Continental: granite
oceanic: basalt
Oceanic crust is thinner and denser than continental crust. Oceanic crust is primarily made of basalt, while continental crust is composed of granitic rocks. Continental crust is older and more complex in structure compared to oceanic crust. Oceanic crust is constantly being created at mid-ocean ridges and destroyed at subduction zones, while continental crust is more stable and less prone to being recycled.
Yes. It is more dense than continental crust.
The rock that makes up both continental and oceanic crust is called basalt. Basalt is a mafic extrusive igneous rock that forms when lava cools and solidifies rapidly at the Earth's surface. It is commonly found in oceanic crust, while continental crust is made up of a variety of rocks including basalt.
The crust that makes up the continents, or land masses on Earth is called continental crust. The crust that makes up the oceans is called oceanic crust.
Oceanic crust is more active than continental crust because it is thinner, younger, and more dense. This makes oceanic crust more prone to subduction beneath tectonic plates, leading to more frequent volcanic and seismic activity. Continental crust, on the other hand, is older, thicker, and less dense, resulting in fewer tectonic movements and less geologic activity.
The oceanic plate is thin, dense, and makes up the ocean floor. The continental plate is less-dense, thick, and make up the continents.
Oceanic crust is thinner and denser than continental crust. Oceanic crust is primarily made of basalt, while continental crust is composed of granitic rocks. Continental crust is older and more complex in structure compared to oceanic crust. Oceanic crust is constantly being created at mid-ocean ridges and destroyed at subduction zones, while continental crust is more stable and less prone to being recycled.
Yes. It is more dense than continental crust.
The part of the Earth's crust that is not covered by ocean water is called the continental crust. It is thicker and less dense than the oceanic crust and primarily makes up the continents.
The continental crust is mainly composed of igneous rocks like granite and metamorphic rocks like gneiss. The oceanic crust is primarily made of basalt, which is an igneous rock that forms from cooling lava at mid-ocean ridges.
The two types of crust are oceanic crust, which is denser and thinner, and continental crust, which is less dense and thicker. Oceanic crust is typically found beneath the ocean floor, while continental crust makes up the landmasses on Earth.
Continental plates are thicker and less dense. Continental plates are mainly granitic in composition. Oceanic plates are mainly basaltic in composition. The rock of continental plates is on average, much older than the rock of the oceanic plates. The oceanic plate underlies the oceans, and the continental plate makes up the land masses. Continental plates do not subduct at convergent plate boundaries.
The rock that makes up both continental and oceanic crust is called basalt. Basalt is a mafic extrusive igneous rock that forms when lava cools and solidifies rapidly at the Earth's surface. It is commonly found in oceanic crust, while continental crust is made up of a variety of rocks including basalt.
Continental crust is thicker and less dense while oceanic crust is thinner and more dense, so essentially continental crust takes a higher position than oceanic crust. When oceanic and continental plates collide, oceanic plates slide underneath continental plates(if this makes what I said any clearer).
continental crust
The oceanic crust is denser than the continental crust. This is due to the composition of the rocks that make up each type of crust. Oceanic crust is primarily composed of basalt, which is denser than the granite that makes up the continental crust. This density difference is a key factor in the process of plate tectonics and the formation of oceanic trenches and volcanic arcs.
Thicker, less dense, and older than oceanic crust. It primarily consists of granitic rock, is less abundant, and makes up the continents' landmasses. Continental crust also tends to have higher elevations and is more likely to contain mineral resources.