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Test your basic knowledge |
Geology
Start Test
Study First
Subject
:
science
Instructions:
Answer 50 questions in 15 minutes.
If you are not ready to take this test, you can
study here
.
Match each statement with the correct term.
Don't refresh. All questions and answers are randomly picked and ordered every time you load a test.
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 sedimentary soil/rock; Calcite in a pedocal soil accumulates in the B-horizon and may cement soil together - creating this solid mass.
Caliche
Mantle plume
Why magma rises
Hydrolysis
2. A cut and finished stone ready to be used in jewelry. Examples - diamond - ruby - sapphire - emerald.
Divergent plate boundary
Gem
Basaltic magma
Crust
3. Sedimentary rocks consisting of carbon-rich relicts of plants.
Organic sedimentary rocks
Volatiles
Cinder cone
Sedimentary rocks
4. Sedimentary rocks made up of the shells of organisms.
Biochemical sedimentary rocks
Decompression
Felsic - intermediate - mafic - ultramafic
Asthenosphere
5. 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
Ash
Slab-pull force
Magnetic reversals
Ignimbrite
6. Magma viscosity depends upon temperature - volatile content - and silica content. Hotter magma - more volatiles - and mafic magma all have less viscosity.
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7. Forms from a chemical reaction between solid calcite and magnesium-bearing groundwater.
Dolostone
Silicates
Metals
Paleomagnetism
8. The base of the soil profile; consists of material derived from the substrate that's been chemically weathered and broken apart - but has not yet undergone leaching or accumulation.
Dipole
Glassy igneous rocks
C-horizon
Slab-pull force
9. 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.
Geothermal gradient
O-horizon
Cross beds
Specific gravity
10. 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.
Rhyolitic lava flows
Chert
Mantle
Mafic
11. Sedimentary rocks made up of minerals that precipitate directly from water solutions.
Mid-ocean ridges
Chemical sedimentary rocks
12km
Ridge-push force
12. Physical property of a mineral; represents the density of a mineral - as specified by the ratio between the weight of a volume of the mineral and the weight of an equal volume of water a 4 degrees C.
Specific gravity
Crystal lattice
Melting
Igneous rocks
13. Type of lava flow; a lava flow with warm - pasty surfaces wrinkling into smooth - glassy - rope-like bridges.
pahoehoe
Lava
Agrillaceous rocks
Hydration
14. Mineral crystal formation type; from directly from a vapor - occurs around volcanic vents or around geysers. At such locations - volcanic gases or steam enter the atmosphere and cool - so certain elements cannot remain in gaseous form.
Fumerolic mineralization
Hot-spot track
Paleopole
The effect of the environment on eruptive style
15. 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.
Thermal expansion
Biomineralization
Geothermal gradient
Deep-ocean trenches
16. Carbon-containing compounds that either occur in living organisms - or have characteristics that resemble the molecules within living organisms. Examples - oil - protein - plastic - fat - and rubber.
Organic chemicals
Rhyolitic lava flows
Dipole
Magnetic inclination
17. 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.
Decompression
Metamorphic foliation
Fractional crystallization
Upper mantle
18. After sand has lost its feldspar composition due to weathering over time - sediment composed entirely of quartz grains gets buried and lithified to form this type of rock.
Lapilli
Bathymetry
Magma mixing
Quartz sandstone
19. Type of soil; forms directly from underlying bedrock.
Convective flow
Mineral
Residual soil
Laccolith
20. Refers to the chemical reactions that alter or destroy minerals when rock comes in contact with water solutions or air.
Assimilation
Convective flow
Lithosphere
Chemical weathering
21. Occurs within the asthenosphere - actively drags plates along and attributes partially for the mechanism shifting the plates along the Earth's surface.
Siliceous rocks
Mantle plume
Convective flow
Redbeds
22. Molten rock that has flowed out onto Earth's surface.
Lava
Relative plate velocity
Transported soil
Dunes
23. Sphere; Surface water along with groundwater - Earth consists of 70% surface water (oceans - lakes - and streams).
Organic sedimentary rocks
Volcano
Glassy igneous rocks
Hydrosphere
24. Fracture type; smoothly curving - clamshell-shaped surfaces; typically formed in quartz.
Conchoidal fractures
Continental rift
Bathymetry
Lava
25. Relatively small - elongated ridges that form on a bed surface at right angles to the direction of the current flow of the rock.
Precipitation
Clastic
Asthenosphere
Ripples
26. Physical property of a mineral; refers to the way a mineral surface scatters light. Metallic versus non-metallic in nature.
Volatiles
Oxidation
Divergent plate boundary
Luster
27. 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.
Earth's atmosphere
Hydrosphere
Metamorphic foliation
Physical weathering
28. 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
Bedrock
Dolostone
Silicates
29. The combination of processes that separate rock or regolith from its substrate and carry it away. Involves abrasion - plucking - scouring - and dissolution - and is caused by air - water or ice.
Dunes
Lithification
Dipole
Erosion
30. 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.
Crust
Lithosphere
Saprolite
Clastic
31. The fit of the continents - locations of past glaciations - the distribution of equatorial climatic belts - the distribution of fossils - and matching geologic units.
Organic chemicals
Lithosphere
a'a'
Continental drift evidence
32. A reference to the sinking of the lithosphere; allows for sediment to accumulate in regions where this occurs.
Assimilation
Subsidence
Redbeds
Hardness
33. 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
Dunes
Slab-pull force
Sedimentary rocks
34. 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
Metamorphic rocks
Zone of leaching
Five steps of clastic sedimentary rock formation
35. The shape of the sea floor surface. Investigation of the sea-floor revealed the presence of several important features: mid-ocean ridges - deep-ocean trenches - seamount chains - and fracture zones.
Deposition
Streak
Bathymetry
Fracture and cleavage
36. Active hot-spot volcanoes commonly occur at the end of a chain of dead volcanoes.
Compaction
Calderas
Thermal expansion
Hot-spot track
37. 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
Stratagraphic formation
Paleopole
Ridge-push force
Cinder cone
38. 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
The effect of viscosity on eruptive style
Hydrosphere
Explosive eruptions
Flood basalts
39. Coarse pyroclastic debris - apple to refrigerator-sized fragments. Chunks of preexisting igneous rock or large lava blobs which discharge from volcanic eruptions.
Volcanic blocks/bombs
Transition zone
Stoping
Area of igneous activity
40. Sedimentary rock composed of quartz.
Magnetic inclination
rifting
Lapilli
Siliceous rocks
41. 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
Sedimentary rocks
Color
Biomineralization
Magnetic reversals
42. A mineral's growth that is uninhibited - has well-formed crystal faces.
Convective flow
Turbidity current
Euhedral crystal
Conchoidal fractures
43. Two different minerals which have the same composition but have different crystal structures.
Polymorphs
B-horizon
Transform plate boundary
Hot-spot track
44. The distance of the deepest well ever drilled - hole in northern Russia. Penetrates only about 0.03% of the Earth.
Paleomagnetism
Specific gravity
12km
Sulfates
45. Mineral class; consist of pure masses of a single metal - with metallic bonds. Copper and gold can appear in this way.
Superplumes
Area of igneous activity
Native metals
Crystalline
46. On a gem are the ground and polished surfaces made with a certain type of machine.
Pyroclastic flows
Andesitic lava flows
Facets
Special properties of minerals
47. A process occurring when sea level falls - the coast migrates seaward.
Slab-pull force
Carbonates
Regression
Intermediate
48. Rigid outer layer of Earth - 100-150km thick. Consists of the crust plus the uppermost part of the mantle.
Lithosphere
Extrusive igneous rock
The core
triple junction
49. The resistance to flow of magma. Reflects its distinct silica content - for silica tends to polymerize - meaning it links up to form long - chainlike molecules whose presence slows down the flowing ability of magma. Thus felsic magmas flow less easil
Decompression
Viscosity
Fractional crystallization
Ash
50. A mafic rock with large grains. Intrusive - phaneritic igneous rock.
650-1100 degrees C
ravertine
Igneous rocks
Gabbro