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What else can I help you with?
Does granitic lava explode?
No Granites are usually intrusive rocks.
Which ferromagnesian minerals and which of the feldspar's would be the first minerals to crystallize?
The first ferromagnesian mineral to crystallize is usually olivine, followed by pyroxene and amphibole. Among the feldspars, plagioclase feldspar is usually the first to crystallize, followed by potassium feldspar.
What metamorphic rock does granite crystallize?
Granite usually metamorphoses into gneiss.
Which mineral is last to crystallize?
In solidifying igneous rock, usually quartz.
Why is paint usually applied on the surface of wall?
The surface of the wall is the surface you usually want to paint.
Are felsic rocks usually intrusive or extrusive?
Felsic rocks are usually intrusive, meaning they form below the Earth's surface from magma that cools and solidifies slowly. This slow cooling allows minerals such as quartz and feldspar to crystallize and form coarse-grained textures commonly seen in intrusive rocks like granite.
How do travel routes of today differ from the trade routes of classical era civilizations?
Travelers usually have multiple options for reaching a destination.
INTRUSIVE IGNEOUS ROCK ARE NOTED FOR?
Intrusive rocks, also called plutonic rocks, cool slowly without ever reaching the surface. They have large crystals that are usually visible without a microscope. This surface is known as a phaneritic texture. Perhaps the best-known phaneritic rock is granite
Is feldspar extrusive?
Feldspars are a group of common rock forming mineralsthat can appear in all rock types. The term 'extrusive' is usually used to describe an igneous rock that has formed on or near the surface.
Can you see the crystals in basalt?
Not usually unless you have a microscope. Crystals in baslat are usually microscopic. However, in some cases basalt may have a porphyritic texture, where some minerals in the magma have started to crystallize before the eruption.
Can you see crystals in basalt?
Not usually unless you have a microscope. Crystals in baslat are usually microscopic. However, in some cases basalt may have a porphyritic texture, where some minerals in the magma have started to crystallize before the eruption.
Internal friction angle of granitic rock?
The internal friction angle of granitic rock typically ranges from 30 to 45 degrees, with an average value around 35 degrees. This value may vary depending on factors such as mineral composition, weathering, and confining pressure. Granitic rocks are generally considered to have good strength and stability due to their high internal friction angle.
