Because Granite Is Less Dense Than Basalt Continents

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Structure Of The Earth Types Of Crust Structure Of The Earth

Structure Of The Earth Types Of Crust Structure Of The Earth

Granites may have biotite or other micas and might have a little hornblende but not very much.

Because granite is less dense than basalt continents. This is why the continental crust mostly composed of granite floats on oceanic crust made mostly of basalt. 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. Summary of basalt vs. Basalt can form in a few days to months whereas granite plutons can take millions of years to cool and harden.

Granite is less dense than basalt mainly because granite is made up of lighter mass minerals like quartz and feldspars without much in the way of heavier mass weightier mafic minerals like pyroxenes and hornblende. In addition the rock beneath continents is made primarily of silicon rich minerals like granite and quartz which are less dense than the magnesium rich basalt beneath the oceans. Granite is very much less dense 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. 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. Hope it helps you.

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6th Earth Science Plate Tectonics Science Matters Plate Tectonics Earth Science Matter Science

Basalt Is A Dark Fine Grained Igneous Rock With Generally 45 55 Silica Sio2 It Is Mostly Very Liquid And Feeds Effusive Hawaii Igneous Rock Basalt Igneous

Basalt Is A Dark Fine Grained Igneous Rock With Generally 45 55 Silica Sio2 It Is Mostly Very Liquid And Feeds Effusive Hawaii Igneous Rock Basalt Igneous

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Earth Structure And Composition Layers Rocks Minerals And The Rock Cycle Ppt Download

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