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Syncline is a type of fold that is created when the crust bends and curves downward. It is a fold that is convex up and has its oldest beds at its core.
It's often called a trench.
This geological formation is called a syncline. It is a downward fold in the rock layers where the youngest layers are in the center and the oldest are on the outside.
A canyon on the ocean floor where the crust bends downward is known as a "submarine trench." These trenches are formed by the process of subduction, where one tectonic plate is forced beneath another, creating deep, narrow depressions in the ocean floor. The Mariana Trench is the most famous example, reaching depths of over 36,000 feet. These geological features are significant for studying Earth's tectonic activity and marine biodiversity.
An Anticline is formed when the crust bends and curves upward.
Erosion happens in the earths crust and it happens because of that layer is exposed to that weather
The oceans flow to the places where the crust is the lowest. Gravity causes them to flow downward. The mantle, below the crust, is at the same depth everywhere, so if the crust is lower, it is because it is thinner.
A submarine canyon is a deep, steep-sided valley cut into the seabed of the continental slope, often formed by underwater currents. It can be a conduit for sediment transport from the shelf to the deep ocean.
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When the Earth's crust bends but does not break, it is called flexural bending or flexure. This type of deformation can occur in response to tectonic forces, leading to the formation of features like folds, fault-related folds, and anticlines.
deep ocean trench.
A normal fault