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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. The absorption of water into the crystal structure of minerals - causes some minerals to expand.
Crystalline
Hydration
Geothermal gradient
Lava domes
2. 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.
Sulfides
Symmetry
Soil
Fumerolic mineralization
3. Type of lava flow; surface layer of the lava freezes and then breaks up due to the continued movement of lava underneath - becomes a jumble of sharp - angular fragments - yielding a rubbly flow.
4. Rocks whose crystals interlock with each other.
Outer core
Crystalline
Precipitation
Strata
5. Magma type; contains about 52% to 66% silica. Name indicates that these magmas have a composition between that of felsic and mafic magma.
Inner core
Halides
Area of igneous activity
Intermediate
6. A linear belt in which continental lithosphere pulls apart - the lithosphere stretches horizontally.
Magma's speed of flow
Ridge-push force
Chert
Continental rift
7. A fine spray of lava instantly freezes to form fine particles of glass.
Intrusive igneous rock
ravertine
Polymorphs
Ash
8. A reference to the supposed position of the Earth's magnetic pole at a time in the past.
Weathering
Plate tectonics
Paleopole
Clastic sedimentary rocks
9. The Earth radiated heat into space and slowly cooled. Eventually - the early formed sea of lava solidified and formed igneous rock. The cumulative effect of radioactivity has been sufficient to slow the cooling of the planet and subsequently allow fo
10. 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.
Seamount chains
Pyroclastic debris
Depositional environment
Volatiles
11. Lava flow; associated with felsic magma - consists of ash and pumice fragments - material is propelled from the vent at a high speed.
Magnetic declination
Deposition
Pyroclastic flows
Root wedging
12. Mineral crystal formation type; form from a solidification of a melt - meaning the freezing of a liquid.
Melting
Crystal lattice
Volcano
Pangaea
13. Magma type; contains about 66% to 76% silica. Name reflects the occurrence of feldspar and quartz in rocks formed in this magma.
Erosion
Zone of accumulation
Felsic
Hardness
14. Blocks of rock that are solid and durable but composed of rough quartz sand grains cemented together.
Transform fault
Silicate minerals
Transgression
Sandstone
15. 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.
Carbonates
Magma's speed of flow
Physical weathering
Effusive eruptions
16. Rocks that forms by the freezing of lava above ground - after it spills out (extrudes) onto the surface of the Earth and comes into contact with the atmosphere or ocean.
Symmetry
The core
Extrusive igneous rock
Tuff
17. 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.
Transgression
Deep-ocean trenches
Siltstone and mudstone
Crust
18. Rigid outer layer of Earth - 100-150km thick. Consists of the crust plus the uppermost part of the mantle.
Lithosphere
12km
Partial melting
rifting
19. A naturally occurring solid - formed by geologic processes - has a crystalline structure and a definable chemical composition - and is generally inorganic.
Pyroclastic debris
Mineral
Siltstone and mudstone
Lava tube
20. Mineral crystal formation type; form from a solution - meaning that atoms - molecules - or ions dissolved in water bond together out of water.
Precipitation
Ultramafic
Sedimentary Basins
Earth's atmosphere
21. Mineral class; consist of pure masses of a single metal - with metallic bonds. Copper and gold can appear in this way.
Organic chemicals
Native metals
Paleopole
Evaporites
22. Type of soil; forms directly from underlying bedrock.
Sulfates
Residual soil
Crust
Felsic - intermediate - mafic - ultramafic
23. Rock made by the freezing of magma underground - after it has pushed its way (intruded) into preexisting rock of the crust.
3.5km (2 miles)
Tuff
Intrusive igneous rock
Granitic magma
24. 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
Decompression
Streak
Regression
triple junction
25. A plate boundary at which one plate slips along the side of another plate. No new plate is formed and no old plate is consumed. But the grinding between the plates generates frequent and destructive earthquakes.
Transform plate boundary
Granitic magma
Metals
Carbonate rocks
26. 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
Paleopole
Convergent plate boundary
Siltstone and mudstone
Silicates
27. 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.
Felsic - intermediate - mafic - ultramafic
Gabbro
Zone of leaching
Rock texture
28. The crust moves away from the Mid-Atlantic Ridge axis at a rate of 1cm per year. This velocity of sea-floor spreading is determined by the relationship between the paleomagnetic anomaly-stripe's width and the reverse polarity duration - the data reve
Sulfides
Spreading rate
Transform fault
Solid-state diffusion
29. Type of sedimentary rock; rocks whose grains are stuck together by cement.
Clastic
12km
Superplumes
Crust
30. Chemical weathering during Which minerals dissolve into water.
Hot spots
Chemical sedimentary rocks
collision
Dissolution
31. 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.
Assimilation
Loam
Mantle
Granitic composition
32. The rate of increase in temperature - decreases with increasing depth. The dashed lines represent the solidus and liquidus for mantle rock (peridotite). The solidus line defines the conditions of pressure and temperature at Which mantle rock begins t
Biochemical sedimentary rocks
Seamount chains
Magma
Geothermal gradient
33. 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
Hot spots
collision
Rhyolitic lava flows
Explosive eruptions
34. Equant - meaning that they have the same dimensions in all directions. Or inequant - meaning their dimensions are not the same in all directions.
Conglomerate
Grain sizes
Clastic
Area of igneous activity
35. A type of carbonate rock; rocks formed from the calcite or aragonite skeletons of organisms form this biochemical sedimentary rock.
Continental rift
Deep-ocean trenches
Factors of magma cooling time
Limestone
36. 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
Five steps of clastic sedimentary rock formation
Diagenesis
Laterite
37. A felsic rock with large grains. Intrusive - phaneritic igneous rock.
Seamount chains
Bedding
Granite
Luster
38. The conditions in which sediment was deposited. Examples - beach - glacial - and/or river environments.
Depositional environment
Felsic
Abyssal plains
triple junction
39. On a gem are the ground and polished surfaces made with a certain type of machine.
Large Igneous Provinces (LIPs)
Lithification
Sedimentary rocks
Facets
40. 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.
Fumerolic mineralization
Stratagraphic formation
Crystalline igneous rocks
Five steps of clastic sedimentary rock formation
41. A reaction during which an element loses electrons - commonly takes place when elements combine with oxygen.
Oxidation
Rock texture
Melts
Basaltic lava flows
42. Irregular or blob-shaped intrusions that range in size from tens of meters across to tens of kilometers across.
Clastic sedimentary rocks
3.5km (2 miles)
Plutons
Viscosity
43. The record of paleomagnetism revealed that the location of Earth's magnetic poles had been changing through geologic time. This 'wandering' meant that Earth's magnetic poles do not move with respect to fixed continents. Rather - continents move relat
Flood basalts
Partial melting
Volatiles
Apparent polar-wander path
44. The most common minerals in the Earth. Contain silica (SiO2) mixed in varying proportions with other elements (typically iron - magnesium - aluminum - calcium - potassium - and sodium).
Weathering
Igneous rocks
Silicate minerals
Volcano
45. The process by which sediment settles out of the transporting medium.
Melting
Felsic
Deposition
atmospheres (atm)
46. Places with particularly voluminous quantities of magma erupting or intruding.
Large Igneous Provinces (LIPs)
Rock texture
Intrusive igneous rock
Sedimentary structure
47. Subsoil - ions and clay leached and transported down from above accumulate here. As a result - new minerals form - and clay fills open spaces. Part of the zone of accumulation.
B-horizon
Seamount chains
Evaporites
Convective flow
48. Soil section below the O-horizon - humus has decayed further and has mixed with mineral grains (clay - silt - and sand). Water percolating through this horizon causes chemical weathering reactions to occur and produces ions in solution and new clay m
Relative plate velocity
Cementation
A-horizon
Spreading rate
49. Volcanic landform; bulbous mass of congealed lava - associated with explosive eruptions of gas-rich magma.
Lava domes
Soil
Stoping
Silicate minerals
50. Actively slipping segment of a fracture zone between two ocean ridge segments - these faults make a third type of plate boundary - transforms.
Continental drift evidence
Transform fault
Five steps of clastic sedimentary rock formation
Convective flow