The continental crust is thicker and less dense than oceanic crust. Oceanic crust is younger and primarily composed of basalt, while continental crust is older and made up of a variety of rock types, including granite and sedimentary rocks.
Earth's oceanic crust is thinner, denser, and younger than Earth's continental crust. It is primarily composed of basaltic rock, whereas continental crust is made up of less dense granitic rock. Oceanic crust is constantly being formed at mid-ocean ridges and destroyed at subduction zones.
Continental crust is thicker, less dense, and older than oceanic crust. It is primarily composed of granite and sedimentary rocks. In contrast, oceanic crust is thinner, denser, and younger, and is primarily composed of basalt.
The two types of crust are oceanic and continental. Oceanic crust is thinner, denser, and younger than continental crust. Continental crust is thicker, less dense, and older, with more variety in rock types.
Two differences are that the oceanic crust is more dense than continental, and continental crust is composed mostly of granite, while oceanic is mostly basalt
Oceanic and Continental crusts are alike because they both shift and move and grow. They differ by there rock types. Oceanic crust is made up of dense basalt while continental crust is made up of less dense granite.
The continental crust is thicker and less dense than oceanic crust. Oceanic crust is younger and primarily composed of basalt, while continental crust is older and made up of a variety of rock types, including granite and sedimentary rocks.
Earth's oceanic crust is thinner, denser, and younger than Earth's continental crust. It is primarily composed of basaltic rock, whereas continental crust is made up of less dense granitic rock. Oceanic crust is constantly being formed at mid-ocean ridges and destroyed at subduction zones.
Continental crust is thicker, less dense, and older than oceanic crust. It is primarily composed of granite and sedimentary rocks. In contrast, oceanic crust is thinner, denser, and younger, and is primarily composed of basalt.
The two types of crust are oceanic and continental. Oceanic crust is thinner, denser, and younger than continental crust. Continental crust is thicker, less dense, and older, with more variety in rock types.
Two differences are that the oceanic crust is more dense than continental, and continental crust is composed mostly of granite, while oceanic is mostly basalt
Continental crust is the thicker, less dense, and older type of crust found beneath continents, primarily composed of granite and sedimentary rock. Oceanic crust is the thinner, more dense, and younger type of crust located beneath oceans, primarily composed of basalt. The boundary between continental and oceanic crust is known as the continental-oceanic crust boundary.
Oceanic crust is thinner, denser, and primarily composed of basaltic rock, while continental crust is thicker, less dense, and mainly consists of granitic rock. Oceanic crust is younger and continuously forming at mid-ocean ridges, whereas continental crust is older and more stable. Oceanic crust is also denser because it is made from more mafic, iron and magnesium-rich rocks.
Oceanic crust is denser than continental crust because it is primarily composed of basalt, which is a mafic rock with a higher density than the felsic rocks that make up continental crust. Additionally, oceanic crust is thinner and younger than continental crust, contributing to its higher density.
Oceanic crust is typically thinner, denser, and younger than continental crust. It is primarily composed of basaltic rocks and forms the ocean floor, while continental crust is thicker, less dense, and contains a wider variety of rock types, including granitic rocks. Continental crust forms the continents and is older than oceanic crust.
Oceanic crust is denser than continental crust because it is made up of denser rock types, such as basalt, and it is also thinner and younger. Continental crust is less dense because it is composed of lighter rock types, such as granite, and is thicker and older due to the accumulation of layers over time.
there are two types of crust such as the oceanic crust and the continental crust, the oceanic crust is thinner and more dense than the continental crust and is constantly being recycled via subduction upon collisions with Continental crust, and creating at mid-ocean ridges. x