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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 mafic rock with small grains. Extrusive - aphanitic igneous rock.
Light silicates
Transported soil
Basalt
Heat transfer
2. Forms when clots of lava fly into the air in lava fountains and then freeze to form solid chunks before hitting the ground. Some forms when the explosion of a volcano shatters preexisting rock and ejects the fragments over the countryside.
Pyroclastic debris
Conchoidal fractures
Plates
Lava tube
3. Magma type; contains about 45% to 52% silica. Named because it produces rock containing abundant mafic minerals - magnesium and iron combinations.
Pyroclastic flows
650-1100 degrees C
Mafic
a'a'
4. 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.
Granite
O-horizon
Cinder cone
Evaporites
5. A distinctive sequence of strata traced across a fairly large region. For example - a region may contain a succession of alternating sandstone and shale beds deposited by rivers - overlain by beds of marine limestone deposited later.
Diagenesis
Stratagraphic formation
Mantle plume
Sedimentary Basins
6. Magma is less dense than surrounding rock - and thus is buoyant. Magma is less dense both because rock expands as it melts and because magma tends to contain smaller proportions of heavy elements. Also - magma rises because the weight of overlying ro
O-horizon
Glassy igneous rocks
Why magma rises
Glass
7. 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
Intrusive igneous rock
Fracture and cleavage
Volcano
Residual soil
8. Occurs within the asthenosphere - actively drags plates along and attributes partially for the mechanism shifting the plates along the Earth's surface.
Mid-ocean ridges
Volatiles
Convective flow
Abyssal plains
9. Rocks that consist of mineral crystals that intergrow when the melt solidifies - interlocking structure. Examples - granite and rhyolite.
Gabbro
Saprolite
Effusive eruptions
Crystalline igneous rocks
10. During the final stages of cooling - lava flows contract and may fracture into roughly hexagonal columns.
Hot-spot track
Columnar jointing
Carbonate rocks
Effusive eruptions
11. The way in which the atoms are packed together within a mineral by chemical bonds. Five difference types of bonding can occur - covalent - ionic - metallic - Van der Waal's - and hydrogen.
Chemical weathering
Luster
Crystal structure
Organic chemicals
12. Times when the Earth's magnetic field flips from normal to reversed polarity - or vice versa. When the Earth has reversed polarity - the south magnetic pole lies near the north geographic pole - and the north magnetic pole lies near the south geograp
Soil erosion
Asthenosphere
Magnetic reversals
Phreatomagmatic eruptions
13. Similar to ripples - but are much larger. Small ripples often form on the surface of these structures.
Dunes
Stratagraphic formation
Continental shelf
Composite cone (stratovolcano)
14. A solid in which atoms are not arranged in an orderly pattern. Forms when a liquid freezes so fast that atoms do not have time to organize into an orderly pattern.
Lithification
Rhyolitic lava flows
Halides
Glass
15. A process occurring when sea level falls - the coast migrates seaward.
triple junction
Silicate minerals
Chemical weathering
Regression
16. By melting - dissolving - or other chemical reactions.
Mineral crystal destruction
Outer core
Silicate minerals
Earth's atmosphere
17. Because different soil-forming processes operate at different depths - soils typically develop into these distinct zones. These zones can be arranged vertically into a soil profile.
Viscosity
Quartz sandstone
Soil Horizons
Strata
18. Type of volcanic eruption; pyroclastic - produce clouds and avalanches of pyroclastic debris. Gas expands in the rising magma - cannot escape. The pressure becomes so great that it blasts the lava - and volcanic rock - out of the volcano.
Viscosity
Explosive eruptions
Intrusive igneous rock
Hydration
19. Type of lava flow; the most viscous of any lava flow because it is the most silicic and the coolest in nature. Tends to accumulate in a lava dome above the vent or in short and bulbous flows 1 to 2 km long.
Columnar jointing
Rhyolitic lava flows
Volcanic blocks/bombs
Fracture and cleavage
20. Fluid basaltic lava extruded from crustal fractures called fissures.
Deposition
Fissure eruptions/lava plateaus
Dolostone
Ripples
21. A plate boundary at which two plates move toward one another so that one plate sinks beneath the other. Subduction zones; Engage the sinking process known as subduction - between plates - consuming old oceanic lithosphere due to high density. Can sim
Tephra
Convergent plate boundary
Lava
Spreading rate
22. Type of volcano; most are adjacent to the Pacific - larger in size - interbedded lavas and pyroclastics - consist of alternating layers of lava and tephra - most violent type of activity - may produce nuee ardente or lahars.
Lava domes
Hydrosphere
Composite cone (stratovolcano)
Depositional environment
23. In addition to islands that rise above sea level - seamounts have been detected (isolated submarine mountains) - once volcanoes but no longer erupt.
Transported soil
Seamount chains
Cement
Elemental composition of Earth
24. A vent at Which melt from inside the Earth spews onto the planet's surface. Erupt.
Volatiles
Volcano
Silicate minerals
Fracture zones
25. 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.
Columnar jointing
Sedimentary rocks
Magnetic declination
Symmetry
26. Cause of melting; the variation in temperature with depth is expressed in the geotherm; because pressure prevents melting - a decrease in pressure can permit melting. Specifically - if the pressure affecting hot mantle rock decreases while the temper
Reason for Earth's internal heat
Decompression
Sulfides
Diagenesis
27. A reference to the supposed position of the Earth's magnetic pole at a time in the past.
Conchoidal fractures
Luster
Paleopole
Hydration
28. Rock made by the freezing of magma underground - after it has pushed its way (intruded) into preexisting rock of the crust.
Fractional crystallization
Hydration
Intrusive igneous rock
Frost wedging
29. 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.
Reason for Earth's internal heat
Volatiles
Convective flow
Metamorphic rocks
30. Mineral crystal formation type; form from a solution - meaning that atoms - molecules - or ions dissolved in water bond together out of water.
Precipitation
Explosive eruptions
B-horizon
Magma
31. Type of igneous rock composition; composed of dark silicates and calcium-rich feldspar - referred to as mafic (magnesium and iron). Make up the ocean floor/volcanic islands.
Spreading rate
Pangaea
Basaltic composition
Deposition
32. 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.
Transported soil
Fragmental igneous rocks
Mantle
Zone of leaching
33. During this process - water chemically reacts with minerals and breaks them down - working faster in slightly acidic water.
Hydrolysis
Columnar jointing
Bedrock
Slab-pull force
34. Places with particularly voluminous quantities of magma erupting or intruding.
Plutons
Transition zone
collision
Large Igneous Provinces (LIPs)
35. A reference to the sinking of the lithosphere; allows for sediment to accumulate in regions where this occurs.
Magma's speed of flow
Sill
Organic sedimentary rocks
Subsidence
36. A name for any kind of unconsolidated debris that covers bedrock. Includes both soil and accumulations of sediment that have not evolved into soil.
C-horizon
Granitic magma
Physical weathering
Regolith
37. Solids composed of metal atoms (such as iron - aluminum - copper - and tin). Within this type of solid - outer electrons are able to flow freely.
Metals
Strata
Melts
Precipitation
38. Rocks whose crystals interlock with each other.
Assimilation
Crystalline
Subsidence
Crystal
39. A nearly horizontal - tabletop-shaped tabular intrusion - parallel to layering within the earth.
Volcano
Mafic
Mid-ocean ridges
Sill
40. Most common mineral on Earth; compose over 95% of the continental crust. Consist of combinations of a fundamental building block called silicon-oxygen tetrahedron - different groups: independent tetrahedra - single chains - double chains - sheet sili
Quartz sandstone
Silicate minerals
Metals
Crust
41. 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.
Rhyolitic lava flows
Color
Subsidence
Factors of magma cooling time
42. Rock formations still attached to the Earth's crust.
Conchoidal fractures
Hydrolysis
Bedrock
Pyroclastic flows
43. 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
Divergent plate boundary
Conchoidal fractures
Zone of accumulation
Factors classifying clastic sedimentary rocks
44. Forms from a chemical reaction between solid calcite and magnesium-bearing groundwater.
Hydration
Dolostone
Outer core
pahoehoe
45. Type of sedimentary rock; rocks whose grains are stuck together by cement.
Agrillaceous rocks
Hydrosphere
Volcanic pipes/necks
Clastic
46. 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.
Ridge-push force
Mantle
Hot-spot track
Lithification
47. 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.
Special properties of minerals
Sulfates
O-horizon
Felsic - intermediate - mafic - ultramafic
48. 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.
Mantle
Igneous rocks
Fumerolic mineralization
Solid-state diffusion
49. Magma type; contains about 52% to 66% silica. Name indicates that these magmas have a composition between that of felsic and mafic magma.
Felsic - intermediate - mafic - ultramafic
Reason for Earth's internal heat
A-horizon
Intermediate
50. Distinguishing feature of magma; the composition of the melt reflects the composition of the solid from which it was derived. Not all magmas form from the same source rock - therefore not all magmas have the same compositions.
E-horizon
Inner core
Source rock composition
Dissolution
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