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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. 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.
Transform plate boundary
Siltstone and mudstone
Sulfides
Glass
2. 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.
Thermal expansion
Phreatomagmatic eruptions
Crust
Chemical sedimentary rocks
3. Four settings: in volcanic arcs bordering deep-ocean trenches - isolated hot spots - within continental rifts - and along mid-ocean ridges.
Convergent plate boundary
Mid-ocean ridges
Hydrosphere
Area of igneous activity
4. Sedimentary rock composed of quartz.
Silicate minerals
Siliceous rocks
Zone of accumulation
Inner core
5. Distinguishing feature of magma; the process where magma sits in a magma chamber before completely solidifying - it may incorporate chemicals derived from the walls rocks of the chamber.
Decompression
Felsic - intermediate - mafic - ultramafic
Apparent polar-wander path
Assimilation
6. The resistance to flow of magma. Reflects its distinct silica content - for silica tends to polymerize - meaning it links up to form long - chainlike molecules whose presence slows down the flowing ability of magma. Thus felsic magmas flow less easil
Cross beds
Peridotite
Sulfides
Viscosity
7. Materials that easily transform into gas at the relatively low temperatures found at the Earth's surface.
Fractional crystallization
Facets
Volatiles
12km
8. 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).
Chemical sedimentary rocks
Laccolith
Silicate minerals
Residual soil
9. Subsoil - ions and clay leached and transported down from above accumulate here. As a result - new minerals form - and clay fills open spaces. Part of the zone of accumulation.
B-horizon
Crystalline
Lower mantle
Specific gravity
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
Dipole
Siliceous rocks
Plates
11. Type of magma; high silica content - viscous - liquid at temperatures as low as 700 degrees C.
Granitic magma
Crystal structure
Differential weathering
Continental drift evidence
12. A plate boundary at which two plates move toward one another so that one plate sinks beneath the other. Subduction zones; Engage the sinking process known as subduction - between plates - consuming old oceanic lithosphere due to high density. Can sim
Rock layering
Pangaea
Convergent plate boundary
Superplumes
13. Type of soil; forms in tropical regions where abundant rainfall drenches the land during the rainy season - and the soil dries during the dry season.
Evaporites
Laterite
Regression
Effusive eruptions
14. 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
Bedrock
Magnetic anomaly
Sea-floor spreading
Compaction
15. 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.
Pangaea
Strata
Lava domes
Volcanic pipes/necks
16. Sedimentary rock composed of clay.
Glass
Fracture zones
Agrillaceous rocks
Plutons
17. An organic sedimentary rock; black - combustible rock consisting of over 50% carbon.
Granitic composition
Conchoidal fractures
Carbonates
Coal
18. Layering in sedimentary rocks.
Factors of magma cooling time
Bedding
Salt wedging
Continental shelf
19. 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.
Rock layering
Sea-floor spreading
Magnetic declination
Fragmental igneous rocks
20. The fit of the continents - locations of past glaciations - the distribution of equatorial climatic belts - the distribution of fossils - and matching geologic units.
Hot spots
Transported soil
Continental drift evidence
Chert
21. The four classes of igneous silicate rocks based on the proportion of silicon to iron and magnesium. As the proportion of silicon in a rock increases - the density decreases - thus felsic rocks are less dense than mafic. In order - from greatest to l
Continental drift hypothesis
Polymorphs
Felsic - intermediate - mafic - ultramafic
Metamorphic foliation
22. A plate boundary at which two plates move apart from one another by process of sea-floor spreading. Mid-ocean ridges or simply a ridge. New crust is formed at ridges through the buoyant rising of magma from beneath the surface and solidifies to creat
The effect of the environment on eruptive style
Divergent plate boundary
Ash
Asthenosphere
23. Chemical weathering during Which minerals dissolve into water.
Dissolution
Luster
Root wedging
Five steps of clastic sedimentary rock formation
24. Inorganic limestone; rock composed of crystalline calcium carbonate formed by chemical precipitation.
ravertine
Evaporites
Factors of magma cooling time
Apparent polar-wander path
25. 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.
Chemical weathering
Phreatomagmatic eruptions
Paleopole
Symmetry
26. Magma type; contains about 45% to 52% silica. Named because it produces rock containing abundant mafic minerals - magnesium and iron combinations.
Bathymetry
Alloy
Mafic
Frost wedging
27. Chemical weathering occurring in warm - wet climates can produce a layer of rotten rock - over 100km thick.
Saprolite
Pangaea
Gem
Metals
28. 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.
Sedimentary structure
Continental drift evidence
Explosive eruptions
Factors of magma cooling time
29. Two different minerals which have the same composition but have different crystal structures.
Root wedging
Phreatomagmatic eruptions
Polymorphs
Mid-ocean ridges
30. Type of magma; low in silica - fluid - crystallize at high temperatures.
Rock composition
Basaltic magma
Special properties of minerals
Tuff
31. 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
Coal
Polymorphs
Granitic magma
32. A thick accumulation of sediment (10-15km) - the surface of this sediment layer is this broad - shallow region.
Magnetic inclination
Continental shelf
Granitic composition
Conchoidal fractures
33. Hot basaltic lava that erupts with such low viscosity that it can flow tens to hundreds of kilometers across the landscape.
Flood basalts
Agrillaceous rocks
Evaporites
Chemical weathering
34. During the final stages of cooling - lava flows contract and may fracture into roughly hexagonal columns.
Fragmental igneous rocks
Felsic
Convective flow
Columnar jointing
35. When different rocks in an outcrop undergo weathering at different rates.
12km
Glass
Hydration
Differential weathering
36. Type of rock; accumulated sand bars - within are mineral grains of quartz and feldspar - this sediment if buried and lithified.
Marine magnetic anomaly
Arkose
Fracture and cleavage
The effect of viscosity on eruptive style
37. When water is trapped in a joint freezes - it forces the joint open and may cause the joint to grow.
Frost wedging
Upper mantle
Volcanic pipes/necks
Batholiths
38. During this process - water chemically reacts with minerals and breaks them down - working faster in slightly acidic water.
Source rock composition
Gem
Hydrolysis
Sandstone
39. 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.
Fracture and cleavage
Cementation
Cement
Glass
40. Layering in metamorphic rocks.
Lava
Thermal expansion
Transform plate boundary
Metamorphic foliation
41. A type of carbonate rock; rocks formed from the calcite or aragonite skeletons of organisms form this biochemical sedimentary rock.
Color
Limestone
Dolostone
Fissure eruptions/lava plateaus
42. 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
Crystal habit
Agrillaceous rocks
Earth's atmosphere
Carbonate rocks
43. Mineral crystal formation type; form from a solidification of a melt - meaning the freezing of a liquid.
Redbeds
Quartz sandstone
Geothermal gradient
Melting
44. 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.
Calderas
Hydrosphere
Compaction
Why magma rises
45. 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
Subsidence
Compaction
Volatiles
Magma mixing
46. 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.
Extrusive igneous rock
Subduction
pahoehoe
ravertine
47. A place where three plate boundaries intersect at a point.
The core
Pangaea
Volatiles
triple junction
48. The record of paleomagnetism revealed that the location of Earth's magnetic poles had been changing through geologic time. This 'wandering' meant that Earth's magnetic poles do not move with respect to fixed continents. Rather - continents move relat
Convective flow
Apparent polar-wander path
Oxidation
Sill
49. A naturally occurring solid - formed by geologic processes - has a crystalline structure and a definable chemical composition - and is generally inorganic.
Mineral
Relative plate velocity
Dipole
Granitic composition
50. Magma viscosity depends upon temperature - volatile content - and silica content. Hotter magma - more volatiles - and mafic magma all have less viscosity.