inverted relief

Inverted relief, inverted topography, or topographic inversion refers to landscape features that have reversed their elevation relative to other features.

See Laterite and Inverted relief

Ion

An ion is an atom or molecule with a net electrical charge.

See Laterite and Ion

Iron

Iron is a chemical element. Laterite and Iron are building materials.

See Laterite and Iron

Iron oxide

Iron oxides are chemical compounds composed of iron and oxygen.

See Laterite and Iron oxide

Island arc

Island arcs are long chains of active volcanoes with intense seismic activity found along convergent tectonic plate boundaries.

See Laterite and Island arc

Kaolinite

Kaolinite (also called kaolin) is a clay mineral, with the chemical composition: Al2Si2O5(OH)4. Laterite and Kaolinite are aluminium minerals.

See Laterite and Kaolinite

Khmer Empire

The Khmer Empire was a Hindu-Buddhist empire in Southeast Asia, centered around hydraulic cities in what is now northern Cambodia.

See Laterite and Khmer Empire

Latin

Latin (lingua Latina,, or Latinum) is a classical language belonging to the Italic branch of the Indo-European languages.

See Laterite and Latin

Leachate

A leachate is any liquid that, in the course of passing through matter, extracts soluble or suspended solids, or any other component of the material through which it has passed.

See Laterite and Leachate

Leaching (pedology)

In pedology, leaching is the removal of soluble materials from one zone in soil to another via water movement in the profile. Laterite and leaching (pedology) are Sedimentology.

See Laterite and Leaching (pedology)

Lead

Lead is a chemical element; it has symbol Pb (from Latin plumbum) and atomic number 82.

See Laterite and Lead

Limestone

Limestone (calcium carbonate) is a type of carbonate sedimentary rock which is the main source of the material lime.

See Laterite and Limestone

Madhya Pradesh

Madhya Pradesh (meaning 'central province') is a state in central India.

See Laterite and Madhya Pradesh

Mafic

A mafic mineral or rock is a silicate mineral or igneous rock rich in magnesium and iron.

See Laterite and Mafic

Magnesite

Magnesite is a mineral with the chemical formula (magnesium carbonate).

See Laterite and Magnesite

Magnesium

Magnesium is a chemical element; it has symbol Mg and atomic number 12.

See Laterite and Magnesium

Manganese

Manganese is a chemical element; it has symbol Mn and atomic number 25.

See Laterite and Manganese

Manganese oxide

Manganese oxide is any of a variety of manganese oxides and hydroxides.

See Laterite and Manganese oxide

Masonry

Masonry is the craft of building a structure with brick, stone, or similar material, including mortar plastering which are often laid in, bound, and pasted together by mortar. Laterite and Masonry are building materials.

See Laterite and Masonry

Mesozoic

The Mesozoic Era is the penultimate era of Earth's geological history, lasting from about, comprising the Triassic, Jurassic and Cretaceous Periods.

See Laterite and Mesozoic

Metamorphic rocks arise from the transformation of existing rock to new types of rock in a process called metamorphism.

See Laterite and Metamorphic rock

Migmatite

Migmatite is a composite rock found in medium and high-grade metamorphic environments, commonly within Precambrian cratonic blocks.

See Laterite and Migmatite

Mineral

In geology and mineralogy, a mineral or mineral species is, broadly speaking, a solid substance with a fairly well-defined chemical composition and a specific crystal structure that occurs naturally in pure form.

See Laterite and Mineral

Mineralogy

Mineralogy is a subject of geology specializing in the scientific study of the chemistry, crystal structure, and physical (including optical) properties of minerals and mineralized artifacts.

See Laterite and Mineralogy

Monsoon

A monsoon is traditionally a seasonal reversing wind accompanied by corresponding changes in precipitation but is now used to describe seasonal changes in atmospheric circulation and precipitation associated with annual latitudinal oscillation of the Intertropical Convergence Zone (ITCZ) between its limits to the north and south of the equator.

See Laterite and Monsoon

National Polytechnic Institute of Toulouse

Toulouse Institute of Technology (also called National Polytechnic Institute of Toulouse or INPT) is a French university cluster based in Toulouse, France, part of University of Toulouse.

See Laterite and National Polytechnic Institute of Toulouse

Nickel

Nickel is a chemical element; it has symbol Ni and atomic number 28.

See Laterite and Nickel

Nickel mining in New Caledonia

Nickel mining in New Caledonia is a major sector of the New Caledonian economy.

See Laterite and Nickel mining in New Caledonia

Niger

Niger or the Niger, officially the Republic of the Niger, is a country in West Africa.

See Laterite and Niger

Northern Ireland

Northern Ireland (Tuaisceart Éireann; Norlin Airlann) is a part of the United Kingdom in the north-east of the island of Ireland that is variously described as a country, province or region.

See Laterite and Northern Ireland

Olivine

The mineral olivine is a magnesium iron silicate with the chemical formula.

See Laterite and Olivine

Ore

Ore is natural rock or sediment that contains one or more valuable minerals concentrated above background levels, typically containing metals, that can be mined, treated and sold at a profit.

See Laterite and Ore

Oxide

An oxide is a chemical compound containing at least one oxygen atom and one other element in its chemical formula.

See Laterite and Oxide

Parent rock

In the earth sciences, parent rock, also sometimes substratum, is the original rock from which younger rock or soil is formed. Laterite and parent rock are Regolith.

See Laterite and Parent rock

Peridotite

Peridotite is a dense, coarse-grained igneous rock consisting mostly of the silicate minerals olivine and pyroxene.

See Laterite and Peridotite

PH

In chemistry, pH, also referred to as acidity or basicity, historically denotes "potential of hydrogen" (or "power of hydrogen").

See Laterite and PH

Pisolite

A pisolite is a sedimentary rock made of pisoids, which are concretionary grains – typically of calcium carbonate which resemble ooids, but are more than 2 mm in diameter.

See Laterite and Pisolite

Plagioclase

Plagioclase is a series of tectosilicate (framework silicate) minerals within the feldspar group. Laterite and Plagioclase are aluminium minerals.

See Laterite and Plagioclase

Plateau

In geology and physical geography, a plateau (plateaus or plateaux), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side.

See Laterite and Plateau

Potassium

Potassium is a chemical element; it has symbol K (from Neo-Latin kalium) and atomic number19.

See Laterite and Potassium

Precambrian

The Precambrian (or Pre-Cambrian, sometimes abbreviated pC, or Cryptozoic) is the earliest part of Earth's history, set before the current Phanerozoic Eon.

See Laterite and Precambrian

Pyroxene

The pyroxenes (commonly abbreviated Px) are a group of important rock-forming inosilicate minerals found in many igneous and metamorphic rocks.

See Laterite and Pyroxene

Quartz

Quartz is a hard, crystalline mineral composed of silica (silicon dioxide).

See Laterite and Quartz

Quaternary

The Quaternary is the current and most recent of the three periods of the Cenozoic Era in the geologic time scale of the International Commission on Stratigraphy (ICS).

See Laterite and Quaternary

Regolith

Regolith is a blanket of unconsolidated, loose, heterogeneous superficial deposits covering solid rock. Laterite and Regolith are pedology and Sedimentology.

See Laterite and Regolith

Sahel

The Sahel region or Sahelian acacia savanna is a biogeographical region in Africa.

See Laterite and Sahel

Salt (chemistry)

In chemistry, a salt or ionic compound is a chemical compound consisting of an assembly of positively charged ions (cations) and negatively charged ions (anions), which results in a compound with no net electric charge (electrically neutral).

See Laterite and Salt (chemistry)

Sandstone

Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains, cemented together by another mineral.

See Laterite and Sandstone

Saprolite

Saprolite is a chemically weathered rock. Laterite and Saprolite are ore deposits, pedology, Regolith, Sedimentology and Weathering.

See Laterite and Saprolite

Savanna

A savanna or savannah is a mixed woodland-grassland (i.e. grassy woodland) biome and ecosystem characterised by the trees being sufficiently widely spaced so that the canopy does not close.

See Laterite and Savanna

Schist

Schist is a medium-grained metamorphic rock showing pronounced schistosity.

See Laterite and Schist

Sea surface temperature

Sea surface temperature (or ocean surface temperature) is the temperature of ocean water close to the surface.

See Laterite and Sea surface temperature

Sedimentary rock

Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation.

See Laterite and Sedimentary rock

Sesquioxide

A sesquioxide is an oxide of an element (or radical), where the ratio between the number of atoms of that element and the number of atoms of oxygen is 2:3.

See Laterite and Sesquioxide

Silcrete

Silcrete is an indurated (resists crumbling or powdering) soil duricrust formed when surface soil, sand, and gravel are cemented by dissolved silica.

See Laterite and Silcrete

Silicon oxide

Silicon oxide may refer to either of the following.

See Laterite and Silicon oxide

Smallholding

A smallholding or smallholder is a small farm operating under a small-scale agriculture model.

See Laterite and Smallholding

Sodium

Sodium is a chemical element; it has symbol Na (from Neo-Latin natrium) and atomic number 11.

See Laterite and Sodium

Soil horizon

A soil horizon is a layer parallel to the soil surface whose physical, chemical and biological characteristics differ from the layers above and beneath. Laterite and soil horizon are pedology.

See Laterite and Soil horizon

Steppe

In physical geography, a steppe is an ecoregion characterized by grassland plains without closed forests except near rivers and lakes.

See Laterite and Steppe

Subsoil

Subsoil is the layer of soil under the topsoil on the surface of the ground.

See Laterite and Subsoil

Sudbury Basin

The Sudbury Basin, also known as Sudbury Structure or the Sudbury Nickel Irruptive, is a major geological structure in Ontario, Canada.

See Laterite and Sudbury Basin

Sulfide mineral

The sulfide minerals are a class of minerals containing sulfide (S2−) or disulfide as the major anion.

See Laterite and Sulfide mineral

Supercontinent

In geology, a supercontinent is the assembly of most or all of Earth's continental blocks or cratons to form a single large landmass.

See Laterite and Supercontinent

Suryavarman II

Suryavarman II (សូរ្យវរ្ម័នទី២, UNGEGN:, ALA-LC), posthumously named Paramavishnuloka, was the ruler of the Khmer Empire from 1113 until his death in 1150.

See Laterite and Suryavarman II

Terrain

Terrain or relief (also topographical relief) involves the vertical and horizontal dimensions of land surface.

See Laterite and Terrain

Tertiary

Tertiary is an obsolete term for the geologic period from 66 million to 2.6 million years ago.

See Laterite and Tertiary

Tin

Tin is a chemical element; it has symbol Sn and atomic number 50.

See Laterite and Tin

Titanium

Titanium is a chemical element; it has symbol Ti and atomic number 22.

See Laterite and Titanium

Tropic of Cancer

The Tropic of Cancer, also known as the Northern Tropic, is the Earth's northernmost circle of latitude where the Sun can be seen directly overhead.

See Laterite and Tropic of Cancer

Tropic of Capricorn

The Tropic of Capricorn (or the Southern Tropic) is the circle of latitude that contains the subsolar point at the December (or southern) solstice.

See Laterite and Tropic of Capricorn

Ultramafic rock

Ultramafic rocks (also referred to as ultrabasic rocks, although the terms are not wholly equivalent) are igneous and meta-igneous rocks with a very low silica content (less than 45%), generally >18% MgO, high FeO, low potassium, and are composed of usually greater than 90% mafic minerals (dark colored, high magnesium and iron content).

See Laterite and Ultramafic rock

Water table

The water table is the upper surface of the zone of saturation.

See Laterite and Water table

Weathering

Weathering is the deterioration of rocks, soils and minerals (as well as wood and artificial materials) through contact with water, atmospheric gases, sunlight, and biological organisms. Laterite and Weathering are pedology.

See Laterite and Weathering

Western Ethiopian Shield

The Western Ethiopian Shield is a small geological shield along the western border of Ethiopia.

See Laterite and Western Ethiopian Shield

Wet season

The wet season (sometimes called the rainy season or monsoon season) is the time of year when most of a region's average annual rainfall occurs.

See Laterite and Wet season

The white metals are a series of often decorative bright metal alloys used as a base for plated silverware, ornaments or novelties, as well as any of several lead-based or tin-based alloys used for things like bearings, jewellery, miniature figures, fusible plugs, some medals and metal type.

See Laterite and White metal

Zeitschrift für Geomorphologie

The Zeitschrift für Geomorphologie is a peer-reviewed scientific journal about geomorphology.

See Laterite and Zeitschrift für Geomorphologie

Zircon

Zircon is a mineral belonging to the group of nesosilicates and is a source of the metal zirconium.

See Laterite and Zircon

See also

Ore deposits

Regolith

Soil-based building materials

Weathering

References

[1] https://en.wikipedia.org/wiki/Laterite

Also known as Laterisation, Laterite rocks, Laterite soil, Laterites, Lateritic, Lateritic soil, Lateritization.

, Igneous rock, India, International Crops Research Institute for the Semi-Arid Tropics, Inverted relief, Ion, Iron, Iron oxide, Island arc, Kaolinite, Khmer Empire, Latin, Leachate, Leaching (pedology), Lead, Limestone, Madhya Pradesh, Mafic, Magnesite, Magnesium, Manganese, Manganese oxide, Masonry, Mesozoic, Metamorphic rock, Migmatite, Mineral, Mineralogy, Monsoon, National Polytechnic Institute of Toulouse, Nickel, Nickel mining in New Caledonia, Niger, Northern Ireland, Olivine, Ore, Oxide, Parent rock, Peridotite, PH, Pisolite, Plagioclase, Plateau, Potassium, Precambrian, Pyroxene, Quartz, Quaternary, Regolith, Sahel, Salt (chemistry), Sandstone, Saprolite, Savanna, Schist, Sea surface temperature, Sedimentary rock, Sesquioxide, Silcrete, Silicon oxide, Smallholding, Sodium, Soil horizon, Steppe, Subsoil, Sudbury Basin, Sulfide mineral, Supercontinent, Suryavarman II, Terrain, Tertiary, Tin, Titanium, Tropic of Cancer, Tropic of Capricorn, Ultramafic rock, Water table, Weathering, Western Ethiopian Shield, Wet season, White metal, Zeitschrift für Geomorphologie, Zircon.