Our changing earth final
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The document contains a series of multiple choice questions related to landforms, weathering, erosion, deposition, minerals, rocks, and soil. The questions cover topics such as how sedimentary rock can change into metamorphic rock through heat and pressure under the earth's surface, and how the composition of sand, silt and clay in soil affects how well plants can take up water and nutrients.
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Metamorphic Rocks
Sandstone forms from cemented sand grains through compaction and cementation. Shale forms from compacted clay and mud sediments. Coal forms from compacted organic material. Limestone forms from cemented calcium carbonate sediments and shells. Sedimentary rocks like sandstone, shale, and limestone can contain fossils.
Sedimentary Rocks
The document discusses different types of igneous and sedimentary rocks. It states that igneous rocks form from cooled magma and their crystal size depends on the cooling rate, with slowly cooled rocks like granite having large crystals and quickly cooled rocks like basalt or pumice having small or no crystals. It describes sedimentary rocks as forming from compacted and cemented sediments, including pieces of other rocks, once-living things like plants and shells, and liquid solutions that leave impressions of fossils.
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Diamonds were originally found in river deposits in India and Borneo, but are now primarily mined from South Africa, other parts of Africa, and Siberia. Diamonds are transparent crystals made of pure carbon that can appear colorless, white, yellow, green, blue or brown. Due to their extreme hardness and density, diamonds are highly valuable and commonly used in jewelry.
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The document summarizes geological information from a field assignment, including descriptions of different rock samples found in various environments. It discusses the rocks chert, granite, sandstone, phyllite, and marble. It also covers the San Andreas Fault, sedimentary environments, weathering processes, examples of erosion and mass wasting, and the practical use of geology at a local power plant.
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This document summarizes different types of rocks found in Parkfield, California through descriptions and photos provided by a geologist. It describes sedimentary rocks like marine sediment containing seashell fossils over 10 million years old. It also describes igneous rocks like volcanic rocks with gas pockets and granite from Yosemite. Additionally, it summarizes a metamorphic rock sample from the Calaveras formation displaying changes from heat and pressure. The document credits the geologist Andy Snyder for providing the rock samples and information.
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The document discusses different types of igneous and sedimentary rocks. It states that igneous rocks form from cooled magma and their crystal size depends on the cooling rate, with slowly cooled rocks like granite having large crystals and quickly cooled rocks like basalt or pumice having small or no crystals. It describes sedimentary rocks as forming from compacted and cemented sediments, including pieces of other rocks, once-living things like plants and shells, and liquid solutions that leave impressions of fossils.
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This document summarizes different types of rocks found in Parkfield, California through descriptions and photos provided by a geologist. It describes sedimentary rocks like marine sediment containing seashell fossils over 10 million years old. It also describes igneous rocks like volcanic rocks with gas pockets and granite from Yosemite. Additionally, it summarizes a metamorphic rock sample from the Calaveras formation displaying changes from heat and pressure. The document credits the geologist Andy Snyder for providing the rock samples and information.
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The document discusses several types of rocks and geological concepts:
- Blueschist, a metamorphic rock formed under high pressure and relatively cool temperatures in subduction zones.
- Igneous rocks such as granite and gabbro found in San Luis Obispo, formed from intrusive and extrusive processes. Extrusive scoria is also mentioned.
- Sandstone, a sedimentary rock found in Poly Canyon consisting of cemented quartz and sand.
- The San Andreas Fault as an example of a transform fault still actively moving plates.
- Examples of mechanical and chemical weathering processes.
- Evidence of mass wasting and erosion seen in Yosemite National Park streams and waterfalls.
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c.
Roundness doesn't mean anything; the hardness of a mineral impacts how far clasts can travel
d.
Angular clasts have travelled further than rounded clasts
10. Which of the following rocks is NOT a biochemical sedimentary rock?
a.
Dolostone
b.
Travertine
c.
Chert
d.
Coal
e.
Limestone
11. A rock that has clasts that are bigger than 2mm that are rounded, What is that?. (one word, spelled correct, no punctuation).
12. Potash, Salt, and Gypsum are chemical rocks formed by this process, process name?
14. What two factors impact how a rock will be metamorphosed?
a.
Rate of Cooling and Pressure
b.
Pressure and Depth of Burial
c.
Heat and Depth of Burial
d.
Heat and Pressure
15: Metamorphism of rocks causes the recrystallization of minerals, resulting in smaller crystal sizes.
Select one:
True
False
16: The parallel alignment or layering of mineral grains due to metamorphism is called what?
18. Why do you not find fossils in igneous and metamorphic rocks?
a.
The textures of these rocks makes it impossible to see the fossils
b.
The heat and pressure used to form these rocks would destroy any fossils
c.
The fossils are replaced by crystals of new minerals
d.
Yes you do, they are just too small to see.
.
2 ROCKS.pptx
The document discusses different types of rocks. It describes that rocks are classified based on how they were formed into three main types: igneous, sedimentary, and metamorphic. Igneous rocks form from the cooling and solidification of magma either below ground as plutonic igneous rocks or above ground as volcanic igneous rocks. Sedimentary rocks form from the compaction and cementation of sediments. Metamorphic rocks form from the transformation of existing rocks through heat, pressure, and chemically active fluids in a process called metamorphism.
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- 1. Mr. Ball’s 4th Grade
- 2. A landforms b. sediment c. deposition d. weathering
- 3. A. physical b. chemical c. lava d. deposition
- 4. a. weathering b. landforms c. erosion d. delta
- 5. A. sediment b. delta c. dunes d. glaciers
- 6. a. physical weathering b. chemical weathering c. erosion d. deposition
- 7. A. Volcano b. Island c. glacier d. delta
- 8. A. magma b. dunes c. glaciers d. icebergs
- 9. A glaciers b. desserts c. dunes d. igneous
- 10. A physical b. chemical c. erosion d. deposition
- 11. A. mass effect b. mass movement c. masquerade d. landforms
- 12. A. luster b. mineral c. streak d. sediment
- 13. A. mineral b. luster c. streak d. hardness
- 14. A. luster b. mineral c. gem d. fungi
- 15. A. talc b. quartz c. diamond d. topaz
- 16. A Molten b. Metamorphic c. Igneous d. Sedimentary
- 17. A. Igneous b. Metamorphic c. Lava d. Sedimentary
- 18. A. Sedimentary b. Metamorphic c. Igneous d. Molten
- 19. A. dirt b. humus c. fungus d. erosion
- 20. A. mountain b. canyon c. glacier d. sand dune
- 21. A. crops b. humus c. soil d. particles
- 22. Sedimentary rock is changed into metamorphic rock by heat and pressure deep under the earth’s surface
- 23. The amount of sand, silt, and clay affect how well plants can soak up water and nutrients and how well a plants roots can spread.