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Test your basic knowledge |
Geology
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Subject
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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. 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.
Shield volcano
Compaction
Sedimentary structure
Sandstone
2. The distance of the deepest well ever drilled - hole in northern Russia. Penetrates only about 0.03% of the Earth.
Sedimentary structure
12km
Lava
Soil
3. Magma type; contains about 45% to 52% silica. Named because it produces rock containing abundant mafic minerals - magnesium and iron combinations.
Pyroclastic debris
Pyroclastic flows
Crystalline igneous rocks
Mafic
4. Refers to the proportions of different chemicals making up the rock - and thus the proportion chemicals affects the proportions of different minerals constituting the rock.
Fracture and cleavage
The effect of the environment on eruptive style
Rock composition
Transform plate boundary
5. 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.
Bathymetry
650-1100 degrees C
Fissure eruptions/lava plateaus
Rock layering
6. 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
Rock composition
Lava tube
Organic sedimentary rocks
7. A sheet of tuff formed from a pyroclastic flow.
Special properties of minerals
Ignimbrite
Sulfates
Biomineralization
8. 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
Lava tube
Calderas
Continental drift hypothesis
Volatiles
9. Sublayer of the mantle - depth of 660km.
Erosion
Upper mantle
Thermal expansion
Siliceous rocks
10. 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
Silicates
Euhedral crystal
Superplumes
11. Forms from a chemical reaction between solid calcite and magnesium-bearing groundwater.
Zone of accumulation
Mineral
Dolostone
Halides
12. 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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13. 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
Magma's speed of flow
Quartz sandstone
Residual soil
14. After sand has lost its feldspar composition due to weathering over time - sediment composed entirely of quartz grains gets buried and lithified to form this type of rock.
Transition zone
Lava domes
Cinder cone
Quartz sandstone
15. Magma type; contains about 66% to 76% silica. Name reflects the occurrence of feldspar and quartz in rocks formed in this magma.
Felsic
ravertine
Melts
Cementation
16. Process where new divergent boundaries form when a continent splits and separates into two continents.
C-horizon
rifting
Evaporites
Organic sedimentary rocks
17. 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.
Redbeds
Color
Rock composition
Sandstone
18. 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.
Rocks
Oxides
Superplumes
Rock texture
19. Sedimentary rocks made up of minerals that precipitate directly from water solutions.
Erosion
Chemical sedimentary rocks
Basaltic lava flows
Rock layering
20. During this process - water chemically reacts with minerals and breaks them down - working faster in slightly acidic water.
Crust
Mineral
Hydrolysis
Transform plate boundary
21. The compiled data from many marine cruises which defined a distinctive - striped and alternating bands of paleomagnetism.
Evaporites
Marine magnetic anomaly
Sulfates
Deposition
22. Two different minerals which have the same composition but have different crystal structures.
Sulfides
Gem
Polymorphs
Basalt
23. Relatively small - elongated ridges that form on a bed surface at right angles to the direction of the current flow of the rock.
Ash
Crystal habit
Ripples
Mafic
24. Sedimentary rock composed of clay.
collision
Strata
Salt wedging
Agrillaceous rocks
25. 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.
Lava domes
Andesitic lava flows
Batholiths
Caliche
26. Molten rock beneath Earth's surface.
Light silicates
Upper mantle
Mineral crystal destruction
Magma
27. Magma viscosity depends upon temperature - volatile content - and silica content. Hotter magma - more volatiles - and mafic magma all have less viscosity.
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28. A column of very hot rock that flows upward until it reaches the base of the lithosphere. In this model - such deep-mantle plumes form because heat rising from the Earth's core is warming rock at the base of the mantle. A possible explanation to the
Deposition
Weathering
a'a'
Mantle plume
29. Natural bond connecting rocks; mineral material that precipitates from water and fills the space between grains.
Cement
Grain sizes
Gabbro
Silicate minerals
30. 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.
Transported soil
Rock-forming silicate minerals
Diagenesis
Apparent polar-wander path
31. Mineral class; the molecule CO23 serves as the anionic group. Elements like calcium or magnesium bond to this group. Examples - calcite and dolomite.
Rocks
Carbonates
Intermediate
Igneous rocks
32. A vent at Which melt from inside the Earth spews onto the planet's surface. Erupt.
Thermal expansion
Transform fault
Euhedral crystal
Volcano
33. A linear belt in which continental lithosphere pulls apart - the lithosphere stretches horizontally.
Stratagraphic formation
Metamorphic foliation
Crystal structure
Continental rift
34. Type of soil; forms directly from underlying bedrock.
Rock layering
Residual soil
Magma mixing
ravertine
35. Materials that easily transform into gas at the relatively low temperatures found at the Earth's surface.
Volatiles
triple junction
Crystal
O-horizon
36. An exposure of bedrock.
Alloy
Sulfates
Seamount chains
Outcrop
37. A process occurring when the sea level rises - the coast migrates inland. Through this - an extensive layer of beach forms.
Silicate minerals
Sedimentary rocks
Transgression
The effect of the environment on eruptive style
38. Fluid basaltic lava extruded from crustal fractures called fissures.
Fissure eruptions/lava plateaus
Felsic - intermediate - mafic - ultramafic
Laccolith
Siltstone and mudstone
39. The boundary between two beds is a bedding plane; several beds constitute this structure.
Fracture and cleavage
Strata
Regression
Factors classifying clastic sedimentary rocks
40. Physical property of a mineral; refers to the way a mineral surface scatters light. Metallic versus non-metallic in nature.
Luster
Upper mantle
Dike
Andesitic lava flows
41. 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.
Asthenosphere
Factors of magma cooling time
Euhedral crystal
Convective flow
42. Chemical precipitates; salt deposits formed as a consequence of evaporation. Examples - rock salt and gypsum.
Alloy
Biochemical sedimentary rocks
Zone of accumulation
Evaporites
43. A reaction during which an element loses electrons - commonly takes place when elements combine with oxygen.
Gabbro
Lava tube
Ignimbrite
Oxidation
44. A felsic rock with large grains. Intrusive - phaneritic igneous rock.
Factors of magma cooling time
Granite
Facets
Soil erosion
45. 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
Sill
The effect of gas pressure on eruptive style
Reason for Earth's internal heat
Redbeds
46. Type of igneous rock composition; composed of light-colored silicates - very rich in felsic (feldspar and silica). Major constituent of continental crust.
Granitic composition
Rocks
Fragmental igneous rocks
Slab-pull force
47. Clast size - clast composition - angularity and sphericity - sorting - and character of cement.
Basaltic lava flows
Basalt
Polymorphs
Factors classifying clastic sedimentary rocks
48. 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.
Source rock composition
Fracture and cleavage
Magnetic inclination
Felsic - intermediate - mafic - ultramafic
49. Some minerals have distinctive properties - such as calcite which reacts with dilute hydrochloric acid to produce carbon dioxide. Dolomite also reacts with acid - graphite can make clear markings - magnetite attracts a magnet - halite tastes salty -
Special properties of minerals
Shield volcano
Composite cone (stratovolcano)
Dipole
50. In addition to islands that rise above sea level - seamounts have been detected (isolated submarine mountains) - once volcanoes but no longer erupt.
Erosion
Assimilation
Residual soil
Seamount chains
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