Continental Slope Vs Rise at Katie Almond blog

Continental Slope Vs Rise. A continental rise consists mainly of silts, mud, and sand, deposited by turbidity. At the bottom of the slope is the continental rise. A continental rise is a wide, gentle incline from a deep ocean plain (abyssal plain) to a continental slope. Continental rise, a major depositional regime in oceans made up of thick sequences of continental material that accumulate between the continental slope and the abyssal plain. At the bottom of the slope is the continental rise. This area represents where the continental crust meets the oceanic crust, as the slope begins to level off to become the deep ocean floor. This area represents where the continental crust meets the oceanic crust, as the slope begins to level off to become the deep ocean.

PPT Continental Margins and Ocean Basins PowerPoint Presentation
from www.slideserve.com

This area represents where the continental crust meets the oceanic crust, as the slope begins to level off to become the deep ocean. At the bottom of the slope is the continental rise. A continental rise is a wide, gentle incline from a deep ocean plain (abyssal plain) to a continental slope. At the bottom of the slope is the continental rise. A continental rise consists mainly of silts, mud, and sand, deposited by turbidity. This area represents where the continental crust meets the oceanic crust, as the slope begins to level off to become the deep ocean floor. Continental rise, a major depositional regime in oceans made up of thick sequences of continental material that accumulate between the continental slope and the abyssal plain.

PPT Continental Margins and Ocean Basins PowerPoint Presentation

Continental Slope Vs Rise This area represents where the continental crust meets the oceanic crust, as the slope begins to level off to become the deep ocean. Continental rise, a major depositional regime in oceans made up of thick sequences of continental material that accumulate between the continental slope and the abyssal plain. This area represents where the continental crust meets the oceanic crust, as the slope begins to level off to become the deep ocean. This area represents where the continental crust meets the oceanic crust, as the slope begins to level off to become the deep ocean floor. A continental rise is a wide, gentle incline from a deep ocean plain (abyssal plain) to a continental slope. At the bottom of the slope is the continental rise. A continental rise consists mainly of silts, mud, and sand, deposited by turbidity. At the bottom of the slope is the continental rise.

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