Explain whether or not it is possible for two igneous rocks to be composed of the same minerals, but have entirely different names? Please provide an example to go along with your explanation.

Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
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Chapter1: The Study Of Minerals
Section: Chapter Questions
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  1. Explain whether or not it is possible for two igneous rocks to be composed of the same minerals, but have entirely different names? Please provide an example to go along with your explanation.

 

 

 

 

 

 

 

 

 

 

 

 

 

2. Granite is the most common igneous rock that is found in continental crust. Basalt is the most common igneous rock found in oceanic crust. How could you easily distinguish between these two rocks?

 

 

 

 

 

 

 

 

 

 

 

 

 

 

3. In terms of maturity, explain how you can determine the distance from the source the sediments in the rock traveled?

 

 

 

 

 

 

 

 

 

 

4. If you refer to Table 1: Sedimentary Depositional Environments notice that several of the same rocks appear in different rows, associated with different depositional environments.  For example, the rock shale can be found in many different places – deep ocean, lakes, lagoons, continental shelf/slope, submarine fans.  Explain how you could determine which of the possible environments the sample of shale actually formed?

Table 1: Sedimentary Depositional Environments Modified from: Wiese, Katryn
https://fog.ccsf.edu/~kwiese/content/Classes/GeologyLabManual Spring2021.pdf and Open Geology Text: https://opengeology.org/textbook/5-weathering-erosion-and-sedimentary-rocks/
Location
Deep Ocean (Abyssal)
Common Rock Types
Typical Fossils
Sediment
very fine muds and
oozes, diatomaceous
Earth
chert, shale,
mudstone, limestone
microscopic organisms - diatoms &
coccolithophores
Submarine fan
Continental shelf & slope
graded sequences,
alternating
sand/mud
mud, possible sand
larger sediments,
sand and mud
shale, mudstone,
siltstone
shale, mudstone,
siltstone, limestone
sandstone,
conglomerate
rare
rare
Fluvial (River)
Beach (Littoral)
very well sorted sand
sandstone
Reef
Lagoon
Landslide, Fault Zone, Debris
Flow, Impact (meteorite),
Tsunami
Lake (Lacustrine)
lime mud with coral
limestone
laminated mud
mud to boulders,
angular, poorly
sorted fragments
shale
breccia
rare
bioturbation-layers disturbed by
movement of organisms
many, commonly coral
many, bioturbation-layers disturbed by
movement of organisms
varies
fine-grained mud
shale
invertebrates, rare (deep) bone beds
Swamp (Paludal)
Desert (Aeolian)
plant material
very well-sorted sand
and silt
coal
plant debris
sandstone
rare
Glacial
mud to boulders,
poorly sorted
breccia (tillite)
rare
Transcribed Image Text:Table 1: Sedimentary Depositional Environments Modified from: Wiese, Katryn https://fog.ccsf.edu/~kwiese/content/Classes/GeologyLabManual Spring2021.pdf and Open Geology Text: https://opengeology.org/textbook/5-weathering-erosion-and-sedimentary-rocks/ Location Deep Ocean (Abyssal) Common Rock Types Typical Fossils Sediment very fine muds and oozes, diatomaceous Earth chert, shale, mudstone, limestone microscopic organisms - diatoms & coccolithophores Submarine fan Continental shelf & slope graded sequences, alternating sand/mud mud, possible sand larger sediments, sand and mud shale, mudstone, siltstone shale, mudstone, siltstone, limestone sandstone, conglomerate rare rare Fluvial (River) Beach (Littoral) very well sorted sand sandstone Reef Lagoon Landslide, Fault Zone, Debris Flow, Impact (meteorite), Tsunami Lake (Lacustrine) lime mud with coral limestone laminated mud mud to boulders, angular, poorly sorted fragments shale breccia rare bioturbation-layers disturbed by movement of organisms many, commonly coral many, bioturbation-layers disturbed by movement of organisms varies fine-grained mud shale invertebrates, rare (deep) bone beds Swamp (Paludal) Desert (Aeolian) plant material very well-sorted sand and silt coal plant debris sandstone rare Glacial mud to boulders, poorly sorted breccia (tillite) rare
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