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Test your basic knowledge |
Geology
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Study First
Subject
:
science
Instructions:
Answer 50 questions in 15 minutes.
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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. 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
Organic sedimentary rocks
Pangaea
Convergent plate boundary
Clastic sedimentary rocks
2. A proposition in 1960 - by Princeton University professor Harry Hess - that continents drift apart because new ocean floor forms between them by this process.
Sea-floor spreading
Rock layering
Dark Silicates
Strata
3. Type of soil; forms directly from underlying bedrock.
Five steps of clastic sedimentary rock formation
Effusive eruptions
Residual soil
a'a'
4. Sphere; Surface water along with groundwater - Earth consists of 70% surface water (oceans - lakes - and streams).
Dark Silicates
Fumerolic mineralization
Hydrosphere
Mafic
5. An insulated - tunnel-like conduit through which lava moves within a flow.
Dolostone
Volcanic pipes/necks
Ridge-push force
Lava tube
6. Rocks which develop when hot molten rock cools and freezes solid.
Biochemical sedimentary rocks
Light silicates
Hydration
Igneous rocks
7. 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
Partial melting
Superplumes
Phreatomagmatic eruptions
8. The conditions in which sediment was deposited. Examples - beach - glacial - and/or river environments.
Continental shelf
Depositional environment
Basalt
Hot-spot track
9. A reaction during which an element loses electrons - commonly takes place when elements combine with oxygen.
Regression
Oxidation
Crystal structure
Stratagraphic formation
10. Active hot-spot volcanoes commonly occur at the end of a chain of dead volcanoes.
Fragmental igneous rocks
Silicate minerals
Superplumes
Hot-spot track
11. Perhaps the cause for the large igneous provinces; formations within the mantle - plumes that bring up vastly more hot asthenosphere than normal plumes.
Superplumes
The core
Symmetry
Chemical weathering
12. 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).
Seamount chains
Silicate minerals
Dike
Fracture and cleavage
13. The layering nature of sedimentary rocks - surface features of layers formed during deposition - and the arrangement of grains within layers.
Specific gravity
Oxidation
Sedimentary structure
Volcano
14. 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.
Lower mantle
Agrillaceous rocks
Compaction
Clastic
15. 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.
Glassy igneous rocks
Zone of leaching
Physical weathering
Solid-state diffusion
16. Blocks of rock that are solid and durable but composed of rough quartz sand grains cemented together.
Hydrosphere
Turbidite
Light silicates
Sandstone
17. 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.
Decompression
Explosive eruptions
Gem
Paleopole
18. Cause of melting; magma can also form at locations where chemicals called volatiles mix with hot mantle rock. Elements such as water and carbon dioxide mix with hot rock - helping to break chemical bonds - so that if you add volatiles to a solid - ho
Pyroclastic flows
Mineral
Volatiles
Special properties of minerals
19. The speed of the movements of the plates with respect to the speed of the other plates' movements. Absolute plate velocity is a measure of the movement of any plates relative to a fixed point in the mantle.
Metals
Intermediate
Relative plate velocity
Biochemical sedimentary rocks
20. A thick accumulation of sediment (10-15km) - the surface of this sediment layer is this broad - shallow region.
Spreading rate
Decompression
Continental shelf
Viscosity
21. Pea to plum-sized fragments of pyroclastic debris - consists of pumice or scoria fragments.
Lapilli
Differential weathering
Crystalline igneous rocks
Sedimentary structure
22. A mafic rock with small grains. Extrusive - aphanitic igneous rock.
The effect of the environment on eruptive style
Conchoidal fractures
Conglomerate
Basalt
23. In addition to islands that rise above sea level - seamounts have been detected (isolated submarine mountains) - once volcanoes but no longer erupt.
Stoping
Silicates
Seamount chains
Crystalline
24. A felsic rock with large grains. Intrusive - phaneritic igneous rock.
Soil Horizons
Thermal expansion
Euhedral crystal
Granite
25. 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.
pahoehoe
Luster
Symmetry
Hydration
26. Type of soil; forms in tropical regions where abundant rainfall drenches the land during the rainy season - and the soil dries during the dry season.
Ridge-push force
Bedding
Laterite
12km
27. 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.
Carbonate rocks
Laterite
Shield volcano
C-horizon
28. Sedimentary rock composed of quartz.
Siliceous rocks
Fracture and cleavage
Seamount chains
Flood basalts
29. The distance that the world's deepest mine-shaft penetrates into the Earth beneath South Africa.
Felsic
3.5km (2 miles)
pahoehoe
Basaltic composition
30. Molten rock beneath Earth's surface.
Precipitation
Magma
Oxides
Cementation
31. The compiled data from many marine cruises which defined a distinctive - striped and alternating bands of paleomagnetism.
Root wedging
Subduction
Marine magnetic anomaly
Tephra
32. A mafic rock with large grains. Intrusive - phaneritic igneous rock.
Phreatomagmatic eruptions
Laccolith
Gabbro
Cross beds
33. Physical property of a mineral; refers to the way a mineral surface scatters light. Metallic versus non-metallic in nature.
650-1100 degrees C
Luster
Fracture and cleavage
Laccolith
34. 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
Asthenosphere
triple junction
Light silicates
35. Type of volcanic eruption; produce mainly lava flows - yield low-viscosity basaltic lavas.
Effusive eruptions
Lava
Euhedral crystal
Apparent polar-wander path
36. The boundary between two beds is a bedding plane; several beds constitute this structure.
collision
Strata
O-horizon
Fracture zones
37. 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.
Siltstone and mudstone
Partial melting
Paleomagnetism
Crystal lattice
38. A linear belt in which continental lithosphere pulls apart - the lithosphere stretches horizontally.
Source rock composition
Bedding
Continental rift
Transported soil
39. 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.
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40. Soil section below the A-horizon; a soil level that has undergone substantial leaching but has not yet mixed with organic material. Because it lacks organic materials - this horizon tends to be lighter than the A-horizon. Part of the zone of leaching
Mineral
Magma's speed of flow
Bedrock
E-horizon
41. During the final stages of cooling - lava flows contract and may fracture into roughly hexagonal columns.
Fragmental igneous rocks
Native metals
a'a'
Columnar jointing
42. 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).
Cementation
Biochemical sedimentary rocks
Sandstone
Large Igneous Provinces (LIPs)
43. Core division; between 2900 and 5155km deep. Liquid iron alloy - it exists as a liquid because the temperature here is so high that even the great pressures squeezing the region cannot lock atoms into a solid framework. This liquid iron alloy is able
Outer core
Mineral crystal destruction
Streak
Magma's speed of flow
44. In degrees Celsius - the high temperatures at which igneous rocks freeze; the freezing of liquid melt to form solid igneous rock represents the same phenomenon as the freezing of water - except at much higher temperatures.
Flood basalts
650-1100 degrees C
Arkose
Quartz sandstone
45. 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
Magnetic anomaly
Precipitation
Lava
46. Inorganic limestone; rock composed of crystalline calcium carbonate formed by chemical precipitation.
ravertine
12km
Explosive eruptions
Hydrolysis
47. A sheet of tuff formed from a pyroclastic flow.
Strata
Composite cone (stratovolcano)
Ignimbrite
Basalt
48. Four settings: in volcanic arcs bordering deep-ocean trenches - isolated hot spots - within continental rifts - and along mid-ocean ridges.
Quartz sandstone
Area of igneous activity
Loam
Intrusive igneous rock
49. Mineral crystal formation type; form from a solidification of a melt - meaning the freezing of a liquid.
Melting
Hot spots
Ignimbrite
Columnar jointing
50. 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.
Hydrolysis
Mafic
Sedimentary Basins
Deep-ocean trenches
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