Match the rock to its property, texture, and (or) mineral composition. Pahoehoe Rhyolite Granite Peridotite Porphyritic basalt Pumice Obsidian Gabbro Diorite A'a Scoria Basalt Fluid lava results in its ropy tex ✪ Aphanitic texture with quartz, Large, easily visible crystals of [Choose ] [Choose ] [Choose ] [Choose ] [Choose ] [Choose ] [Choose ] [Choose ] [Choose ] (> <> <> <> <> <> () (> Large calcium plagioclase crystals in a fine-grained background indicates two stage of cooling history. Green rock composed primarily of olivine and small amounts of pyroxene. Light colored rock with a frothy texture. Phaneritic rock consisting mostly of calcium plagioclase and pyroxene. Glassy texture results from rapid cooling. Aphanitic rock consisting mostly of pyroxene and calcium plagioclase with minor amounts of olivine and amphiboles. Fluid lava results in its ropy texture. Dark rock with numerous gas vesicles. Phaneritic rock with ampibole, biotite, and plagioclase. Contains no quartz or olivine. Broken texture results from thick, viscous lava. Aphanitic texture with quartz, potassium feldspar, and sodium plagioclase. Large, easily visible crystals of quartz and potassium feldspar.

Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
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Question
Match the rock to its property, texture, and (or) mineral composition.
Pahoehoe
Rhyolite
Granite
Peridotite
Porphyritic basalt
Pumice
Obsidian
Gabbro
Diorite
A'a
Scoria
Basalt
Fluid lava results in its ropy tex ✪
Aphanitic texture with quartz,
Large, easily visible crystals of
[Choose ]
[Choose ]
[Choose ]
[Choose ]
[Choose ]
[Choose ]
[Choose ]
[Choose ]
[Choose ]
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Transcribed Image Text:Match the rock to its property, texture, and (or) mineral composition. Pahoehoe Rhyolite Granite Peridotite Porphyritic basalt Pumice Obsidian Gabbro Diorite A'a Scoria Basalt Fluid lava results in its ropy tex ✪ Aphanitic texture with quartz, Large, easily visible crystals of [Choose ] [Choose ] [Choose ] [Choose ] [Choose ] [Choose ] [Choose ] [Choose ] [Choose ] (> <> <> <> <> <> () (>
Large calcium
plagioclase crystals in a
fine-grained background
indicates two stage of
cooling history.
Green rock composed
primarily of olivine and
small amounts of
pyroxene.
Light colored rock with a
frothy texture.
Phaneritic rock
consisting mostly of
calcium plagioclase and
pyroxene.
Glassy texture results
from rapid cooling.
Aphanitic rock consisting
mostly of pyroxene and
calcium plagioclase with
minor amounts of olivine
and amphiboles.
Fluid lava results in its
ropy texture.
Dark rock with numerous
gas vesicles.
Phaneritic rock with
ampibole, biotite, and
plagioclase. Contains no
quartz or olivine.
Broken texture results
from thick, viscous lava.
Aphanitic texture with
quartz, potassium
feldspar, and sodium
plagioclase.
Large, easily visible
crystals of quartz and
potassium feldspar.
Transcribed Image Text:Large calcium plagioclase crystals in a fine-grained background indicates two stage of cooling history. Green rock composed primarily of olivine and small amounts of pyroxene. Light colored rock with a frothy texture. Phaneritic rock consisting mostly of calcium plagioclase and pyroxene. Glassy texture results from rapid cooling. Aphanitic rock consisting mostly of pyroxene and calcium plagioclase with minor amounts of olivine and amphiboles. Fluid lava results in its ropy texture. Dark rock with numerous gas vesicles. Phaneritic rock with ampibole, biotite, and plagioclase. Contains no quartz or olivine. Broken texture results from thick, viscous lava. Aphanitic texture with quartz, potassium feldspar, and sodium plagioclase. Large, easily visible crystals of quartz and potassium feldspar.
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