Wednesday, November 30, 2011

Help with Earth Science? (Rocks)?

My question is





"Select the rock type most likely to form in each situation"


Andesite, Granite, Diorite, Basalt, Peridotite, Gabbro, Rhyolite





A. Silicic magma cooling slowly in a batholith


B. Mafic magma cooling rapidly in a dike


C. Intermediate magma cooling slowly in a stock


D.Low-silica magma cooling slowly in the mantle


E. Silicic magma cooling quickly near the surface.








I give up, Ive come up with several answers because I always pick 1 rock that I think can fit in 2 of those...so can someone answer this for me?|||Andesite and Rhyolite are extrusives and can be excluded in this question. Basalt is generally an extrusive but can also be applied to shallow intrusives as well.





A. Granite: silica bearing, large-grained=slow cooling in batholith/pluton


B. Diorite: fine-grained=rapid cooling


C. Gabbro: intermediate grained larger than diorite


D. Peridotite: a classic felsic, deep crust/upper mantle and low in silica)


E. Basalt|||use your Earth Science Reference Tables|||A- Granite, It has a high silica content and the large crystals are characteristic of slow cooling.


B- Basalt, there is nothing else in that list which is mafic and contains sufficiently small crystals. Someone mentioned diorite which is coarse grained and therefore the wrong answer.


C- Diorite, Coarse grained (slow cooled) and of intermediate composition. Gabbro is most certainly not the correct answer as it is basic not intermediate.


D- Peridotite, It's the only one on the list which forms in the mantle.


E- Rhyolite, I will show why by saying why it can't be any of the others:


- Andesite cools relatively quickly but is intermediate.


- Granite is silicic but cools slowly.


- Diorite cools too slowly and is intermediate.


- Basalt cools quickly but is basic, not silicic.


- Peridotite forms too deep.


- Gabbro is a basic composition and it cools too slowly.


The only one it can therefore be is rhyolite which fits both criteria of being silicic and rapidly cooled.

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