Answer:
1. oceanic-oceanic boundaries
2. oceanic-continental boundaries
3. continental-continental boundaries
Explanation:
The three types of plate convergence are:
1. oceanic-oceanic boundaries: this occurs when two oceanic plates clash; thereby the heavier plate forms below the lighter plate resulting in dark, heavy, basaltic volcanic islands.
2. oceanic-continental boundaries: this occurs when there is a collision between oceanic and continental plates, resulting in the downward movement of oceanic plate, while the volcanic arc rises on land
3. continental-continental boundaries: this occurs due to the massive crust of slabs clashing against each other. Thereby leading to big mountains forming from folded, faulted, and thickened convergent boundaries
Answer: In some parts of the world, windblown dust and silt blanket the land. This layer of fine, mineral-rich material is called loess. Loess is mostly created by wind, but can also be formed by glaciers. When glaciers grind rocks to a fine powder, loess can form.
Answer:
u be lookin like a hot dog that got burnt hahaha
Explanation:
Washington D.C is the capital of U.S.A and Ottawa is the capital of Canada
The <span>narrow belts of fast-moving air at the higher levels of the troposphere are called jet streams. The paths of the jet streams can be best described as meandering. Jet streams can start or stop or split or move in the reverse direction at any time. I hope that the answer has come to your great help.</span>
