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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. Natural cracks that form in rocks due to removal of overburden or due to cooling.
Extrusive igneous rock
Silicate minerals
Jointing
Coal
2. Occurs within the asthenosphere - actively drags plates along and attributes partially for the mechanism shifting the plates along the Earth's surface.
Erosion
Convective flow
Abyssal plains
Mafic
3. Mineral class; the anion within these types of minerals is a halogen ion (such as chlorine or fluorine).
Thermal expansion
Halides
Pyroclastic debris
Glassy igneous rocks
4. Physical property of a mineral; refers to the color of a powder produced by pulverizing the mineral. Provides a fairly reliable clue to the mineral's identity - since the color of the mineral powder tends to be less variable than the color of the who
A-horizon
Streak
Quartz sandstone
Diagenesis
5. Physical features of the land surface represented by changes in elevation.
Topography
Grain sizes
Cross beds
Bathymetry
6. Distinct internal laminations within a ripple or dune that are inclined at an angle to the boundary of the main sedimentary layer. Form as a consequence of the evolution of dunes or ripples.
Outer core
Differential weathering
Cross beds
Magma
7. Inorganic limestone; rock composed of crystalline calcium carbonate formed by chemical precipitation.
Ripples
ravertine
Volcanic blocks/bombs
Paleomagnetism
8. Natural bond connecting rocks; mineral material that precipitates from water and fills the space between grains.
Cement
Biomineralization
Calderas
Light silicates
9. A sediment-filled depression; in an area where the lithosphere has subsided.
Sedimentary Basins
The effect of viscosity on eruptive style
3.5km (2 miles)
Mantle
10. 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
Solid-state diffusion
Ridge-push force
Volatiles
Stratagraphic formation
11. Physical property of a mineral; refers to the shape (morphology) of a single crystal with well-formed crystal faces - or to the character of an aggregate of many well-formed crystals that grew together as a group. Depends on the internal arrangement
Magma's speed of flow
Physical weathering
Factors classifying clastic sedimentary rocks
Crystal habit
12. When different rocks in an outcrop undergo weathering at different rates.
Differential weathering
Hydrosphere
Melts
Laccolith
13. A mafic rock with large grains. Intrusive - phaneritic igneous rock.
E-horizon
Fractional crystallization
Effusive eruptions
Gabbro
14. A plate boundary at which two plates move apart from one another by process of sea-floor spreading. Mid-ocean ridges or simply a ridge. New crust is formed at ridges through the buoyant rising of magma from beneath the surface and solidifies to creat
Magnetic declination
Biochemical sedimentary rocks
Divergent plate boundary
C-horizon
15. The fit of the continents - locations of past glaciations - the distribution of equatorial climatic belts - the distribution of fossils - and matching geologic units.
Turbidity current
Continental drift evidence
collision
Granite
16. The four classes of igneous silicate rocks based on the proportion of silicon to iron and magnesium. As the proportion of silicon in a rock increases - the density decreases - thus felsic rocks are less dense than mafic. In order - from greatest to l
B-horizon
Magma's speed of flow
Gabbro
Felsic - intermediate - mafic - ultramafic
17. The supercontinent; existence proposed by Wegener - suggested that the supercontinent later fragmented into separate continents that then drifted apart - moving slowly to their present positions.
Fragmental igneous rocks
Pangaea
Pyroclastic flows
Arkose
18. 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.
Flood basalts
triple junction
Assimilation
Turbidity current
19. Type of volcano; broad and slightly domed - primarily made of basaltic lava - large and erupt large volumes of lava. Form from either low viscosity basaltic lava or from large pyroclastic sheets.
Shield volcano
Slab-pull force
Strata
Compaction
20. Sphere; Surface water along with groundwater - Earth consists of 70% surface water (oceans - lakes - and streams).
Fracture and cleavage
Subduction
Volcanic pipes/necks
Hydrosphere
21. Mineral crystal formation type; form from a solidification of a melt - meaning the freezing of a liquid.
Dunes
Rocks
Soil
Melting
22. Mineral group; feldspars - quartz - muscovite - clay minerals.
Root wedging
Pyroclastic flows
Divergent plate boundary
Light silicates
23. A linear belt in which continental lithosphere pulls apart - the lithosphere stretches horizontally.
Glassy igneous rocks
The core
Continental rift
Rhyolitic lava flows
24. The conditions in which sediment was deposited. Examples - beach - glacial - and/or river environments.
Magma mixing
Arkose
Depositional environment
Magnetic declination
25. Chemical weathering occurring in warm - wet climates can produce a layer of rotten rock - over 100km thick.
3.5km (2 miles)
Topography
Saprolite
Basaltic lava flows
26. Solids composed of metal atoms (such as iron - aluminum - copper - and tin). Within this type of solid - outer electrons are able to flow freely.
Paleomagnetism
Magnetic anomaly
Metals
Organic chemicals
27. Type of soil; forms in tropical regions where abundant rainfall drenches the land during the rainy season - and the soil dries during the dry season.
Laterite
Coal
Continental drift hypothesis
Color
28. Type of lava flow; higher silica content - greater viscosity - forms a large mound above the vent out of a volcano.
Andesitic lava flows
Dipole
Diagenesis
Physical weathering
29. Type of soil; forms directly from underlying bedrock.
Residual soil
Ignimbrite
Sedimentary rocks
Volatiles
30. Irregular or blob-shaped intrusions that range in size from tens of meters across to tens of kilometers across.
Plutons
Magnetic declination
Paleomagnetism
Tephra
31. The burial and lithification of angular or rounded clasts form these types of rocks.
Specific gravity
E-horizon
Volatiles
Conglomerate
32. An ultramafic rock with large grains. intrusive - phaneritic igneous rock.
Continental shelf
Peridotite
Biochemical sedimentary rocks
Oxidation
33. Rigid outer layer of Earth - 100-150km thick. Consists of the crust plus the uppermost part of the mantle.
Fractional crystallization
Subduction
Sedimentary structure
Lithosphere
34. A mixture containing more than one type of metal atom. Example - bronze is a mixture of copper and tin.
Siliceous rocks
Mid-ocean ridges
Alloy
Ridge-push force
35. The angle between the direction that a compass needle points at a given location and the direction of the 'true' (geographic) north. Through this process - the magnetic poles never stray more than 15 degrees of latitude from the geographic pole.
Precipitation
a'a'
Deep-ocean trenches
Magnetic declination
36. Process where a convergent boundary ceases to exist when a piece of buoyant lithosphere - such as a continent or island arc - moves into the subduction zone. Yield some of the most spectacular mountains/mountain ranges on the planet including the Him
collision
Effusive eruptions
Calderas
Hot-spot track
37. A vent at Which melt from inside the Earth spews onto the planet's surface. Erupt.
Volcano
Silicate minerals
12km
Oxidation
38. 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.
Volcanic blocks/bombs
Heat transfer
Thermal expansion
Frost wedging
39. Factors; the depth of the intrusion - the deeper - the more slowly it cools. The shape and size of a magma body - the greater the surface area - the faster it cools. The presence of circulating groundwater - water passing through cools magma faster.
Factors of magma cooling time
Soil
Dunes
Explosive eruptions
40. 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.
Felsic - intermediate - mafic - ultramafic
Intrusive igneous rock
a'a'
Magnetic inclination
41. Measure of pressure or push in units of force - per unit area. 1 atm = 1.04 kilograms per square centimeter.
Facets
Dipole
atmospheres (atm)
Abyssal plains
42. A column of very hot rock that flows upward until it reaches the base of the lithosphere. In this model - such deep-mantle plumes form because heat rising from the Earth's core is warming rock at the base of the mantle. A possible explanation to the
Grain sizes
Mantle plume
Dipole
Turbidity current
43. Distinguishing feature of magma; the process where magma changes composition as it cools because formation and sinking of crystals preferentially remove certain atoms from the magma.
Subsidence
The effect of the environment on eruptive style
Fractional crystallization
Root wedging
44. A reference to the sinking of the lithosphere; allows for sediment to accumulate in regions where this occurs.
Mineral crystal destruction
Subsidence
Metamorphic rocks
Carbonates
45. Layering in metamorphic rocks.
Fragmental igneous rocks
Felsic
Composite cone (stratovolcano)
Metamorphic foliation
46. The compiled data from many marine cruises which defined a distinctive - striped and alternating bands of paleomagnetism.
Euhedral crystal
Pangaea
Marine magnetic anomaly
Organic chemicals
47. Weathering - erosion - transportation - deposition - and lithification.
Precipitation
Five steps of clastic sedimentary rock formation
O-horizon
Andesitic lava flows
48. Sea-floor spreading proponents - Hess and others realized that in order for the circumference of the Earth to remain constant through time - ocean floor must eventually sink back into the mantle. This sinking process consumes the ocean floor between
Subduction
atmospheres (atm)
Halides
Cementation
49. In addition to islands that rise above sea level - seamounts have been detected (isolated submarine mountains) - once volcanoes but no longer erupt.
Factors of magma cooling time
Seamount chains
Elemental composition of Earth
Siltstone and mudstone
50. Mineral group; olivine group - pyroxene group - amphibole group.
Cross beds
Lava
Dark Silicates
Arkose
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