The term "continental" typically refers to continental crust, which is generally thicker and less dense than oceanic crust. While continental crust can be considered "heavier" in terms of mass due to its greater thickness, it is less dense than the denser oceanic crust. Therefore, in terms of density, oceanic crust is heavier, but in terms of overall mass, continents can be heavier due to their larger volume.
Trench
Continental crust is thicker but less dense, and oceanic crust is thinner but more dense, making it heavier.
Oceanic plates are heavier than continental plates because they are denser and thinner. Continental plates are lighter because they are less dense and thicker. The difference in density and composition accounts for the varying weights of the Earth's plates.
Continental crust and continental crust are made of different types of rock. The rocks in the continental crust do not contain as many of the heavier elements as the ones in the oceanic crust do.
Oceanic crust is heavier and younger compared to continental crust. It is denser because it is composed of basaltic rocks, while continental crust is made up of less dense granitic rocks. Additionally, oceanic crust is continually being formed at mid-ocean ridges through seafloor spreading, making it much younger on average than continental crust.
Continental crust is generally lighter than oceanic crust because it is thicker and less dense. Oceanic crust, being thinner and denser, tends to be heavier.
The main theory on the continental divide is that they relate to the plate techonics theory of the Earth's crust. The other theory is the continental drift theory where lighter rocks float on heavier crustal material.
Oceanic crust is mafic in composition and continental crust is felsic in composition. Mafic minerals generally have a higher density than felsic minerals and therefore, the oceanic crust is heavier.
The oceanic plate is denser than the continental plate due to its composition of heavier mafic rock. This density difference causes the oceanic plate to sink below the continental plate in a process known as subduction.
No, the oceanic crust is denser. That's why the land areas "float" so much higher than the ocean bedrock.
an example of this is the marinas trench of the coast of japan and the continental plate of the Philippine's. the more denser oceanic plate is forced under by the lighter continental plate. this normally happens at destructive plate margins.
This process is known as subduction. As the heavier sea plate is forced beneath the lighter continental plate, it can create deep-sea trenches and can lead to volcanic activity on the Earth's surface. Subduction zones are often associated with seismic activity, including earthquakes.