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- In geology, a trough refers to a linear depression that extends in one direction over a distance. It is less steep than a trench. A trough can be a narrow basin or a geologic rift. There are various oceanic troughs, troughs found under oceans; examples include the rifts along the mid-ocean ridges.
wiki.kidzsearch.com/wiki/Trough_(geology)
In geology, a trough refers to a linear depression that extends in one direction over a distance. It is less steep than a trench. A trough can be a narrow basin or a geologic rift. There are various oceanic troughs, troughs found under oceans; examples include the rifts along the mid-ocean ridges.
- Troughs
A trough is an elongated area of comparatively low...
- Troughs
Oct 16, 2023 · A trough is an elongated area of comparatively low atmospheric pressure, usually in association with weather fronts. Convective cells may form in the surrounding area of troughs and give birth to a tropical cyclone.
In geology, a trough refers to a linear depression that extends in one direction over a distance. It is less steep than a trench. A trough can be a narrow basin or a geologic rift. There are various oceanic troughs, troughs found under oceans; examples include the rifts along the mid-ocean ridges.
definition 1: a long narrow open container used for serving food or water to animals. The pigs gathered at the trough. definition 2: any long narrow depression or channel, such as a gutter, a narrow valley, or the depression in water between two waves. definition 3:
Glacial troughs. Rivers cut V-shaped valleys through the process of erosion. As rivers in their upper course don’t have that much power, they are forced to wind between harder rock leaving ridges...
These are valleys formed by the glacial processes of weathering, erosion and transportation. They have steep sides and flat floors. Unlike V-shaped river valleys, glacial troughs are straight as they have truncated any interlocking spurs which existed prior to glacial advance.
There are two main processes involved with erosion: ‘plucking’ (which involves pieces of rock beneath the glacier being ripped out by the moving ice) and ‘abrasion’ (which involves the rock debris being carried by the ice gouging and scouring the ground beneath and along the sides of the glacier.