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 more dense than granite as it contains more iron and magnesium. This means that it is likely that the more dense basaltic plate would be forced under the less dense granitic plate.
Granite has more silica than basalt in it.
Granite is higher in silica than is basalt.
Continental is made mostly of granite. Oceanic is made mostly of basalt and gabbro.
Water is less dense than any of the other materials listed.In order of density from least to highest:Water (least dense)GraniteBasaltIron (most dense)
Granite is very much less dense than basalt. This is why the continental crust (mostly composed of granite) floats on Oceanic crust (made mostly of basalt). Granite is 70 % silicon. Where basalt is mainly pyroxene.
Basalt does have a greater specific gravity. Granite is not as dense as basalt.
Basalt is more dense than granite as it contains more iron and magnesium. This means that it is likely that the more dense basaltic plate would be forced under the less dense granitic plate.
Granite has more silica than basalt in it.
Granite is higher in silica than is basalt.
The basalt of the oceanic plate is more dense than the granite in the continental plate.
Continental is made mostly of granite. Oceanic is made mostly of basalt and gabbro.
Water is less dense than any of the other materials listed.In order of density from least to highest:Water (least dense)GraniteBasaltIron (most dense)
Basalt and Granite are igneous rocks which are very hard.
Oceanic crust is composed primarily of the dense volcanic rock basalt. Continental crust is composed primarily of the intrusive igneous rock granite, less dense than basalt.
Granite and basalt are both igneous rocks; however, basalt is considered a volcanic rock, and granite is considered a plutonic rock.
No. Granite and basalt have different compositions and form under different circumstances.