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Test your basic knowledge |
Geology
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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. A reference to the supposed position of the Earth's magnetic pole at a time in the past.
Zone of leaching
Agrillaceous rocks
Paleopole
Rhyolitic lava flows
2. Rock formations still attached to the Earth's crust.
Clastic sedimentary rocks
pahoehoe
Plates
Bedrock
3. Mineral class; consist of a metal cation bonded to a sulfide anion. Examples - galena and pyrite. Many have a metallic luster. Can also be considered ores with high proportions of metal within the mineral.
Sulfides
Hardness
Turbidity current
Outer core
4. 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.
Bedding
Andesitic lava flows
Compaction
Frost wedging
5. Rocks with a fragmental texture consist of igneous fragments that are packed together - welded together - or cemented together after having solidified. Examples - pyroclastic rocks such as tuff or breccia.
Fragmental igneous rocks
Ultramafic
Color
Bathymetry
6. 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.
Phreatomagmatic eruptions
Soil
Dolostone
Metamorphic foliation
7. Mineral group; feldspars - quartz - muscovite - clay minerals.
The effect of viscosity on eruptive style
Light silicates
Rock texture
Transform fault
8. Physical property of a mineral; refers to the color of a powder produced by pulverizing the mineral. Provides a fairly reliable clue to the mineral's identity - since the color of the mineral powder tends to be less variable than the color of the who
Streak
Zone of leaching
Topography
Turbidite
9. Chemical precipitates; salt deposits formed as a consequence of evaporation. Examples - rock salt and gypsum.
Soil erosion
Gabbro
Evaporites
Metals
10. 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
Dissolution
Lava
Fracture and cleavage
C-horizon
11. The compiled data from many marine cruises which defined a distinctive - striped and alternating bands of paleomagnetism.
Inner core
Mantle
Marine magnetic anomaly
Crystal habit
12. Type of lava flow; the most viscous of any lava flow because it is the most silicic and the coolest in nature. Tends to accumulate in a lava dome above the vent or in short and bulbous flows 1 to 2 km long.
Mineral
Root wedging
Rhyolitic lava flows
Upper mantle
13. The broad - relatively flat regions of the ocean that lie at a depth of about 4-5km below sea level.
Lapilli
Euhedral crystal
Abyssal plains
C-horizon
14. A mafic rock with small grains. Extrusive - aphanitic igneous rock.
Lava
Basalt
Organic sedimentary rocks
The core
15. Sedimentary rock composed of quartz.
Siliceous rocks
Rock-forming silicate minerals
pahoehoe
Ignimbrite
16. Iron (35%) - oxygen (30%) - silicon (15%) - and magnesium (10%) - and the remaining 10% consists of 88 naturally occurring elements.
Bedrock
Depositional environment
Elemental composition of Earth
Salt wedging
17. The way in which the atoms are packed together within a mineral by chemical bonds. Five difference types of bonding can occur - covalent - ionic - metallic - Van der Waal's - and hydrogen.
Weathering
Siltstone and mudstone
Subduction
Crystal structure
18. An organic sedimentary rock; black - combustible rock consisting of over 50% carbon.
Asthenosphere
Coal
Halides
Felsic
19. 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
Granitic magma
Plate tectonics
Area of igneous activity
Strata
20. Mineral crystal formation type; form at interfaces between the physical and biological components of the Earth system by this process.
Basaltic composition
Bedding
Ultramafic
Biomineralization
21. 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.
Shield volcano
Fracture zones
Specific gravity
Geothermal gradient
22. Sedimentary rocks made up of the shells of organisms.
Deep-ocean trenches
ravertine
Biochemical sedimentary rocks
Tuff
23. Volcanic landform; steep walled depression at the summit - size exceeds one kilometer in diameter.
Grain sizes
collision
A-horizon
Calderas
24. An intrusion starting to inject between layers but then dome upwards - creating this blister-shaped intrusion.
Reason for Earth's internal heat
Melts
Laccolith
Intermediate
25. An insulated - tunnel-like conduit through which lava moves within a flow.
Dissolution
Weathering
Lava tube
Hot-spot track
26. Alfred Wegener's suggestion that the positions of the continents change through time as they drift away from each other. The flaw was that he lacked a plausible moving mechanism.
Subsidence
Transition zone
Continental drift hypothesis
Mantle plume
27. Physical property of a mineral; results from the way a mineral interacts with light. A mineral absorbs certain wavelengths - so the color seen represents the color wavelengths the mineral did not absorb.
Color
Geothermal gradient
Granite
Crystal lattice
28. 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.
Melts
Divergent plate boundary
Erosion
Gem
29. 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.
Bathymetry
Sedimentary Basins
Sedimentary structure
Frost wedging
30. The process by which sediment settles out of the transporting medium.
Flood basalts
Deposition
Facets
Strata
31. Mineral class; the anion within these types of minerals is a halogen ion (such as chlorine or fluorine).
Solid-state diffusion
Deposition
Halides
Granitic composition
32. Sedimentary rock composed of calcite or dolomite.
Rock texture
Siltstone and mudstone
Erosion
Carbonate rocks
33. 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.
Conchoidal fractures
Source rock composition
Color
pahoehoe
34. 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.
B-horizon
Fractional crystallization
Pangaea
Intrusive igneous rock
35. On a gem are the ground and polished surfaces made with a certain type of machine.
Facets
Solid-state diffusion
Arkose
Silicate minerals
36. Places where intrusive igneous rock creates tabular intrusions cutting across rock that does not have layering - this nearly vertical - wall-like tabular intrusions is formed. Cut across layering within the earth.
Subsidence
Dike
Gem
Rhyolitic lava flows
37. Rocks whose crystals interlock with each other.
Crystalline
Hydration
Continental drift evidence
Metals
38. Some rocks develop their magnetization - their ability to produce a magnetic field - at the time that the rocks themselves formed. Such rocks - preserve a record of the Earth's magnetic field at known times in the past.
Marine magnetic anomaly
Dolostone
Chemical weathering
Paleomagnetism
39. Successive turbidity currents deposit successive graded beds - creating this sequence of strata.
Zone of leaching
Turbidite
Tephra
Saprolite
40. 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.
Lava domes
Basaltic composition
Intrusive igneous rock
Sandstone
41. 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.
Hydration
Crust
Columnar jointing
Glassy igneous rocks
42. The nature of Earth's magnetic field - like the familiar magnetic field around a bar magnet - has a North and South pole. The magnetic field is drawn with field lines - the paths along Which magnets would align - or charged particles would flow - if
C-horizon
Compaction
Crystalline
Dipole
43. Weathering - erosion - transportation - deposition - and lithification.
Extrusive igneous rock
Topography
Lithosphere
Five steps of clastic sedimentary rock formation
44. Rocks that consist of mineral crystals that intergrow when the melt solidifies - interlocking structure. Examples - granite and rhyolite.
Magnetic anomaly
Fissure eruptions/lava plateaus
Crystalline igneous rocks
Dolostone
45. Similar to ripples - but are much larger. Small ripples often form on the surface of these structures.
Sulfides
Dunes
Zone of accumulation
Dark Silicates
46. A reaction during which an element loses electrons - commonly takes place when elements combine with oxygen.
Oxidation
Magma
Coal
Convective flow
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).
Ridge-push force
Paleopole
Apparent polar-wander path
Cementation
48. A mineral's growth that is uninhibited - has well-formed crystal faces.
Euhedral crystal
Silicate minerals
Conglomerate
Dunes
49. Mineral group; olivine group - pyroxene group - amphibole group.
Graded bed
Dark Silicates
Rocks
Cross beds
50. Mineral class; the molecule CO23 serves as the anionic group. Elements like calcium or magnesium bond to this group. Examples - calcite and dolomite.
Root wedging
Sill
Granitic composition
Carbonates
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