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artofit.org
- Oceanic trenches are a feature of the Earth's distinctive plate tectonics. They mark the locations of convergent plate boundaries, along which lithospheric plates move towards each other at rates that vary from a few millimeters to over ten centimeters per year.
en.wikipedia.org/wiki/Oceanic_trench
People also ask
What does an oceanic trough do?
What is a trough in geology?
Why does a water trough have a circular motion?
How does a wave move in a trough?
How deep are oceanic troughs?
What does crest trough mean?
Oceanic trough, an elongate depression in the seafloor that is characteristically shallower, shorter, narrower, and topographically gentler than oceanic trenches. Maximal depths of oceanic troughs range between 2,300 m (7,500 feet) in the Papuan Trough and 7,440 m in the Banda Trough.
- The Editors of Encyclopaedia Britannica
In geology, a trough is a linear structural depression that extends laterally over a distance. Although it is less steep than a trench, a trough can be a narrow basin or a geologic rift. These features often form at the rim of tectonic plates. There are various oceanic troughs on the ocean floors.
We are most familiar with the kind of waves that break on shore, or rock a boat at sea, but there are many other types of waves that are important to oceanography: Internal waves form at the boundaries of water masses of different densities (i.e. at a pycnocline), and propagate at depth.
In geology, a trough is a linear structural depression that extends laterally over a distance. Although it is less steep than a trench, a trough can be a narrow basin or a geologic rift. These features often form at the rim of tectonic plates.
Jun 10, 2024 · We are most familiar with the kind of waves that break on shore, or rock a boat at sea, but there are many other types of waves that are important to oceanography: Internal waves form at the boundaries of water masses of different densities (i.e. at a pycnocline), and propagate at depth.
Mar 5, 2020 · For example, in the ocean, the water moves up and down, but returns to surface level. This creates high points called crests and low points called troughs. As the water moves up and down, the crests and troughs move to the side, carrying energy.
Jun 10, 2024 · Most ocean waves are generated by wind. Wind blowing across the water’s surface creates little disturbances called capillary waves, or ripples that start from gentle breezes (Figure \(\PageIndex{1}\)). Capillary waves have a rounded crest with a V-shaped trough, and wavelengths less than 1.7 cm.
