Oceanic crust is generally denser and thinner than continental crust, which makes it harder in terms of density and composition. Oceanic crust is primarily composed of basalt, while continental crust is mainly granite, which is less dense but thicker. However, the "hardness" can also depend on specific geological contexts and factors like temperature and pressure. Overall, oceanic crust is considered harder due to its density and mineral composition.
Continental crust is far older than oceanic 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.
CONTINENTAL CRUST is 35km of thickness and oceanic is 7 km. i hope that helped
Continental crust is mostly composed out of granite, oceanic crust out of basalt.Continental crust is thicker and less dense than oceanic crust.
The continental crust is less dense than the oceanic crust. That's the reason we find that the oceanic crust sinks (subducts) beneath the continental crust.Continental crust is less dense than oceanic crust and so cannot sink below it.
Oceanic crust is more dense than continental crust. As a result, over time, continental crust is harder to "recycle". Rocks are recycled when they are subducted and remelted. Since continental crust is harder to subduct (it wants to keep floating), it is not recycled as much as oceanic crust, which is dense and will sink and remelt.
No, the oceanic crust is denser. That's why the land areas "float" so much higher than the ocean bedrock.
It is not. The oceanic crust is thinner than the continental crust!
Continental crust is far older than oceanic crust.
It is generally easier to drill through continental crust than oceanic crust. Oceanic crust tends to be thinner, denser, and harder than continental crust, making it more challenging to drill through. Continental crust is thicker and less dense, with more varied geological features and compositions that can be easier to penetrate.
Continental crust is the thicker of the two: it extends far beneath and above the Oceanic crust.
The oceanic crust begins at the Mid-Ocean Ridge, where tectonic plates are moving apart, allowing magma to rise and solidify, forming new crust. This process of seafloor spreading creates the youngest oceanic crust at the ridge and older crust farther away from it.
Continental crust is far older than oceanic crust.
Oceanic and Continental crust. Oceanic crust is made of basalt. Continental crust is made of granite
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.
The continental crust because it is thicker than the oceanic crust
younger