Want this question answered?
Textures of volcanic rocks include aphantitic (mineral grains are present but microscopic) , porphyritic (some grains are visible to the naked eye), glassy (all or much of the rock lacks a crystalline structure), and vesicular (solidified gas bubbles are present).
When water combines with mineral grains, the grains become larger. The increase in size of mineral grains strains the rock material and weakens it.
When igneous rocks from a volcanic eruption cool, they can form either intrusive or extrusive rocks. Intrusive igneous rocks form when magma cools slowly beneath the Earth's surface, resulting in larger mineral grains. Examples include granite and diorite. Extrusive igneous rocks form when lava cools quickly on the Earth's surface, resulting in smaller mineral grains. Examples include basalt and pumice.
Minerals crystallize out from the water surrounding the grains and act as cement.
Clay grains
phenocryst
Yes
Textures of volcanic rocks include aphantitic (mineral grains are present but microscopic) , porphyritic (some grains are visible to the naked eye), glassy (all or much of the rock lacks a crystalline structure), and vesicular (solidified gas bubbles are present).
No pumice is not a porphyritic igneous rock, a porphyritic rock is characterized by the presence of phenocrysts (large mineral grains) and very small mineral grains with none in between. This implies that there was two different stages of cooling. Pumice is an extrusive igneous rock that cooled very quickly.
The rock is conglomerate. The other rock would be Breccia if its grains were not rounded.
I believe that porphyritic andesite is formed from volcanic ash and bits and pieces of minerals that eventually become ejected from the volcano. How the andesite becomes porphyritic is that it formed inside the volcano before being blown out of along with the magma and hot gases. You can find silver and gold specs as well as a few other metals encased by a smooth texture of solidifyed ash. Lee Durst (WVC 08)
When water combines with mineral grains, the grains become larger. The increase in size of mineral grains strains the rock material and weakens it.
Mineral grains are crystals or pieces of crystals that vary widely in chemicalcomposition
Pumice does not have grains.
volcanic ash
The process of fractional crystallization is part of igneous differentiation, where minerals crystallize at different temperatures and under complex circumstances.
The material that would normally form mineral crystals does not have time to form a crystalline structure because of very rapid cooling after volcanically erupting into the air or onto the surface. Obsidian is a volcanic glass.