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A ridge-like deposit of sediment at the edge of a glacier is called a "moraine." Moraines are formed from the accumulation of debris and sediment that has been pushed along by the glacier's movement. They can be classified into different types, such as terminal moraines, which mark the furthest advance of the glacier, and lateral moraines, which form along the sides of the glacier.
A trough is distinguished on the weather chart by system of isobars which appear sharply curved along a line .this curves are concave towards low pressure. Trough may be termed deep or shallow according to whether the curvature of the isobar is acute or gentle. The weather associated with a trough is generally cloudy with precipitation.
Another ridge similar to the Mid-Atlantic Ridge can be found in the Indian Ocean, known as the Southwest Indian Ridge. It is a divergent boundary where the African Plate and the Antarctic Plate are moving apart. This ridge, like the Mid-Atlantic Ridge, is associated with volcanic activity and the creation of new oceanic crust.
A Synform fold or Syncline.
In sea-floor spreading,the sea floor spreads apart along both sides of the mid-ocean ridge as a new crust is added.As a result,the ocean floors move like conveyor belts,carrying the continents along with them.
A trough-like fold of rock strata is known as a syncline. Synclines are downward-arching folds where the youngest layers are located in the center of the fold and the oldest layers are along the outer edges. They are typically U-shaped in appearance.
An ocean ridge is most likely to be located at the boundary where two tectonic plates are moving apart, such as the Mid-Atlantic Ridge. This is where new oceanic crust is formed as magma rises to the surface and solidifies, creating a ridge-like structure along the seafloor.
If the cylinder is cut in half along the side it is still a cylinder. If the cylinder is cut in half along one of the circular faces it is a horizontal cylindrical segment, which would look like a pig trough not hollowed out.
This is likely a moraine, which is formed when rocks and sediment are picked up and transported by a glacier. As the glacier melts, it deposits this material along its edges, creating a ridge-like feature. There are different types of moraines, such as lateral, medial, and terminal moraines, each forming in specific locations along the glacier's path.
A ridge-like deposit of sediment at the edge of a glacier is called a "moraine." Moraines are formed from the accumulation of debris and sediment that has been pushed along by the glacier's movement. They can be classified into different types, such as terminal moraines, which mark the furthest advance of the glacier, and lateral moraines, which form along the sides of the glacier.
Ridge push is a geological concept where the force of gravity causes oceanic lithosphere to move downhill from a mid-ocean ridge, pushing tectonic plates away from the ridge. This process contributes to plate motion along with other forces like slab pull and mantle convection.
The sea-floor spreading begins at the mid-ocean ridge, which forms along a crack in the oceanic crust. Along the ridge, molten material that forms several kilometers beneath the surface, rises and erupts. At the same time, older rock moves outward on both sides of the ridge. As the molten material cools, it forms a strip of solid rock in the center of the ridge. When more molten material flows into the crack, it forms a new strip of rock.
A bee guard for a hummingbird feeder looks like a trough of water. The trough looks like a circle around the top of the feeder.
synclines
A manger is like a feeding trough
Well a sand dune is a ridge of sand that is created by the wind... They have a smooth appearance and faint lines running along them
A dune is a mound or ridge of sand typically found in deserts or along coastlines. It can vary in size and shape, often shaped by wind or water. Dunes can have a slope on one side and a more gradual incline on the other.