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mainly of basaltic lava flows and minor, coralline limestone

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What is the difference between continental and ocenic crust?

Continental crust is thicker, averaging about 30-50 kilometers, and primarily composed of lighter, granitic rocks, making it less dense than oceanic crust. Oceanic crust, on the other hand, is thinner, around 5-10 kilometers thick, and composed mainly of denser basaltic rocks. Additionally, continental crust is older and more stable, while oceanic crust is continuously created and destroyed at mid-ocean ridges and subduction zones. This fundamental difference contributes to various geological features and processes on Earth.


What is the difference between oceanic plate and continential plate?

Oceanic plates are young and made of basalt and recent sediments. Continental plates are old and contain continental crust made of old rocks and they are usually considerably thicker than the oceanic plates


What is the difference between oceanic and continental Croat?

Oceanic crust is primarily composed of basalt and is denser and thinner than continental crust, which is mainly made up of granitic rocks. Oceanic crust forms at mid-ocean ridges and is continuously created and recycled at subduction zones. In contrast, continental crust is thicker, less dense, and older, forming the landmasses we live on. These differences result in distinct geological features and processes associated with each type of crust.


What are four differences between the oceanic crust and the continental crust?

1. The Oceanic crust is dense while the Continental crust is relatively lighter. 2. The Oceanic crust consists of Silicon and Magnessium, while the Continental crust has Silicon and Alluminium. 3. The Oceanic crust is thin, while the Continental crust is thick. 4. The Oceanic crust makes up the ocean floor, while the Continental crust carries the continents.


What is produced at continental continental convergent boundaries?

At continental-continental convergent boundaries, large mountain ranges are produced due to the collision of two continental plates. The intense pressure and heat generated during the collision can also lead to the formation of deep crustal roots and high-pressure rocks. These boundaries can also trigger earthquakes and volcanic activity.