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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.
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 place where three plate boundaries intersect at a point.
Clastic
Ignimbrite
Zone of leaching
triple junction
2. A thick accumulation of sediment (10-15km) - the surface of this sediment layer is this broad - shallow region.
Polymorphs
O-horizon
Continental shelf
Rock texture
3. During the final stages of cooling - lava flows contract and may fracture into roughly hexagonal columns.
Columnar jointing
Mineral
Ripples
Calderas
4. Mineral class; consist of a metal cation bonded to the anionic group. Many form by precipitation out of water at or near the Earth's surface. Example - gypsum.
Volatiles
Xenolith
Gem
Sulfates
5. The boundary between two beds is a bedding plane; several beds constitute this structure.
Graded bed
Physical weathering
Rocks
Strata
6. The distance of the deepest well ever drilled - hole in northern Russia. Penetrates only about 0.03% of the Earth.
Graded bed
atmospheres (atm)
Weathering
12km
7. Refers to the processes that break up and corrode solid rock - eventually transforming it into sediment. Physical and chemical variations.
Chert
Metamorphic foliation
Weathering
C-horizon
8. Chemical weathering occurring in warm - wet climates can produce a layer of rotten rock - over 100km thick.
Saprolite
Viscosity
Peridotite
Felsic - intermediate - mafic - ultramafic
9. 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
Volcano
Biomineralization
Rhyolitic lava flows
10. Natural bond connecting rocks; mineral material that precipitates from water and fills the space between grains.
ravertine
Chemical sedimentary rocks
Cement
O-horizon
11. Mineral class; consist of metal cations bonded by oxygen anions. Examples - hematite and magnetite. Some contain a relatively high proportion of metal atoms - and thus are ore minerals.
Deep-ocean trenches
Biomineralization
Oxides
Mantle
12. Volcanic landform; bulbous mass of congealed lava - associated with explosive eruptions of gas-rich magma.
Graded bed
Lava domes
Intermediate
Melts
13. Mineral class; the fundamental component within these types of minerals in the Earth's crust is the silicon-oxygen tetrahedron anionic group - a silicon atom surrounded by four oxygen atoms that are arranged to define the corners of a tetrahedron - a
Salt wedging
Silicates
E-horizon
Metamorphic foliation
14. An ultramafic rock with large grains. intrusive - phaneritic igneous rock.
Laccolith
Crystal
Peridotite
Dunes
15. A process occurring when sea level falls - the coast migrates seaward.
Relative plate velocity
Sill
Regression
Marine magnetic anomaly
16. 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.
Factors classifying clastic sedimentary rocks
Carbonate rocks
Oxides
Quartz sandstone
17. Built up deposit of volcanic bombs and lapilli - known as volcanic agglomerate.
Plates
Continental rift
Tuff
Explosive eruptions
18. Rocks that consist of mineral crystals that intergrow when the melt solidifies - interlocking structure. Examples - granite and rhyolite.
Superplumes
Crystalline igneous rocks
Sedimentary Basins
Asthenosphere
19. Process where new divergent boundaries form when a continent splits and separates into two continents.
Why magma rises
Oxides
rifting
Caliche
20. 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 -
Phreatomagmatic eruptions
Special properties of minerals
Rocks
Crystalline igneous rocks
21. Physical features of the land surface represented by changes in elevation.
The effect of viscosity on eruptive style
Outcrop
Topography
Ash
22. 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.
Evaporites
Hot spots
Dike
Limestone
23. Some rock bodies appear to contain distinct formations - defined either by bands of different compositions or textures - or by the alignment of inequant grains so that they trend parallel to one another.
Fissure eruptions/lava plateaus
Rhyolitic lava flows
Subduction
Rock layering
24. Refers to the chemical reactions that alter or destroy minerals when rock comes in contact with water solutions or air.
Soil Horizons
Chemical weathering
Salt wedging
Magnetic anomaly
25. A mixture containing more than one type of metal atom. Example - bronze is a mixture of copper and tin.
Partial melting
Alloy
Fracture zones
Cementation
26. Rocks which develop when hot molten rock cools and freezes solid.
Abyssal plains
Rhyolitic lava flows
Igneous rocks
Grain sizes
27. Tree roots that grow into joints can push those joints open in this process.
Root wedging
Grain sizes
Euhedral crystal
Explosive eruptions
28. The compiled data from many marine cruises which defined a distinctive - striped and alternating bands of paleomagnetism.
Volcanic blocks/bombs
Mafic
Marine magnetic anomaly
Dike
29. Weathering - erosion - transportation - deposition - and lithification.
Five steps of clastic sedimentary rock formation
Reason for Earth's internal heat
Tuff
Facets
30. The angle between the direction that a compass needle points at a given location and the direction of the 'true' (geographic) north. Through this process - the magnetic poles never stray more than 15 degrees of latitude from the geographic pole.
Magnetic declination
Zone of accumulation
Fracture and cleavage
a'a'
31. Volcanic landform; steep walled depression at the summit - size exceeds one kilometer in diameter.
Siliceous rocks
Volcano
Paleomagnetism
Calderas
32. The removal of soil by running water or by wind.
Native metals
Transform plate boundary
Soil erosion
Hydration
33. Cause of melting; the variation in temperature with depth is expressed in the geotherm; because pressure prevents melting - a decrease in pressure can permit melting. Specifically - if the pressure affecting hot mantle rock decreases while the temper
Conglomerate
Gem
Fumerolic mineralization
Decompression
34. Unconsolidated deposits of pyroclastic grains - regardless of size - that have been erupted from a volcano constitute these pyroclastic deposits.
Calderas
Tephra
Precipitation
Magnetic anomaly
35. 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.
Pyroclastic debris
Compaction
Luster
Continental shelf
36. Materials that easily transform into gas at the relatively low temperatures found at the Earth's surface.
Composite cone (stratovolcano)
Volatiles
Relative plate velocity
Special properties of minerals
37. 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
Fractional crystallization
Weathering
Fracture zones
38. A process occurring when the sea level rises - the coast migrates inland. Through this - an extensive layer of beach forms.
650-1100 degrees C
Continental rift
Plutons
Transgression
39. Layering in sedimentary rocks.
Peridotite
Bedding
A-horizon
Mantle
40. Distinguishing feature of magma; the process where different magmas formed in different locations from different sources may come in contact within a magma chamber prior to freezing. Thus the originally distinct magmas mix to create a new - different
Source rock composition
Zone of leaching
Magma mixing
Continental shelf
41. Type of lava flow; higher silica content - greater viscosity - forms a large mound above the vent out of a volcano.
A-horizon
Pyroclastic flows
Andesitic lava flows
Rock-forming silicate minerals
42. Farther down from a zone of leaching - new mineral crystals precipitate directly out of the water or form when the water reacts with debris - this the region where the new minerals and clay collect.
Cement
Zone of accumulation
Streak
Intrusive igneous rock
43. A fine spray of lava instantly freezes to form fine particles of glass.
Ash
Felsic
Diagenesis
Organic chemicals
44. A reference to the supposed position of the Earth's magnetic pole at a time in the past.
Laterite
Facets
Paleopole
12km
45. Mineral crystal formation type; form from a solution - meaning that atoms - molecules - or ions dissolved in water bond together out of water.
Asthenosphere
Transform fault
Transgression
Precipitation
46. A cut and finished stone ready to be used in jewelry. Examples - diamond - ruby - sapphire - emerald.
Basaltic magma
Dipole
Gem
Reason for Earth's internal heat
47. Pea to plum-sized fragments of pyroclastic debris - consists of pumice or scoria fragments.
Siltstone and mudstone
Slab-pull force
Limestone
Lapilli
48. Volcanic landform; pipes are short conduits that connect a magma chamber to the surface.
Outer core
atmospheres (atm)
Mineral
Volcanic pipes/necks
49. An intrusion starting to inject between layers but then dome upwards - creating this blister-shaped intrusion.
Biomineralization
Laccolith
Effusive eruptions
Cementation
50. Rocks that forms by the freezing of lava above ground - after it spills out (extrudes) onto the surface of the Earth and comes into contact with the atmosphere or ocean.
Ripples
Lava domes
Extrusive igneous rock
Abyssal plains
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