Granitic rock forms the majority of the continental crust.
Granitic rock forms the majority of the continental crust.
The light colored rock that makes up most of the continental crust is granite. It is a coarse-grained igneous rock composed mainly of quartz and feldspar minerals. Granite is less dense than the dark basaltic rock that makes up oceanic crust.
The light-colored rock that makes up the continental crust is called granite. Granite is a coarse-grained igneous rock composed mainly of quartz, feldspar, and mica. It is less dense and more buoyant than the darker basaltic rock that makes up the oceanic crust.
granite or rhyolite
Granite
granite
Granite
granite or rhyolite
Granite is the rock that makes up most of the continental crust. It is a coarse-grained igneous rock that is formed through the slow cooling of magma beneath the Earth's surface. Granite is composed mainly of quartz, feldspar, and mica minerals.
The predominant rock in the Earth's crust and upper mantle is called silicate rock, composed mainly of silicon and oxygen. This type of rock is known as "peridotite" in the mantle and "granite" in the crust.
The continental crust is composed mostly of granite, a type of igneous rock that is rich in silica and aluminum. Granite is formed through the solidification of magma deep beneath the Earth's surface.
The rock that underlies the oceans is primarily basalt, not granite. Basalt is a volcanic rock that forms from solidified lava, and it makes up most of the oceanic crust. Granite, on the other hand, is a different type of rock that is more commonly found in continental crust.