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Geology
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Subject
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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. Type of lava flow; higher silica content - greater viscosity - forms a large mound above the vent out of a volcano.
Redbeds
E-horizon
Facets
Andesitic lava flows
2. The layering nature of sedimentary rocks - surface features of layers formed during deposition - and the arrangement of grains within layers.
12km
Marine magnetic anomaly
Fracture and cleavage
Sedimentary structure
3. A place where three plate boundaries intersect at a point.
Stoping
Plate tectonics
triple junction
Basaltic lava flows
4. A name for any kind of unconsolidated debris that covers bedrock. Includes both soil and accumulations of sediment that have not evolved into soil.
Paleopole
Extrusive igneous rock
Magnetic declination
Regolith
5. An ultramafic rock with large grains. intrusive - phaneritic igneous rock.
Chert
Peridotite
Magnetic inclination
Redbeds
6. 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.
Fracture zones
Zone of leaching
Siltstone and mudstone
Fractional crystallization
7. A vent at Which melt from inside the Earth spews onto the planet's surface. Erupt.
Heat transfer
Graded bed
Volcano
Transition zone
8. Sedimentary rock composed of calcite or dolomite.
Cross beds
Andesitic lava flows
Igneous rocks
Carbonate rocks
9. A rock made of solid mass of glass - or of tiny crystals surrounded by glass. Reflect light as glass does and tend to break conchoidally. Examples - obsidian - tachylite - pumice.
Glassy igneous rocks
Lapilli
Residual soil
Saprolite
10. An insulated - tunnel-like conduit through which lava moves within a flow.
Frost wedging
Lava tube
Fracture and cleavage
Columnar jointing
11. Refers to the arrangement of grains in a rock; that is - the way the grains connect each other and whether inequant grains are aligned parallel to one another.
Rock texture
Crystal lattice
Continental drift evidence
Mineral crystal destruction
12. The Earth radiated heat into space and slowly cooled. Eventually - the early formed sea of lava solidified and formed igneous rock. The cumulative effect of radioactivity has been sufficient to slow the cooling of the planet and subsequently allow fo
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13. Core division; between 2900 and 5155km deep. Liquid iron alloy - it exists as a liquid because the temperature here is so high that even the great pressures squeezing the region cannot lock atoms into a solid framework. This liquid iron alloy is able
Alloy
Fractional crystallization
Continental drift hypothesis
Outer core
14. Alfred Wegener's suggestion that the positions of the continents change through time as they drift away from each other. The flaw was that he lacked a plausible moving mechanism.
Continental drift hypothesis
Pyroclastic debris
Magma
Fractional crystallization
15. 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
Weathering
Loam
The effect of gas pressure on eruptive style
Slab-pull force
16. Lava flowing on dry land cools more slowly that lava erupting underwater.
The effect of the environment on eruptive style
Residual soil
Granitic magma
Area of igneous activity
17. 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
Differential weathering
A-horizon
Depositional environment
The effect of viscosity on eruptive style
18. The compiled data from many marine cruises which defined a distinctive - striped and alternating bands of paleomagnetism.
Saprolite
Intrusive igneous rock
Cement
Marine magnetic anomaly
19. A sheet of tuff formed from a pyroclastic flow.
Ignimbrite
Pyroclastic flows
a'a'
Organic sedimentary rocks
20. 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.
Soil
Lapilli
Special properties of minerals
Thermal expansion
21. Forms from a chemical reaction between solid calcite and magnesium-bearing groundwater.
Volatiles
Dolostone
Divergent plate boundary
Laterite
22. A sediment-filled depression; in an area where the lithosphere has subsided.
B-horizon
Conchoidal fractures
Erosion
Sedimentary Basins
23. The intrusion of numerous plutons in a region - produces a vast composite body that may be several hundred kilometers long and over 100km wide; an immense body of igneous rock.
Batholiths
Slab-pull force
Mantle plume
Crystal habit
24. 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.
Polymorphs
Topography
Oxides
Dike
25. Mineral crystal formation type; form at interfaces between the physical and biological components of the Earth system by this process.
Biomineralization
A-horizon
Saprolite
Fumerolic mineralization
26. Process that occurs after the sediment has been buried - pressure cause by the overburden squeezes out water and air that had been trapped between clasts - and the clasts press together tightly.
Physical weathering
Euhedral crystal
Coal
Compaction
27. Type of igneous rock composition; composed of light-colored silicates - very rich in felsic (feldspar and silica). Major constituent of continental crust.
Loam
Granitic composition
Carbonate rocks
Zone of accumulation
28. A reference to the sinking of the lithosphere; allows for sediment to accumulate in regions where this occurs.
Intermediate
Shield volcano
Subsidence
Root wedging
29. Center of the Earth - consists mainly of iron alloy.
12km
Tephra
Dike
The core
30. A mineral's growth that is uninhibited - has well-formed crystal faces.
Plutons
pahoehoe
Deposition
Euhedral crystal
31. 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.
Rhyolitic lava flows
Plutons
Magnetic declination
Upper mantle
32. Occurs within the asthenosphere - actively drags plates along and attributes partially for the mechanism shifting the plates along the Earth's surface.
Hardness
Spreading rate
Convective flow
Weathering
33. Along much of the perimeter of the Pacific Ocean - the ocean floor reaches astounding depths of 8-12km. These areas define elongate troughs - and they border volcanic arcs - the curving chains of active volcanoes.
Laterite
O-horizon
Cross beds
Deep-ocean trenches
34. A felsic rock with large grains. Intrusive - phaneritic igneous rock.
Transform fault
ravertine
Saprolite
Granite
35. The most important mineral group; comprise the most rock-forming minerals - they are very abundant due to large % of silicon and oxygen in Earth's crust. Examples - oxygen - silica - aluminum.
Five steps of clastic sedimentary rock formation
Dissolution
Rock-forming silicate minerals
Fumerolic mineralization
36. The broad - relatively flat regions of the ocean that lie at a depth of about 4-5km below sea level.
Frost wedging
Regression
Abyssal plains
A-horizon
37. Mineral group; feldspars - quartz - muscovite - clay minerals.
Intermediate
Light silicates
Dike
Sedimentary structure
38. Subsoil - ions and clay leached and transported down from above accumulate here. As a result - new minerals form - and clay fills open spaces. Part of the zone of accumulation.
Erosion
Explosive eruptions
Plates
B-horizon
39. If a stoped block does not melt entirely - but rather becomes surrounded by new igneous rock - it becomes this; xeno - meaning foreign.
Upper mantle
Xenolith
Saprolite
Bedding
40. The rate of increase in temperature - decreases with increasing depth. The dashed lines represent the solidus and liquidus for mantle rock (peridotite). The solidus line defines the conditions of pressure and temperature at Which mantle rock begins t
Composite cone (stratovolcano)
A-horizon
Geothermal gradient
Differential weathering
41. Type of volcanic eruption; produce mainly lava flows - yield low-viscosity basaltic lavas.
Effusive eruptions
Area of igneous activity
Dunes
Tephra
42. A reference to the pattern structure of a mineral. A material in which atoms are fixed in an orderly pattern - a crystalline solid.
Crystal lattice
Solid-state diffusion
Magnetic anomaly
Fumerolic mineralization
43. Forms a 2885-km-thick layer surrounding the core. In terms of volume - it is the largest part of the Earth. It consists entirely of ultramafic rock - peridotite.
Mantle
Polymorphs
Slab-pull force
Weathering
44. Rocks that forms by the freezing of lava above ground - after it spills out (extrudes) onto the surface of the Earth and comes into contact with the atmosphere or ocean.
12km
Rock layering
Continental rift
Extrusive igneous rock
45. A plate boundary at which one plate slips along the side of another plate. No new plate is formed and no old plate is consumed. But the grinding between the plates generates frequent and destructive earthquakes.
Transform plate boundary
Volatiles
Sandstone
Convective flow
46. An intrusion starting to inject between layers but then dome upwards - creating this blister-shaped intrusion.
Laccolith
Streak
Intrusive igneous rock
Crystal structure
47. Elongate submarine mountain ranges whose peaks lie only about 2-2.5km below sea level. Consist of a ridge axis - are roughly symmetrical - and can include escarpments - axial troughs - and valleys. Examples - Mid-Atlantic Ridge - East Pacific Rise -
Mid-ocean ridges
Silicate minerals
Oxidation
Fracture and cleavage
48. Type of sedimentary rock; rocks whose grains are stuck together by cement.
Symmetry
Rocks
Compaction
Clastic
49. Natural bond connecting rocks; mineral material that precipitates from water and fills the space between grains.
Fragmental igneous rocks
The effect of the environment on eruptive style
Cement
Magnetic reversals
50. A type of soil consisting of about 10-30% clay and the rest silt and sand. Pores remain between grains so that water and air can pass through and roots can easily penetrate.
Lithosphere
Sedimentary rocks
Sill
Loam
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