Basalt is more dense than granite true false weegy.
Is granit more thick than basalt.
All rocks of igneous origin consist of magma or molten earth that finds its way up to.
Basalt is an igneous volcanic rock that forms commonly in oceanic crust and parts of continental crust.
Gabbro basalt and gabbro have a similar composition just the crystal size differs from different cooling rates same for rhyolite and granite.
It forms from lava flows which extrude onto the surface and cool.
This slow cooling gives time for crystals to grow making it more coarsely grained than an extrusive rock.
Basalt on the other hand has a smooth texture from rapid cooling usually by water.
Granite is a very hard granular crystalline igneous rock which consists mainly of quartz mica and feldspar and is often used as building stone.
This coarse grain makes granite a favorite of rock climbers.
School montclair state university.
Course title eaes 101.
Basalt is more common in oceanic crust while granite is more common in continental crust.
Granite is more dense than basalt a true b false answer page 3 of 12 references.
Granite is more dense than basalt a true b false.
Granite is an intrusive rock that is formed when magma cools inside the crust.
Basalt is denser than granite because basalt is a an oceanic type of rock so it has had more pressure from the ocean making it denser than granite because granite is a continental type of rock.
You can also know more about granite and basalt reserves.
The key difference between basalt and granite is that basalt is mostly occurring on ocean floors while granite is in the crust of the earth in all continents.
Earth contains three kinds of rocks namely igneous rocks sedimentary rocks and metamorphic rocks basalt and granite are two types of igneous rocks.
Basalt is denser than granite because basalt is a an oceanic type of rock so it has had more pressure from the ocean making it denser than granite because granite is a continental type of rock.
Basalt is a common extrusive igneous rock formed by the rapid cooling of basaltic lava exposed at or very near the surface of earth.