Information about Plain

Moghan plain, East Azarbaijan Province, Iran
Types of plains
- Abyssal plain, a flat or very gently sloping area of the deep ocean basin floor.
- Alluvial plain, with formed by the deposition of alluvial soil over a long period of time by a river coming from the mountains.
- Coastal plain, an area of flat, low-lying land adjacent to a sea coast and separated from the interior by other features.
- Flood plain, flat or nearly flat land adjacent to a stream or river that experiences occasional or periodic flooding.
- Fluvial plain
- Lacustrine plain, a plain that originally formed in a lacustrine environment, that is, as the bed of a lake
- Lava plain, an expanse of land where lava is flowing.
- Scroll plain, an area where a river meanders with a very low gradient.
- Till plain, a flat plain of glacial till that forms when a sheet of ice becomes detached from the main body of a glacier and melts in place depositing the sediments it carried.
Notes and references
See also
- Field
- Flooded grasslands and savannas
- Flood-meadow
- Grassland
- Meadow
- Pasture
- Plateau
- Prairie
- Rangeland
- Savanna
- Steppe
- Water-meadow
- Wet meadow
- Veld
Geography - (from the Greek words Geo (γη) or Gaea (γαία), both meaning "Earth", and graphein (γράφειν) meaning "to describe" or "to write"
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landscape comprises the visible features of an area of land, including physical elements such as landforms, living elements of flora and fauna, abstract elements such as lighting and weather conditions, and human elements, for instance human activity or the built environment.
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Agriculture (from Agri Latin for ager ("a field"), and culture, from the Latin cultura "cultivation" in the strict sense of "tillage of the soil". A literal reading of the English word yields "tillage of the soil of a field".
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plateau, also called a high plateau or tableland, is an area of highland, usually consisting of relatively flat rural area.
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Genesis
A plateau is a large and highland area of fairly level land separated from surrounding land by steep slopes (as in the Tibet),..... Click the link for more information.
mountain is a landform that extends above the surrounding terrain in a limited area. A mountain is generally steeper than a hill, but there is no universally accepted standard definition for the height of a mountain or a hill although a mountain usually has an identifiable
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Erosion is displacement of solids (soil, mud, rock and other particles) usually by the agents of currents such as, wind, water, or ice by downward or down-slope movement in response to gravity or by living organisms (in the case of bioerosion).
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Volcano:
1. Large magma chamber
2. Bedrock
3. Conduit (pipe)
4. Base
5. Sill
6. Branch pipe
7. Layers of ash emitted by the volcano
8. Flank 9. Layers of lava emitted by the volcano
10. Throat
11. Parasitic cone
12. Lava flow
13. Vent
14.
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1. Large magma chamber
2. Bedrock
3. Conduit (pipe)
4. Base
5. Sill
6. Branch pipe
7. Layers of ash emitted by the volcano
8. Flank 9. Layers of lava emitted by the volcano
10. Throat
11. Parasitic cone
12. Lava flow
13. Vent
14.
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Abyssal plain are flat or very gently sloping areas of the deep ocean basin floor. They are among the Earth's flattest and smoothest regions and the least explored. Abyssal plains cover approximately 40% of the ocean floor and reach depths between 2,200 and 5,500 m (7,200 and
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Earth's oceans
(World Ocean)
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(World Ocean)
- Arctic Ocean
- Atlantic Ocean
- Indian Ocean
- Pacific Ocean
- Southern Ocean
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An alluvial plain is a relatively flat and gently sloping landform found at the base of a range of hills or mountains, formed by the deposition of alluvial soil over a long period of time by one or more rivers coming from the mountains.
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Alluvium (from the Latin, alluvius, from alluere, "to wash against") is soil or sediments deposited by a river or other running water. Alluvium is typically made up of a variety of materials, including fine particles of silt and clay and larger particles of sand
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river is a natural waterway that transits water through a landscape from higher to lower elevations. It is an integral component of the water cycle. The water within a river is generally collected from precipitation through surface runoff, groundwater recharge (as seen at baseflow
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mountain is a landform that extends above the surrounding terrain in a limited area. A mountain is generally steeper than a hill, but there is no universally accepted standard definition for the height of a mountain or a hill although a mountain usually has an identifiable
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A coastal plain is an area of flat, low-lying land adjacent to a seacoast and separated from the interior by other features. One of the world's longest coastal plains is located in western South America.
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worldwide view.
A floodplain, or flood plain, is flat or nearly flat land adjacent to a stream or river that experiences occasional or periodic flooding.
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flood is an overflow of an expanse of water that submerges land, a deluge.[1] In the sense of "flowing water", the word is applied to the inflow of the tide, as opposed to the outflow or "ebb".
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A Lacustrine plain is a plain that originally formed in a lacustrine environment, that is, as the bed of a lake, but from which the water has disappeared, by natural drainage, evaporation or other geophysical processes.
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Lacustrine, in ecology, is the environment of a lake. Lacustrine, in geology, is a sedimentary environment of a lake. Lacustrine, in ichthyology, describes a population of fish which complete the bulk of their life cycle within lakes.
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lake (from Latin ligacus) is a body of water or other liquid of considerable size contained on a body of land. A vast majority of lakes on Earth are fresh water, and most lie in the Northern Hemisphere at higher latitudes.
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lava plain, or lava field, is a large expanse of nearly flat-lying lava flows. Such features are generally composed of highly-fluid basalt lava, and can extend for tens or even hundreds of miles across the underlying terrain.
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Lava is molten rock expelled by a volcano during an eruption. When first expelled from a volcanic vent, it is a liquid at temperatures from 700 °C to 1,200 °C (1,300 °F to 2,200 °F).
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A scroll plain occurs where a river meanders across an area with a very low gradient, usually with a fairly continuous discharge. In addition to meanders, scroll plains are also characterised by many oxbow lakes.
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A meander is a bend in a river, also known as an oxbow loop, or simply an oxbow. A stream or river flowing through a wide valley or flat plain will tend to form a meandering stream course as it alternatively erodes and deposits sediments along its course.
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A till plain is an extensive flat plain of glacial till that forms when a sheet of ice becomes detached from the main body of a glacier and melts in place depositing the sediments it carried. A till plain with irregular topography is referred to as a ground moraine.
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Till is an unsorted glacial sediment. Glacial drift is a general term for the coarsely graded and extremely heterogeneous sediments of glacial origin. Glacial till is that part of glacial drift which was deposited directly by the glacier.
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ICE may refer to:
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- Internal combustion engine, a fuel engine
- In case of emergency, the emergency contact program created after the 7 July 2005 London Bombings
- International Cometary Explorer, a former spacecraft
- Integrated Collaboration Environment
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glacier is a large, slow moving river of ice, formed from compacted layers of snow, that slowly deforms and flows in response to gravity. Glacier ice is the largest reservoir of fresh water on Earth, and second only to oceans as the largest reservoir of total water.
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Sediment is any particulate matter that can be transported by fluid flow and which eventually is deposited as a layer of solid particles on the bed or bottom of a body of water or other liquid. Sedimentation is the deposition by settling of a suspended material.
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field refers generally to an area of land enclosed or otherwise and used for agricultural purposes such as:
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- Cultivating crops
- Usage as a paddock or generally an enclosure of livestock
- Land left to lie fallow or as arable land
Language
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Flooded grasslands and savannas are a biome, generally located at subtropical and tropical latitudes, where which are flooded seasonally or year-round.
It is characterized by
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It is characterized by
- water : very wet
- temperature : warm
- soils : nutrient rich soil
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