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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. A sediment-filled depression; in an area where the lithosphere has subsided.
Conchoidal fractures
Sedimentary Basins
Sill
Pyroclastic flows
2. A process occurring when the sea level rises - the coast migrates inland. Through this - an extensive layer of beach forms.
Mineral
Melts
Transgression
Hardness
3. Type of soil; forms directly from underlying bedrock.
Plates
Residual soil
Subsidence
Biochemical sedimentary 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
Seamount chains
Streak
650-1100 degrees C
Continental rift
5. Highest soil horizon; consists almost entirely of organic matter and contains barely any mineral matter. Surface level has 'litter' and deeper it contains 'humus'. Part of the zone of leaching.
Divergent plate boundary
Agrillaceous rocks
O-horizon
Volcano
6. Rock made by the freezing of magma underground - after it has pushed its way (intruded) into preexisting rock of the crust.
The core
Dike
Intrusive igneous rock
Strata
7. The injection of magma within the magma chamber and conduit generates an outward pressure within the volcano. The presence of gas within the magma increases this pressure - as gas expands greatly as it rises toward the Earth's surface. Rhyolitic and
Native metals
The effect of gas pressure on eruptive style
Organic sedimentary rocks
Extrusive igneous rock
8. Physical property of a mineral; results from the way a mineral interacts with light. A mineral absorbs certain wavelengths - so the color seen represents the color wavelengths the mineral did not absorb.
Source rock composition
Erosion
Native metals
Color
9. 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.
Sulfides
B-horizon
atmospheres (atm)
Source rock composition
10. 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.
Superplumes
Convergent plate boundary
Cross beds
Chert
11. Sedimentary rocks made up of minerals that precipitate directly from water solutions.
Redbeds
Chemical sedimentary rocks
Stoping
Ripples
12. A reference to the supposed position of the Earth's magnetic pole at a time in the past.
Depositional environment
Paleopole
650-1100 degrees C
Pyroclastic flows
13. A mafic rock with small grains. Extrusive - aphanitic igneous rock.
Quartz sandstone
collision
Transported soil
Basalt
14. A mixture containing more than one type of metal atom. Example - bronze is a mixture of copper and tin.
Alloy
Plate tectonics
Chemical weathering
Glassy igneous rocks
15. Solids composed of metal atoms (such as iron - aluminum - copper - and tin). Within this type of solid - outer electrons are able to flow freely.
Rhyolitic lava flows
Why magma rises
Metals
Jointing
16. Low-viscosity (basaltic) lava flows out of a volcano easily - whereas high-viscosity (andesitic and rhyolitic) lava can clog and build pressure within a volcano. Basaltic eruptions are typically effusive and produce shield volcanoes - whereas rhyolit
Rock texture
The effect of the environment on eruptive style
Felsic
The effect of viscosity on eruptive style
17. A single - continuous (uninterrupted) piece of a crystalline solid bounded by flat surfaces called crystal faces that grew naturally as the mineral formed. Come in a variety of shapes - cubes - trapezoids - pyramids - octahedrons - hexagonal columns
Sedimentary structure
Soil
Crystal
Rhyolitic lava flows
18. Magma type; contains about 52% to 66% silica. Name indicates that these magmas have a composition between that of felsic and mafic magma.
Light silicates
Transform plate boundary
Mantle
Intermediate
19. 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.
Residual soil
Basalt
Biochemical sedimentary rocks
Heat transfer
20. 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
Ridge-push force
Redbeds
Carbonate rocks
Clastic
21. Mineral crystal formation type; form by type of diffusion - the movement of atoms or ions through a solid to arrange into a new crystal structure; process takes place very slowly.
Hot spots
Solid-state diffusion
pahoehoe
Crystal habit
22. 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.
Intermediate
Intrusive igneous rock
Xenolith
Batholiths
23. Created from preexisting rocks which undergo changes - such as the growth of new minerals in response to pressure and heat - and/or as a result of squashing - stretching - or shear.
Metamorphic rocks
B-horizon
Marine magnetic anomaly
Precipitation
24. An envelope of gas surrounding Earth consisting of 78% nitrogen (N2) and 28% oxygen (O2) - with minor amounts 1% of argon - carbon dioxide - methane - etc. And 99% of the gas in the atmosphere lies below 50km.
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25. Places with particularly voluminous quantities of magma erupting or intruding.
Large Igneous Provinces (LIPs)
Transgression
Dark Silicates
Clastic
26. 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
B-horizon
Geothermal gradient
Bed
Flood basalts
27. The compiled data from many marine cruises which defined a distinctive - striped and alternating bands of paleomagnetism.
Marine magnetic anomaly
Explosive eruptions
Crystal
Hydration
28. A vent at Which melt from inside the Earth spews onto the planet's surface. Erupt.
Volcano
E-horizon
Sulfates
Chemical sedimentary rocks
29. 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.
Dipole
Sulfides
atmospheres (atm)
Crystal structure
30. Type of volcanic eruption; takes place when water gains access to the hot rock around the magma chamber and suddenly transforms into steam - a pyroclastic eruption involving the reaction of water with magma.
Weathering
Phreatomagmatic eruptions
Glass
Compaction
31. Form when solid materials become hot and transform into liquid - example - molten rock.
Subsidence
Mineral
Ultramafic
Melts
32. Type of volcanic eruption; produce mainly lava flows - yield low-viscosity basaltic lavas.
E-horizon
Effusive eruptions
Columnar jointing
Zone of leaching
33. The process by which sediment settles out of the transporting medium.
Lava
Magnetic declination
Deposition
Laccolith
34. Unconsolidated deposits of pyroclastic grains - regardless of size - that have been erupted from a volcano constitute these pyroclastic deposits.
Fissure eruptions/lava plateaus
Peridotite
Granite
Tephra
35. 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.
Fractional crystallization
Subsidence
Deep-ocean trenches
Felsic - intermediate - mafic - ultramafic
36. Rocks whose crystals interlock with each other.
Five steps of clastic sedimentary rock formation
Soil Horizons
Stratagraphic formation
Crystalline
37. A reference to the pattern structure of a mineral. A material in which atoms are fixed in an orderly pattern - a crystalline solid.
Organic sedimentary rocks
Volcano
Crystal lattice
Laccolith
38. Volcanoes that exist as isolated points and appear to be independent of movement at a plate boundary - hot-spot volcanoes. Mostly are located on the interior of plates - away from boundaries.
Residual soil
Hydrosphere
Biochemical sedimentary rocks
Hot spots
39. Form from grains that break off preexisting rock and become cemented together - or from minerals that precipitate out of a water solution.
Basalt
Sedimentary rocks
Grain sizes
Pangaea
40. Type of rock; accumulated sand bars - within are mineral grains of quartz and feldspar - this sediment if buried and lithified.
Laterite
Arkose
Decompression
Effusive eruptions
41. 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
Alloy
Elemental composition of Earth
Magnetic reversals
42. Some minerals have distinctive properties - such as calcite which reacts with dilute hydrochloric acid to produce carbon dioxide. Dolomite also reacts with acid - graphite can make clear markings - magnetite attracts a magnet - halite tastes salty -
Special properties of minerals
Outcrop
Continental drift hypothesis
Crystal habit
43. Rocks that consist of mineral crystals that intergrow when the melt solidifies - interlocking structure. Examples - granite and rhyolite.
Transgression
Magnetic anomaly
Ash
Crystalline igneous rocks
44. Tree roots that grow into joints can push those joints open in this process.
Convergent plate boundary
Subsidence
pahoehoe
Root wedging
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.
Continental rift
Crust
Hot spots
Outer core
46. Perhaps the cause for the large igneous provinces; formations within the mantle - plumes that bring up vastly more hot asthenosphere than normal plumes.
Batholiths
Superplumes
Plates
Hot-spot track
47. The bottom portion of the upper mantle - the interval lying between 400km and 660km deep. Here within the Earth - the character of the mantle undergoes a series of abrupt changes.
Transported soil
Transition zone
Euhedral crystal
Oxides
48. Breaks intact rocks into unconnected grains or chunks - collectively called debris or detritus. Grain size from largest to smallest: boulders - cobbles - pebbles - sand - silt - mud/clay.
Spreading rate
Mineral
A-horizon
Physical weathering
49. An exposure of bedrock.
Outcrop
Factors classifying clastic sedimentary rocks
Effusive eruptions
Paleopole
50. Physical property of a mineral; different minerals fracture in different ways - depending on the internal arrangement of atoms. If a mineral breaks to form distinct planar surfaces that have a specific orientation in relation to the crystal structure
Fracture and cleavage
Hydrosphere
C-horizon
Extrusive igneous rock
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