Brittle rock.
Some geologists believe there are no tectonic plates composed solely of continental crust, as plates typically consist of both continental and oceanic crust. The concept of a plate composed entirely of continental crust is not widely accepted in the field of plate tectonics.
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.
Continental and oceanic crust are both less dense than mafic rocks. Continental crust is primarily composed of granitic materials, while oceanic crust is mainly basaltic, which is mafic in composition. However, basalt is denser than the average continental crust, making oceanic crust denser than continental crust but still less dense than pure mafic rocks. Therefore, in general, both types of crust are less dense than mafic materials.
The Earth's crust is the rocky inorganic part primarily composed of various minerals. It forms the outermost layer of the planet and includes both continental and oceanic crust. The composition of the crust varies, with continental crust being primarily granitic and oceanic crust being predominantly basaltic.
A conversion boundary is a place where 2 tectonic plates are mving toward each other. There are 3 types of convergent boundaries OCEANIC CRUST-OCEANIC CRUST OCEANIC CRUST-CONTINENTAL CRUST CONTINENTAL CRUST-CONTINENTAL CRUST They are classified according to their crust
The oceanic crust is composed mainly of basalt, rich in iron and magnesium. The continental crust is composed mainly of granite, rich in aluminum. Although they are both rich in oxygen and silicon, the rocks that compose the oceanic crust are of higher density than the rocks that compose the continental crust.
Both oceanic and continental crust are part of the Earth's outermost layer, called the lithosphere. They are both composed of rocks and minerals, but oceanic crust is denser and younger than continental crust. Additionally, both types of crust are involved in plate tectonics and play a role in shaping the Earth's surface.
The continental crust is primarily composed of granite and sedimentary rocks, while the oceanic crust is mainly composed of basalt. Both types of crust consist mainly of silicate minerals such as feldspar, quartz, and mica.
Some geologists believe there are no tectonic plates composed solely of continental crust, as plates typically consist of both continental and oceanic crust. The concept of a plate composed entirely of continental crust is not widely accepted in the field of plate tectonics.
Both oceanic and continental crusts consist primarily of igneous rock although they both contain some sedimentary rock. Oceanic crust is composed mainly of basaltic rock, while continental crust is composed of granitic rock.
Tectonic plates consist of both continental and oceanic crust. The Earth's lithosphere is divided into several large and small plates that constantly move and interact with each other. Some plates are predominantly made up of continental crust, while others are mostly composed of oceanic crust.
Both oceanic and continental crust are composed of solid rock and are part of the Earth's outermost layer. They both float on the semi-liquid layer of the mantle. Additionally, both types of crust are important components of the Earth's tectonic plates.
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.
Yes, lithospheric plates can include both continental and oceanic crust. These plates are composed of the rigid outer layer of Earth's surface, which consists of the upper part of the mantle and the crust. Continental crust is less dense and thicker than oceanic crust, but both can form part of lithospheric plates.
The oceanic crust is mostly composed of basalt, while the continental crust is primarily made up of granite. Both types of crust contain some amount of silica-rich minerals like feldspar and quartz.
Continental and oceanic crust are both less dense than mafic rocks. Continental crust is primarily composed of granitic materials, while oceanic crust is mainly basaltic, which is mafic in composition. However, basalt is denser than the average continental crust, making oceanic crust denser than continental crust but still less dense than pure mafic rocks. Therefore, in general, both types of crust are less dense than mafic materials.
they both are part of the crust