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Test your basic knowledge |
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. Sublayer of the mantle - depth of 660km.
Soil erosion
Upper mantle
Granite
Hardness
2. 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
Rock composition
Felsic - intermediate - mafic - ultramafic
Carbonate rocks
Why magma rises
3. Similar to ripples - but are much larger. Small ripples often form on the surface of these structures.
Dunes
Magnetic inclination
Biochemical sedimentary rocks
Earth's atmosphere
4. The distance that the world's deepest mine-shaft penetrates into the Earth beneath South Africa.
Turbidity current
Reason for Earth's internal heat
Cementation
3.5km (2 miles)
5. Rock formations still attached to the Earth's crust.
Oxidation
Continental rift
Pyroclastic flows
Bedrock
6. Layering in metamorphic rocks.
Partial melting
Volcanic blocks/bombs
Crystalline igneous rocks
Metamorphic foliation
7. The nature of Earth's magnetic field - like the familiar magnetic field around a bar magnet - has a North and South pole. The magnetic field is drawn with field lines - the paths along Which magnets would align - or charged particles would flow - if
Phreatomagmatic eruptions
Continental rift
a'a'
Dipole
8. Magma type; contains about 45% to 52% silica. Named because it produces rock containing abundant mafic minerals - magnesium and iron combinations.
Plate tectonics
E-horizon
Rock composition
Mafic
9. 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
collision
Crystal habit
Mineral crystal destruction
Salt wedging
10. 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.
Rock composition
Divergent plate boundary
Transition zone
The core
11. 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.
Outcrop
collision
Soil erosion
Source rock composition
12. Molten rock beneath Earth's surface.
Magma
Outcrop
Mineral
Luster
13. 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
Andesitic lava flows
Conchoidal fractures
Color
Ridge-push force
14. 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.
rifting
Relative plate velocity
Clastic sedimentary rocks
Soil
15. 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.
Soil Horizons
Oxides
Magnetic reversals
Gem
16. Mineral crystal formation type; form at interfaces between the physical and biological components of the Earth system by this process.
Crystalline igneous rocks
Bedrock
Transported soil
Biomineralization
17. Unconsolidated deposits of pyroclastic grains - regardless of size - that have been erupted from a volcano constitute these pyroclastic deposits.
Fracture and cleavage
Tephra
Conglomerate
Metamorphic rocks
18. 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
Frost wedging
Arkose
Streak
Convergent plate boundary
19. 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.
ravertine
Mantle
The effect of viscosity on eruptive style
Cinder cone
20. During the final stages of cooling - lava flows contract and may fracture into roughly hexagonal columns.
Gem
Basaltic magma
Reason for Earth's internal heat
Columnar jointing
21. A felsic rock with large grains. Intrusive - phaneritic igneous rock.
Glass
Rhyolitic lava flows
Granite
Magma mixing
22. Some rock bodies appear to contain distinct formations - defined either by bands of different compositions or textures - or by the alignment of inequant grains so that they trend parallel to one another.
Laccolith
Continental rift
Rock layering
Sea-floor spreading
23. 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
The effect of gas pressure on eruptive style
Why magma rises
Laterite
Bathymetry
24. Process where new divergent boundaries form when a continent splits and separates into two continents.
rifting
Dark Silicates
Soil Horizons
Sill
25. A mixture containing more than one type of metal atom. Example - bronze is a mixture of copper and tin.
Explosive eruptions
Chert
Alloy
Columnar jointing
26. Two different minerals which have the same composition but have different crystal structures.
Fracture and cleavage
Felsic - intermediate - mafic - ultramafic
Polymorphs
Dark Silicates
27. A linear belt in which continental lithosphere pulls apart - the lithosphere stretches horizontally.
Sedimentary structure
Bedding
Agrillaceous rocks
Continental rift
28. 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
Oxides
Inner core
Marine magnetic anomaly
Divergent plate boundary
29. Theory confirmed by 1968 - geologists had developed the complete model of continental drift - sea-floor spreading - and subduction. Within this model - Earth's lithosphere consists of about 20 distinct pieces - or plates - that move relative to each
Solid-state diffusion
Effusive eruptions
Hot spots
Plate tectonics
30. A reference to the supposed position of the Earth's magnetic pole at a time in the past.
a'a'
Viscosity
12km
Paleopole
31. Rocks whose crystals interlock with each other.
Convergent plate boundary
Crystalline
Magma mixing
Weathering
32. The layering nature of sedimentary rocks - surface features of layers formed during deposition - and the arrangement of grains within layers.
Transition zone
Sedimentary structure
Glassy igneous rocks
The effect of gas pressure on eruptive style
33. 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.
Pangaea
Mantle plume
Relative plate velocity
Crust
34. A cut and finished stone ready to be used in jewelry. Examples - diamond - ruby - sapphire - emerald.
Gem
Transported soil
E-horizon
Rock composition
35. Refers to the chemical reactions that alter or destroy minerals when rock comes in contact with water solutions or air.
Chemical weathering
Special properties of minerals
Crystal habit
Fragmental igneous rocks
36. Type of rock; accumulated sand bars - within are mineral grains of quartz and feldspar - this sediment if buried and lithified.
Chemical sedimentary rocks
Arkose
Batholiths
Effusive eruptions
37. The absorption of water into the crystal structure of minerals - causes some minerals to expand.
Hydration
Glassy igneous rocks
Mantle plume
Fragmental igneous rocks
38. Type of sedimentary soil/rock; Calcite in a pedocal soil accumulates in the B-horizon and may cement soil together - creating this solid mass.
Erosion
Caliche
Pangaea
Mid-ocean ridges
39. Mineral class; the molecule CO23 serves as the anionic group. Elements like calcium or magnesium bond to this group. Examples - calcite and dolomite.
Mineral crystal destruction
Upper mantle
Pyroclastic debris
Carbonates
40. 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.
Pyroclastic flows
Shield volcano
Redbeds
Lapilli
41. Type of igneous rock composition; composed of light-colored silicates - very rich in felsic (feldspar and silica). Major constituent of continental crust.
Redbeds
Melts
Granitic composition
Silicate minerals
42. During this process - water chemically reacts with minerals and breaks them down - working faster in slightly acidic water.
Hydrolysis
Conglomerate
Transported soil
Limestone
43. The display of the pattern of atoms or ions within a mineral. Meaning that the shape of one part of a mineral is a mirror image of the shape of another part.
Shield volcano
Symmetry
A-horizon
Fractional crystallization
44. Sedimentary rock composed of calcite or dolomite.
Carbonate rocks
Grain sizes
Abyssal plains
Mineral
45. 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.
Mineral crystal destruction
Bedding
Hot spots
Erosion
46. A place where three plate boundaries intersect at a point.
Conchoidal fractures
Metamorphic rocks
Ash
triple junction
47. A process occurring when the sea level rises - the coast migrates inland. Through this - an extensive layer of beach forms.
Reason for Earth's internal heat
Transgression
Decompression
Flood basalts
48. 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.
Limestone
Metamorphic rocks
Ash
Cementation
49. 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
Granitic composition
pahoehoe
Dolostone
50. Pea to plum-sized fragments of pyroclastic debris - consists of pumice or scoria fragments.
Loam
The effect of viscosity on eruptive style
Lapilli
Coal
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