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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.
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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. Volcanic landform; pipes are short conduits that connect a magma chamber to the surface.
Volcano
Paleopole
12km
Volcanic pipes/necks
2. A mafic rock with large grains. Intrusive - phaneritic igneous rock.
Gabbro
Bed
Graded bed
Mantle plume
3. 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.
Convergent plate boundary
Symmetry
Viscosity
Granitic composition
4. Mineral crystal formation type; form at interfaces between the physical and biological components of the Earth system by this process.
Silicates
Lithosphere
Biomineralization
3.5km (2 miles)
5. The fit of the continents - locations of past glaciations - the distribution of equatorial climatic belts - the distribution of fossils - and matching geologic units.
Relative plate velocity
Stratagraphic formation
Mid-ocean ridges
Continental drift evidence
6. Volcanic landform; bulbous mass of congealed lava - associated with explosive eruptions of gas-rich magma.
Lava domes
Composite cone (stratovolcano)
Paleopole
Ridge-push force
7. 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.
Volcanic blocks/bombs
Paleopole
Oxides
Explosive eruptions
8. Forms from a chemical reaction between solid calcite and magnesium-bearing groundwater.
Cross beds
Dolostone
The effect of the environment on eruptive style
Igneous rocks
9. Mineral class; the molecule CO23 serves as the anionic group. Elements like calcium or magnesium bond to this group. Examples - calcite and dolomite.
Hydration
Carbonates
Seamount chains
Siliceous rocks
10. A process occurring when the sea level rises - the coast migrates inland. Through this - an extensive layer of beach forms.
Zone of accumulation
Conglomerate
Transgression
Mantle
11. A mineral's growth that is uninhibited - has well-formed crystal faces.
Oxides
Sandstone
Why magma rises
Euhedral crystal
12. Molten rock beneath Earth's surface.
Chemical weathering
Felsic
Magma
Basaltic composition
13. 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
Melting
Arkose
Fissure eruptions/lava plateaus
14. 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
Rocks
Granitic composition
Crystal habit
Elemental composition of Earth
15. 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
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16. The injection of magma within the magma chamber and conduit generates an outward pressure within the volcano. The presence of gas within the magma increases this pressure - as gas expands greatly as it rises toward the Earth's surface. Rhyolitic and
The effect of gas pressure on eruptive style
Arkose
Diagenesis
Soil erosion
17. Rock made by the freezing of magma underground - after it has pushed its way (intruded) into preexisting rock of the crust.
Sedimentary structure
Dark Silicates
Intrusive igneous rock
Composite cone (stratovolcano)
18. Sedimentary rocks made up of the shells of organisms.
Siltstone and mudstone
12km
Biochemical sedimentary rocks
Lapilli
19. Form from grains that break off preexisting rock and become cemented together - or from minerals that precipitate out of a water solution.
Deposition
Sedimentary rocks
650-1100 degrees C
Magnetic reversals
20. Rigid outer layer of Earth - 100-150km thick. Consists of the crust plus the uppermost part of the mantle.
Evaporites
Lithosphere
Source rock composition
Bed
21. A mafic rock with small grains. Extrusive - aphanitic igneous rock.
Turbidity current
Metals
Basalt
Earth's atmosphere
22. 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.
collision
Transform plate boundary
Ripples
Dipole
23. 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.
Cinder cone
Transition zone
Limestone
Granitic magma
24. The difference between the expected strength of the Earth's main field at a certain location and the actual measure strength of the magnetic field at that location. Places where the field strength is stronger that expected are positive anomalies - an
Silicates
Depositional environment
Mid-ocean ridges
Magnetic anomaly
25. Chemical weathering occurring in warm - wet climates can produce a layer of rotten rock - over 100km thick.
Gabbro
Continental shelf
Lava
Saprolite
26. Process where new divergent boundaries form when a continent splits and separates into two continents.
rifting
Depositional environment
Rhyolitic lava flows
Effusive eruptions
27. Equant - meaning that they have the same dimensions in all directions. Or inequant - meaning their dimensions are not the same in all directions.
Grain sizes
Lava tube
Bed
Source rock composition
28. Aggregates of mineral crystals or grains - and masses of natural glass; a coherent - naturally occurring solid - consisting of an aggregate of minerals or a mass of glass.
Deposition
Silicate minerals
Strata
Rocks
29. Sedimentary rock composed of quartz.
Rock-forming silicate minerals
Effusive eruptions
Grain sizes
Siliceous rocks
30. A single layer of sediment or sedimentary rock with a recognizable top and bottom.
Bed
Cinder cone
Mineral crystal destruction
Arkose
31. An insulated - tunnel-like conduit through which lava moves within a flow.
Intrusive igneous rock
Lapilli
Factors classifying clastic sedimentary rocks
Lava tube
32. 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.
Transported soil
Source rock composition
Explosive eruptions
Extrusive igneous rock
33. A single - continuous (uninterrupted) piece of a crystalline solid bounded by flat surfaces called crystal faces that grew naturally as the mineral formed. Come in a variety of shapes - cubes - trapezoids - pyramids - octahedrons - hexagonal columns
Soil erosion
Crystal
Asthenosphere
Fragmental igneous rocks
34. Rocks which develop when hot molten rock cools and freezes solid.
Ridge-push force
Igneous rocks
Paleomagnetism
a'a'
35. Form when solid materials become hot and transform into liquid - example - molten rock.
Shield volcano
atmospheres (atm)
Melts
Rocks
36. 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.
Arkose
Extrusive igneous rock
Cinder cone
collision
37. Actively slipping segment of a fracture zone between two ocean ridge segments - these faults make a third type of plate boundary - transforms.
Erosion
Transform fault
Silicate minerals
The effect of the environment on eruptive style
38. A fine spray of lava instantly freezes to form fine particles of glass.
Bedding
Columnar jointing
Ash
Caliche
39. In addition to islands that rise above sea level - seamounts have been detected (isolated submarine mountains) - once volcanoes but no longer erupt.
Loam
Dissolution
Seamount chains
Lava domes
40. The process by which sediment settles out of the transporting medium.
Crystal lattice
Deposition
Alloy
Bed
41. Tree roots that grow into joints can push those joints open in this process.
Sill
Root wedging
Large Igneous Provinces (LIPs)
Polymorphs
42. 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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43. Type of lava flow; higher silica content - greater viscosity - forms a large mound above the vent out of a volcano.
Soil Horizons
Native metals
Carbonate rocks
Andesitic lava flows
44. Mineral class; the anion within these types of minerals is a halogen ion (such as chlorine or fluorine).
Dissolution
Halides
Transform plate boundary
Metamorphic foliation
45. Sphere; Surface water along with groundwater - Earth consists of 70% surface water (oceans - lakes - and streams).
Deposition
Bedrock
Hydrosphere
Geothermal gradient
46. 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.
Conglomerate
Andesitic lava flows
Organic chemicals
Stratagraphic formation
47. 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
Fracture zones
Laccolith
Regression
48. Type of volcanic eruption; takes place when water gains access to the hot rock around the magma chamber and suddenly transforms into steam - a pyroclastic eruption involving the reaction of water with magma.
Transgression
Biomineralization
Sedimentary Basins
Phreatomagmatic eruptions
49. 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
Plates
Five steps of clastic sedimentary rock formation
Siltstone and mudstone
50. The most important mineral group; comprise the most rock-forming minerals - they are very abundant due to large % of silicon and oxygen in Earth's crust. Examples - oxygen - silica - aluminum.
Felsic - intermediate - mafic - ultramafic
Agrillaceous rocks
Rock-forming silicate minerals
Pangaea
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