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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. Fluid basaltic lava extruded from crustal fractures called fissures.
Laccolith
Explosive eruptions
Fissure eruptions/lava plateaus
Magnetic reversals
2. 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.
Fracture and cleavage
Frost wedging
Fractional crystallization
Factors of magma cooling time
3. A mafic rock with small grains. Extrusive - aphanitic igneous rock.
Dolostone
Dunes
Felsic
Basalt
4. Mineral crystal formation type; form from a solution - meaning that atoms - molecules - or ions dissolved in water bond together out of water.
Precipitation
Symmetry
Dissolution
Luster
5. A mineral's growth that is uninhibited - has well-formed crystal faces.
Ridge-push force
Specific gravity
Chert
Euhedral crystal
6. The supercontinent; existence proposed by Wegener - suggested that the supercontinent later fragmented into separate continents that then drifted apart - moving slowly to their present positions.
Fracture zones
Pangaea
Streak
pahoehoe
7. Layer that lies below the lithosphere - and is the portion of the mantle in which rock can flow (slowly; 10-15cm per year) despite still being solid. Entirely within the mantle and lies below a depth of 100-150km.
Weathering
Asthenosphere
Transform plate boundary
Siliceous rocks
8. 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.
Gabbro
Jointing
Factors of magma cooling time
Solid-state diffusion
9. A reference to the pattern structure of a mineral. A material in which atoms are fixed in an orderly pattern - a crystalline solid.
Redbeds
Weathering
Hot-spot track
Crystal lattice
10. Process where new divergent boundaries form when a continent splits and separates into two continents.
Five steps of clastic sedimentary rock formation
Rock layering
rifting
Xenolith
11. Magma type; contains about 45% to 52% silica. Named because it produces rock containing abundant mafic minerals - magnesium and iron combinations.
Laterite
Mafic
Streak
Erosion
12. 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.
The effect of viscosity on eruptive style
triple junction
Soil Horizons
Seamount chains
13. 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.
Basaltic composition
Streak
Volcanic pipes/necks
Reason for Earth's internal heat
14. 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.
Seamount chains
Alloy
Cinder cone
Silicates
15. 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
Plate tectonics
Deep-ocean trenches
Sill
Agrillaceous rocks
16. 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.
Basaltic lava flows
Rock layering
Glassy igneous rocks
Organic sedimentary rocks
17. During this process - water chemically reacts with minerals and breaks them down - working faster in slightly acidic water.
Oxides
Transition zone
Five steps of clastic sedimentary rock formation
Hydrolysis
18. Volcanic landform; pipes are short conduits that connect a magma chamber to the surface.
Mantle plume
Volcanic pipes/necks
Lithification
Siltstone and mudstone
19. The transformation of loose sediment into solid rock.
Lithification
Metals
Turbidite
Zone of accumulation
20. The freely pivoting up and down compass needle's angle of tilt relative to the location upon the Earth's surface. At the equator - the specialized magnetic needle would position horizontally and at a magnetic pole it would point straight down.
Sedimentary Basins
Magnetic inclination
Glass
Fissure eruptions/lava plateaus
21. Form from grains that break off preexisting rock and become cemented together - or from minerals that precipitate out of a water solution.
Continental shelf
Sedimentary rocks
Clastic sedimentary rocks
E-horizon
22. Blocks of rock that are solid and durable but composed of rough quartz sand grains cemented together.
Sandstone
Hydrolysis
Salt wedging
Lava
23. The burial and lithification of angular or rounded clasts form these types of rocks.
Spreading rate
collision
Granite
Conglomerate
24. Farther down from a zone of leaching - new mineral crystals precipitate directly out of the water or form when the water reacts with debris - this the region where the new minerals and clay collect.
Laterite
Magma's speed of flow
Zone of accumulation
Biochemical sedimentary rocks
25. Type of sedimentary rock; rocks whose grains are stuck together by cement.
Clastic
Calderas
Thermal expansion
3.5km (2 miles)
26. The boundary between two beds is a bedding plane; several beds constitute this structure.
Oxidation
Strata
Heat transfer
Alloy
27. Sedimentary rocks made up of the shells of organisms.
Earth's atmosphere
Hot-spot track
Biochemical sedimentary rocks
Residual soil
28. A reference to the sinking of the lithosphere; allows for sediment to accumulate in regions where this occurs.
Lava tube
Subsidence
a'a'
Grain sizes
29. A submarine suspension of sediment.
Turbidity current
Silicate minerals
Paleomagnetism
12km
30. 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
collision
Plate tectonics
Pangaea
Asthenosphere
31. Magma type; contains about 52% to 66% silica. Name indicates that these magmas have a composition between that of felsic and mafic magma.
Calderas
Outcrop
Intermediate
Inner core
32. Iron (35%) - oxygen (30%) - silicon (15%) - and magnesium (10%) - and the remaining 10% consists of 88 naturally occurring elements.
Elemental composition of Earth
Glass
Partial melting
Bedrock
33. Tree roots that grow into joints can push those joints open in this process.
Deep-ocean trenches
Root wedging
Continental drift hypothesis
Grain sizes
34. 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.
Geothermal gradient
Rhyolitic lava flows
Crust
Grain sizes
35. A mafic rock with large grains. Intrusive - phaneritic igneous rock.
Melting
Gabbro
Phreatomagmatic eruptions
Outer core
36. 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
Agrillaceous rocks
Residual soil
Basaltic lava flows
Felsic - intermediate - mafic - ultramafic
37. Sublayer of the mantle - depth of 660km.
Geothermal gradient
Crystal
Upper mantle
A-horizon
38. 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.
Grain sizes
Conchoidal fractures
Batholiths
Streak
39. Weathering - erosion - transportation - deposition - and lithification.
Five steps of clastic sedimentary rock formation
Biomineralization
Inner core
Igneous rocks
40. 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
Bed
Depositional environment
The effect of viscosity on eruptive style
Factors of magma cooling time
41. Type of sedimentary soil/rock; Calcite in a pedocal soil accumulates in the B-horizon and may cement soil together - creating this solid mass.
Calderas
Source rock composition
Sedimentary rocks
Caliche
42. The distance that the world's deepest mine-shaft penetrates into the Earth beneath South Africa.
Ash
Rock composition
3.5km (2 miles)
Erosion
43. Contributes to formation of soil; occurs when rainwater percolates through the debris and carries dissolved ions and clay flakes downward - This is the region where the downward transport occurs.
Zone of leaching
Felsic
Intrusive igneous rock
Plutons
44. 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.
Stratagraphic formation
Igneous rocks
Crystal
Strata
45. 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.
Soil
Sulfates
Laterite
Factors classifying clastic sedimentary rocks
46. Lava flow; associated with felsic magma - consists of ash and pumice fragments - material is propelled from the vent at a high speed.
Organic chemicals
Pyroclastic flows
Plate tectonics
Flood basalts
47. 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).
Hydrolysis
Mantle plume
Deposition
Cementation
48. A type of carbonate rock; rocks formed from the calcite or aragonite skeletons of organisms form this biochemical sedimentary rock.
Hot-spot track
Volatiles
Earth's atmosphere
Limestone
49. A process occurring when the sea level rises - the coast migrates inland. Through this - an extensive layer of beach forms.
Fractional crystallization
Glass
Ripples
Transgression
50. 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.
Convective flow
Clastic
Loam
B-horizon