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Geology
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Subject
:
science
Instructions:
Answer 50 questions in 15 minutes.
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Match each statement with the correct term.
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This is a study tool. The 3 wrong answers for each question are randomly chosen from answers to other questions. So, you might find at times the answers obvious, but you will see it re-enforces your understanding as you take the test each time.
1. Mineral crystal formation type; form from a solution - meaning that atoms - molecules - or ions dissolved in water bond together out of water.
Precipitation
Basalt
Laccolith
Mantle
2. Type of lava flow; mafic - low viscosity - extremely hot - flows very quickly.
3.5km (2 miles)
Fracture and cleavage
Basaltic lava flows
Mineral crystal destruction
3. Layering in metamorphic rocks.
Symmetry
Metamorphic foliation
Transform plate boundary
C-horizon
4. Inorganic limestone; rock composed of crystalline calcium carbonate formed by chemical precipitation.
Glass
Deposition
Cinder cone
ravertine
5. Some rock bodies appear to contain distinct formations - defined either by bands of different compositions or textures - or by the alignment of inequant grains so that they trend parallel to one another.
Rock layering
Extrusive igneous rock
Polymorphs
Crystal habit
6. In degrees Celsius - the high temperatures at which igneous rocks freeze; the freezing of liquid melt to form solid igneous rock represents the same phenomenon as the freezing of water - except at much higher temperatures.
A-horizon
Transported soil
650-1100 degrees C
Divergent plate boundary
7. Rocks whose crystals interlock with each other.
Crystalline
Effusive eruptions
Soil
Columnar jointing
8. The boundary between two beds is a bedding plane; several beds constitute this structure.
Lava tube
Strata
Melting
Factors classifying clastic sedimentary rocks
9. Solids composed of metal atoms (such as iron - aluminum - copper - and tin). Within this type of solid - outer electrons are able to flow freely.
Marine magnetic anomaly
Gabbro
Metals
Mineral
10. The force that subducting plates apply to oceanic lithosphere at a convergent boundary - arises simply because lithosphere formed 10 million years ago is denser than asthenosphere - so it can sink into the asthenosphere. Thus once an oceanic plate st
Lava
Sedimentary Basins
Soil erosion
Slab-pull force
11. A mafic rock with large grains. Intrusive - phaneritic igneous rock.
Alloy
Transition zone
Native metals
Gabbro
12. Consists of rock and sediment that has been modified by physical and chemical interaction with organic material and rainwater - over time - to produce a substrate that can support the growth of plants.
a'a'
Cement
Composite cone (stratovolcano)
Soil
13. Mineral class; consist of a metal cation bonded to the anionic group. Many form by precipitation out of water at or near the Earth's surface. Example - gypsum.
Sulfates
Frost wedging
Granite
Sandstone
14. Distinguishing feature of magma; the process where different magmas formed in different locations from different sources may come in contact within a magma chamber prior to freezing. Thus the originally distinct magmas mix to create a new - different
Stratagraphic formation
Magma mixing
Bed
Turbidity current
15. A pluton formation theory; a process during Which magma assimilates wall rock - and blocks of wall rock break off and sink into the magma.
Stoping
Plutons
Clastic sedimentary rocks
Fumerolic mineralization
16. Mineral class; consist of pure masses of a single metal - with metallic bonds. Copper and gold can appear in this way.
Geothermal gradient
Native metals
Sedimentary structure
Basalt
17. A process occurring when sea level falls - the coast migrates seaward.
Dissolution
Solid-state diffusion
Regression
Silicates
18. A layer of sediment in which grain size varies from coarse at the bottom to fine at the top.
Sedimentary structure
Graded bed
Chemical weathering
Alloy
19. Mineral class; consist of a metal cation bonded to a sulfide anion. Examples - galena and pyrite. Many have a metallic luster. Can also be considered ores with high proportions of metal within the mineral.
Xenolith
Salt wedging
Sulfides
Redbeds
20. Physical features of the land surface represented by changes in elevation.
Effusive eruptions
Dike
Mantle plume
Topography
21. Mineral class; the anion within these types of minerals is a halogen ion (such as chlorine or fluorine).
Pyroclastic flows
Halides
Viscosity
Asthenosphere
22. A sheet of tuff formed from a pyroclastic flow.
Factors of magma cooling time
Apparent polar-wander path
Ignimbrite
Sedimentary structure
23. Forms from a chemical reaction between solid calcite and magnesium-bearing groundwater.
Dolostone
Sea-floor spreading
Oxidation
Euhedral crystal
24. Lava flow; associated with felsic magma - consists of ash and pumice fragments - material is propelled from the vent at a high speed.
Pyroclastic flows
Shield volcano
Native metals
Marine magnetic anomaly
25. The distance of the deepest well ever drilled - hole in northern Russia. Penetrates only about 0.03% of the Earth.
Sea-floor spreading
12km
Intermediate
Intrusive igneous rock
26. Type of volcano; built from ejected lava fragments - cone shaped piles of tephra - steep slope angle - smaller in size - frequently occur in groups - deep craters.
Clastic sedimentary rocks
Cinder cone
Abyssal plains
Fissure eruptions/lava plateaus
27. Soil section below the A-horizon; a soil level that has undergone substantial leaching but has not yet mixed with organic material. Because it lacks organic materials - this horizon tends to be lighter than the A-horizon. Part of the zone of leaching
Dipole
Shield volcano
E-horizon
Abyssal plains
28. Soil section below the O-horizon - humus has decayed further and has mixed with mineral grains (clay - silt - and sand). Water percolating through this horizon causes chemical weathering reactions to occur and produces ions in solution and new clay m
Residual soil
Mantle
A-horizon
Laccolith
29. A linear belt in which continental lithosphere pulls apart - the lithosphere stretches horizontally.
Polymorphs
Strata
Continental rift
Caliche
30. Physical property of a mineral; represents the density of a mineral - as specified by the ratio between the weight of a volume of the mineral and the weight of an equal volume of water a 4 degrees C.
Plates
Decompression
Specific gravity
Factors classifying clastic sedimentary rocks
31. Places where intrusive igneous rock creates tabular intrusions cutting across rock that does not have layering - this nearly vertical - wall-like tabular intrusions is formed. Cut across layering within the earth.
Ultramafic
Sedimentary structure
Fracture and cleavage
Dike
32. The freely pivoting up and down compass needle's angle of tilt relative to the location upon the Earth's surface. At the equator - the specialized magnetic needle would position horizontally and at a magnetic pole it would point straight down.
Paleomagnetism
Magma mixing
Arkose
Magnetic inclination
33. Mineral class; consist of metal cations bonded by oxygen anions. Examples - hematite and magnetite. Some contain a relatively high proportion of metal atoms - and thus are ore minerals.
Oxides
Bed
Continental rift
Volcano
34. Relatively small - elongated ridges that form on a bed surface at right angles to the direction of the current flow of the rock.
Graded bed
Transform fault
Ripples
Redbeds
35. Mineral crystal formation type; from directly from a vapor - occurs around volcanic vents or around geysers. At such locations - volcanic gases or steam enter the atmosphere and cool - so certain elements cannot remain in gaseous form.
Basalt
Plutons
Fumerolic mineralization
Cement
36. A proposition in 1960 - by Princeton University professor Harry Hess - that continents drift apart because new ocean floor forms between them by this process.
Sea-floor spreading
Oxides
Graded bed
Symmetry
37. The distance that the world's deepest mine-shaft penetrates into the Earth beneath South Africa.
3.5km (2 miles)
Five steps of clastic sedimentary rock formation
Mid-ocean ridges
Fissure eruptions/lava plateaus
38. Type of magma; high silica content - viscous - liquid at temperatures as low as 700 degrees C.
Granitic magma
Ash
Ignimbrite
Basaltic magma
39. Cause of melting; when magma rises up from the mantle into the crust - it brings heat with it which raises the temperature of the surrounding crustal rock - and in some cases melting occurs.
Mineral crystal destruction
Intrusive igneous rock
Heat transfer
Lower mantle
40. Mineral crystal formation type; form at interfaces between the physical and biological components of the Earth system by this process.
Biomineralization
Halides
ravertine
Elemental composition of Earth
41. On a gem are the ground and polished surfaces made with a certain type of machine.
Outcrop
Loam
Soil
Facets
42. Develops because mid-ocean ridges lie at a higher elevation than the adjacent abyssal plains of the ocean. The surface of the sea floor overall slopes away from the ridge axis. Gravity causes the elevated lithosphere at the ridge axis to push on the
Saprolite
Polymorphs
Lapilli
Ridge-push force
43. Rocks with a fragmental texture consist of igneous fragments that are packed together - welded together - or cemented together after having solidified. Examples - pyroclastic rocks such as tuff or breccia.
Clastic
Halides
Cinder cone
Fragmental igneous rocks
44. Heat from an intense surface fire bakes and expands the outer layer of the rock. On cooling - the layer contracts - causing the outer part of the rock spall - or break off in sheet-like pieces.
Thermal expansion
Lava
Gem
Organic sedimentary rocks
45. Outer surface level of Earth; composed of granite - basalt - and gabbro. Continental: mostly about 35-40km thick . Oceanic: about 7-10km thick. Oxygen - by far the most abundant element.
Tuff
Soil Horizons
Crust
Facets
46. Sphere; Surface water along with groundwater - Earth consists of 70% surface water (oceans - lakes - and streams).
triple junction
Hydrosphere
Laccolith
Dark Silicates
47. Distinguishing feature of magma; the process where magma sits in a magma chamber before completely solidifying - it may incorporate chemicals derived from the walls rocks of the chamber.
Assimilation
Dunes
Clastic sedimentary rocks
Why magma rises
48. Tree roots that grow into joints can push those joints open in this process.
Root wedging
Polymorphs
Grain sizes
Earth's atmosphere
49. A nearly horizontal - tabletop-shaped tabular intrusion - parallel to layering within the earth.
Mantle
Sill
Crystalline igneous rocks
Viscosity
50. By melting - dissolving - or other chemical reactions.
Physical weathering
Bed
Mineral crystal destruction
Assimilation
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