Strictly speaking it isn't.
It's divided into Continental Crust plates (mainly granite), surrounded by the thinner, denser basalt plates of the ocean floor, and all floating on the viscous Mantle.
These are constantly shuffling around the globe, and individual plates can be stretched, thinned and broken by processes in the Mantle, or warped downwards by ice-pressure during the cold phases of ice-ages.
The Atlantic is widening at about 20mm/yr from its Mid-Atlantic [Spreading] Ridge as the Pacific shrinks by subduction around its coasts. The Mediterranean is shrinking slowly, and Africa starting to split in two. India's collision with Asia is still pushing the Himalaya upwards, etc. The Appalachians, Scottish Highlands and Norwegian mountains were all originally one chain, broken by the Atlantic and North Sea developing.
Until plate tectonics was understood in the later part of 20th Century geologists did call the continents "rigid masses" and could not conceive of them moving; but were unable satisfactorily to explain folding, faulting, mountain-building and volcanoes. Once the light dawned thanks to advances in oceanography and seismology, everything fell into place beautifully!
Igneous rock is what you get when hot, liquid rock cools and becomes solid. Early in the history of the Earth, the whole planet was so hot that all the rock was liquid. Hence, it was all igneous at first, when the planet started to cool. Non-igneous rock is rock that used to be igneous but has since undergone further changes (for various reasons).
Because the word crust means a hard outer layer - and that's what it is.
Because if it was not solid it would not be a crust. It has to solidify before you can call it a crust. The outer part of a molten rock will cool first and become the crust.
The crust is composed of igneous, sedimentary and metamorphic rocks.
No, it is an extrusive igneous rock, which means it is made on the Earth's surface, as opposed to intrusive (or plutonic) rocks, which are made under the Earth's crust. Obsidian is most often produced by the rapid cooling of silica-rich lava, such as by contact with water, which crystallizes the lava into a glassy solid.
Igneous rock.
Metamorphic and igneous rocks are the two most common under the surface of earth.
That would be true.
This is true!
The crust is composed of igneous, sedimentary and metamorphic rocks.
Ultramafic igneous rock.
Aluminum is the Earths most abundant metal and its located in the Earths outer crust.One of the properties of crust is that it consists of a variety of sedimentary,metamorphic and igneous rocks.
Just to say: This question refers to rock groups. Not what type of rock.Igneous rocks make up most of the earth's crust.
No, it is an extrusive igneous rock, which means it is made on the Earth's surface, as opposed to intrusive (or plutonic) rocks, which are made under the Earth's crust. Obsidian is most often produced by the rapid cooling of silica-rich lava, such as by contact with water, which crystallizes the lava into a glassy solid.
Igneous rock.
in the earths mantle
Igneous rock is by far the most common rock of the crust.
That would be true.
Metamorphic and igneous rocks are the two most common under the surface of earth.
Silicate minerals such as quartz and feldspar are the most common minerals located in earths crust