Lab 6 igneous rock samples red granite rhyolite diorite gabbro gray granite obsidian andesite basalt rhyolite tuff pumice lab 6 igneous rock samples red granite rhyolite diorite gabbro gray granite obsidian andesite basalt rhyolite tuff pumice lab exercise 2.
Basalt and granite samples.
Magma volcanism and igneous rocks every igneous rock has a story to tell that geologists can unravel by considering the rock s.
In the first region rt to 400 k for basalt and rt 450 k for granite samples the electrical resistivity exhibits a slight decrease.
Basaltic crust is dark and thin and heavy while granite is light and accumulates into continent sized rafts which bob about like corks in this sea of basalt.
In the second region 400 to 1000 k for basalt and 450 to.
Rest 35 of basaltic samples is evaporation dominance.
Also gabbro has no alkali feldspar only plagioclase feldspar with a high calcium content.
The evaporation increases salinity by increasing na and cl and thus tds.
Basalt and granite are two types of igneous rocks.
As it turns out most of the ocean floor is basalt and most of the continents are granite.
Unlike granite gabbro is low in silica and has no quartz.
Granite is an intrusive rock with few contaminants while basalt is an extrusive rock with many contaminants.
Igneous rock specimens in packs of 10 or as hand samples.
It had shown about 65 in the basalt and 100 in the granite of the samples representing the influence of chemical weathering for rock forming minerals on the groundwater quality by dissolution of host rock minerals.
Earth contains three kinds of rocks namely igneous rocks sedimentary rocks and metamorphic rocks.
Granite is the principal component of the continental crust while basalt is the principal component of the oceanic crust.
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.
Igneous rocks are formed through the cooling and solidification of magma or lava and they may form with or without crystallization.