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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. Biochemical sedimentary rock; it's made from cryptocrystalline quartz. Examples - flint and jasper.
Shield volcano
Silicate minerals
Loam
Chert
2. Equant - meaning that they have the same dimensions in all directions. Or inequant - meaning their dimensions are not the same in all directions.
Five steps of clastic sedimentary rock formation
Soil Horizons
Grain sizes
Metals
3. Rock formations still attached to the Earth's crust.
Bedrock
Ultramafic
Magma's speed of flow
Zone of leaching
4. 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.
Basaltic magma
Geothermal gradient
Explosive eruptions
Magnetic anomaly
5. A mineral's growth that is uninhibited - has well-formed crystal faces.
Fragmental igneous rocks
Rock layering
Euhedral crystal
Siliceous rocks
6. The distance of the deepest well ever drilled - hole in northern Russia. Penetrates only about 0.03% of the Earth.
Crystalline igneous rocks
Ash
Residual soil
12km
7. Mineral group; olivine group - pyroxene group - amphibole group.
Crystal lattice
Dark Silicates
Volcanic blocks/bombs
Carbonates
8. 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
Polymorphs
Color
Crystal
Lava tube
9. The removal of soil by running water or by wind.
The effect of the environment on eruptive style
Assimilation
Soil erosion
Lithosphere
10. 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.
Crystal lattice
Oxidation
Siltstone and mudstone
Solid-state diffusion
11. 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.
Euhedral crystal
Decompression
Rock-forming silicate minerals
Convergent plate boundary
12. 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.
Streak
Hot spots
Heat transfer
Chemical sedimentary rocks
13. Lava flow; associated with felsic magma - consists of ash and pumice fragments - material is propelled from the vent at a high speed.
Intermediate
Mantle plume
Pyroclastic flows
C-horizon
14. 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
Magnetic anomaly
Sea-floor spreading
Seamount chains
15. A process occurring when the sea level rises - the coast migrates inland. Through this - an extensive layer of beach forms.
pahoehoe
Outer core
Sea-floor spreading
Transgression
16. 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.
Dike
Differential weathering
Bed
Basaltic composition
17. 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
Grain sizes
Why magma rises
Volcanic blocks/bombs
Sulfides
18. Process occurring after sediment has been compacted - can then be bounded together to make coherent sedimentary rock. Binding material consists of minerals (commonly quartz or calcite).
Transition zone
Cementation
C-horizon
Fragmental igneous rocks
19. 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.
Differential weathering
Mid-ocean ridges
Hot spots
Stratagraphic formation
20. 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.
A-horizon
Loam
Quartz sandstone
Diagenesis
21. Solids composed of metal atoms (such as iron - aluminum - copper - and tin). Within this type of solid - outer electrons are able to flow freely.
Felsic - intermediate - mafic - ultramafic
Crystal
Metals
Light silicates
22. 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 -
Magnetic reversals
Topography
Mid-ocean ridges
Calderas
23. 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.
Cross beds
Zone of accumulation
Carbonate rocks
Agrillaceous rocks
24. A cut and finished stone ready to be used in jewelry. Examples - diamond - ruby - sapphire - emerald.
Gem
Elemental composition of Earth
Dike
Hot-spot track
25. 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
Tephra
Volcanic pipes/necks
collision
Mineral crystal destruction
26. 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.
Crystal lattice
Large Igneous Provinces (LIPs)
O-horizon
Gabbro
27. 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.
Continental shelf
C-horizon
Biomineralization
Transition zone
28. Magma type; contains about 66% to 76% silica. Name reflects the occurrence of feldspar and quartz in rocks formed in this magma.
Hot spots
Felsic
Oxidation
Rhyolitic lava flows
29. Rock made by the freezing of magma underground - after it has pushed its way (intruded) into preexisting rock of the crust.
Intrusive igneous rock
Frost wedging
Stratagraphic formation
Asthenosphere
30. An ultramafic rock with large grains. intrusive - phaneritic igneous rock.
Sedimentary rocks
Carbonates
Peridotite
Pyroclastic debris
31. 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.
Volatiles
Transform fault
Decompression
Soil
32. A name for any kind of unconsolidated debris that covers bedrock. Includes both soil and accumulations of sediment that have not evolved into soil.
Regolith
Clastic sedimentary rocks
Felsic - intermediate - mafic - ultramafic
Viscosity
33. The broad - relatively flat regions of the ocean that lie at a depth of about 4-5km below sea level.
Stoping
Apparent polar-wander path
Abyssal plains
Batholiths
34. 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
Salt wedging
Tephra
Magnetic declination
35. Active hot-spot volcanoes commonly occur at the end of a chain of dead volcanoes.
Bathymetry
Conchoidal fractures
collision
Hot-spot track
36. Two different minerals which have the same composition but have different crystal structures.
Euhedral crystal
Magma
Topography
Polymorphs
37. A fine spray of lava instantly freezes to form fine particles of glass.
triple junction
Mafic
Turbidity current
Ash
38. 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.
Sandstone
Volatiles
Shield volcano
Compaction
39. A vent at Which melt from inside the Earth spews onto the planet's surface. Erupt.
Volcano
Tuff
Siliceous rocks
Pyroclastic flows
40. When silt and clay accumulate in the flat areas bordering a stream - lagoon - or delta - the silt when lithified becomes this type of sediment. And the mud - when lithified - becomes another type of sediment - also known as shale.
Batholiths
Chemical sedimentary rocks
Peridotite
Siltstone and mudstone
41. Type of magma; low in silica - fluid - crystallize at high temperatures.
Frost wedging
Rock composition
collision
Basaltic magma
42. Mineral class; the anion within these types of minerals is a halogen ion (such as chlorine or fluorine).
Halides
Asthenosphere
triple junction
Cementation
43. Forms from a chemical reaction between solid calcite and magnesium-bearing groundwater.
Clastic
Soil erosion
Dolostone
Weathering
44. Blocks of rock that are solid and durable but composed of rough quartz sand grains cemented together.
Sandstone
Fractional crystallization
Deposition
Specific gravity
45. The boundary between two beds is a bedding plane; several beds constitute this structure.
Turbidity current
Strata
Andesitic lava flows
Magma mixing
46. Physical property of a mineral; a measure of a minerals relative ability to resist scratching - and therefore represents the resistance of bonds in the crystal structure being broken. The atoms or ions in crystals of a hard mineral are more strongly
Light silicates
Apparent polar-wander path
Clastic
Hardness
47. Sedimentary rock composed of clay.
Arkose
Superplumes
Transgression
Agrillaceous rocks
48. If a stoped block does not melt entirely - but rather becomes surrounded by new igneous rock - it becomes this; xeno - meaning foreign.
Quartz sandstone
Xenolith
Agrillaceous rocks
Rocks
49. The transformation of loose sediment into solid rock.
Magnetic anomaly
Lithification
Oxides
Deposition
50. Chemical weathering occurring in warm - wet climates can produce a layer of rotten rock - over 100km thick.
Saprolite
Agrillaceous rocks
Lower mantle
Continental shelf
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