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.
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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