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Mountain ranges are formed when two continental plates collide. When they converge one plate will be forced slightly under the other one.

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Is a deep sea trench a feature of a passive continental margin?

No, a deep sea trench is not a feature of a passive continental margin. Deep sea trenches are associated with convergent plate boundaries where one tectonic plate is being forced beneath another, leading to the formation of a trench. Passive continental margins are characterized by a lack of tectonic activity and are often marked by wide continental shelves and gentle slopes.


What geologic feature seems to be a common location for finding diamonds?

Kimberlite pipes are a common geologic feature where diamonds are found. These cylindrical volcanic rock formations bring diamonds to the Earth's surface from deep within the mantle. Diamonds are typically formed under high pressure and temperature conditions, and kimberlite pipes are one of the few mechanisms for bringing them to the surface.


Sonar shows that the edges of continental shelves match what?

Sonar shows that the edges of continental shelves match the underwater slope known as the continental slope. This underwater feature marks the boundary between the continental shelf and the deeper ocean floor. The continental slope is steeper than the continental shelf and descends into the abyssal plain.


What is formed when two crustal plates collide what surface feature is created?

When two crustal plates collide, they can form mountain ranges. The collision forces the crustal rocks to deform and buckle, leading to the creation of folded and uplifted mountain belts on the Earth's surface.


What is a hydrothermal feature?

A hydrothermal feature is a geologic formation that involves the circulation of hot water underground. This can lead to the formation of geysers, hot springs, fumaroles, and mud pots. These features are common in areas with volcanic activity or where there is high heat flow from the Earth's interior.