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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. 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.
Explosive eruptions
Fracture zones
Siliceous rocks
650-1100 degrees C
2. Clast size - clast composition - angularity and sphericity - sorting - and character of cement.
Intrusive igneous rock
Siltstone and mudstone
Large Igneous Provinces (LIPs)
Factors classifying clastic sedimentary rocks
3. The layering nature of sedimentary rocks - surface features of layers formed during deposition - and the arrangement of grains within layers.
Composite cone (stratovolcano)
Sedimentary structure
Heat transfer
12km
4. Volcanoes that exist as isolated points and appear to be independent of movement at a plate boundary - hot-spot volcanoes. Mostly are located on the interior of plates - away from boundaries.
Subsidence
Hot spots
Stratagraphic formation
Ridge-push force
5. 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.
Basaltic lava flows
Cinder cone
Paleomagnetism
Carbonate rocks
6. A solid in which atoms are not arranged in an orderly pattern. Forms when a liquid freezes so fast that atoms do not have time to organize into an orderly pattern.
Transform fault
Glass
Alloy
Superplumes
7. Type of rock; accumulated sand bars - within are mineral grains of quartz and feldspar - this sediment if buried and lithified.
Bedding
Gem
Convergent plate boundary
Arkose
8. A mafic rock with small grains. Extrusive - aphanitic igneous rock.
Physical weathering
Mafic
Why magma rises
Basalt
9. A submarine suspension of sediment.
12km
Ridge-push force
Turbidity current
Volcanic pipes/necks
10. 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.
Sulfides
Continental drift hypothesis
Pyroclastic debris
Lithosphere
11. A nearly horizontal - tabletop-shaped tabular intrusion - parallel to layering within the earth.
O-horizon
Volatiles
Deep-ocean trenches
Sill
12. Type of soil; forms from sediment that has been carried in from elsewhere. Include those formed from deposits left by rivers - glaciers - or wind.
Transported soil
Pyroclastic flows
Oxides
Superplumes
13. A thick accumulation of sediment (10-15km) - the surface of this sediment layer is this broad - shallow region.
Dark Silicates
Continental shelf
Arkose
Loam
14. 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.
Divergent plate boundary
E-horizon
Factors of magma cooling time
Batholiths
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
16. Cause of melting; when magma rises up from the mantle into the crust - it brings heat with it which raises the temperature of the surrounding crustal rock - and in some cases melting occurs.
Heat transfer
Basaltic composition
Columnar jointing
Glassy igneous rocks
17. A sheet of tuff formed from a pyroclastic flow.
Ignimbrite
C-horizon
Ripples
Plutons
18. 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
Magma mixing
Convergent plate boundary
Streak
Earth's atmosphere
19. 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
Pangaea
Euhedral crystal
Continental rift
Volatiles
20. Coarse pyroclastic debris - apple to refrigerator-sized fragments. Chunks of preexisting igneous rock or large lava blobs which discharge from volcanic eruptions.
Sulfides
Volcanic blocks/bombs
Hot-spot track
Compaction
21. Type of igneous rock composition; composed of light-colored silicates - very rich in felsic (feldspar and silica). Major constituent of continental crust.
Intrusive igneous rock
Granitic composition
Stoping
Area of igneous activity
22. Process occurring in arid climates - dissolved salt in groundwater precipitates and grows as crystals in open pore spaces in rocks. This process pushes apart the surrounding grains and so weakens the rock that when exposed to wind or rain - the rock
Crystalline
Cementation
Thermal expansion
Salt wedging
23. Type of lava flow; higher silica content - greater viscosity - forms a large mound above the vent out of a volcano.
Physical weathering
Andesitic lava flows
Batholiths
Divergent plate boundary
24. 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).
Stratagraphic formation
O-horizon
Carbonate rocks
Silicate minerals
25. 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.
Lithification
650-1100 degrees C
B-horizon
C-horizon
26. Inorganic limestone; rock composed of crystalline calcium carbonate formed by chemical precipitation.
Fumerolic mineralization
ravertine
Pyroclastic debris
Fracture and cleavage
27. Magma type; contains about 66% to 76% silica. Name reflects the occurrence of feldspar and quartz in rocks formed in this magma.
Felsic
Sea-floor spreading
Hot spots
Seamount chains
28. 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.
Sulfides
Lithification
Compaction
Biomineralization
29. 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.
Rock-forming silicate minerals
Sill
Deep-ocean trenches
Explosive eruptions
30. The transformation of loose sediment into solid rock.
Chemical weathering
Source rock composition
Lithification
Volcanic pipes/necks
31. 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.
Effusive eruptions
Fumerolic mineralization
Crystalline igneous rocks
Bathymetry
32. Sedimentary rocks made up of the shells of organisms.
Biochemical sedimentary rocks
Hardness
Salt wedging
Lava tube
33. Solids composed of metal atoms (such as iron - aluminum - copper - and tin). Within this type of solid - outer electrons are able to flow freely.
Redbeds
Metals
Rhyolitic lava flows
Saprolite
34. 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.
Continental shelf
Physical weathering
Paleopole
Phreatomagmatic eruptions
35. Magma is less dense than surrounding rock - and thus is buoyant. Magma is less dense both because rock expands as it melts and because magma tends to contain smaller proportions of heavy elements. Also - magma rises because the weight of overlying ro
Why magma rises
Felsic
Turbidite
Hydrolysis
36. 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.
Outer core
Bedding
Tuff
Source rock composition
37. Fracture type; smoothly curving - clamshell-shaped surfaces; typically formed in quartz.
E-horizon
Conchoidal fractures
The effect of viscosity on eruptive style
Transported soil
38. 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.
Strata
Hydrolysis
Fragmental igneous rocks
C-horizon
39. Physical property of a mineral; refers to the way a mineral surface scatters light. Metallic versus non-metallic in nature.
Magma
Batholiths
Rock-forming silicate minerals
Luster
40. Sedimentary rocks consisting of carbon-rich relicts of plants.
Dark Silicates
Sulfates
rifting
Organic sedimentary rocks
41. Sphere; Surface water along with groundwater - Earth consists of 70% surface water (oceans - lakes - and streams).
Ultramafic
Hydrosphere
Biochemical sedimentary rocks
Topography
42. Type of soil; forms directly from underlying bedrock.
Residual soil
Dipole
Stoping
Siliceous rocks
43. The boundary between two beds is a bedding plane; several beds constitute this structure.
Gabbro
Volatiles
Strata
B-horizon
44. Rigid outer layer of Earth - 100-150km thick. Consists of the crust plus the uppermost part of the mantle.
Earth's atmosphere
B-horizon
Lithosphere
The core
45. 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
Metamorphic foliation
Residual soil
Grain sizes
Magnetic anomaly
46. During this process - water chemically reacts with minerals and breaks them down - working faster in slightly acidic water.
Fractional crystallization
Hydrolysis
Magnetic reversals
Magnetic inclination
47. 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.
Mantle plume
atmospheres (atm)
Basaltic composition
Glass
48. The process by which sediment settles out of the transporting medium.
Deposition
Plate tectonics
Carbonates
Continental drift hypothesis
49. 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.
Stratagraphic formation
Rhyolitic lava flows
Specific gravity
Magnetic declination
50. 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.
Seamount chains
Soil
Stoping
Sedimentary structure