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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. 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.
Erosion
Ridge-push force
Coal
Residual soil
2. 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.
Outcrop
Silicate minerals
Cement
Magnetic declination
3. Magma type; contains about 66% to 76% silica. Name reflects the occurrence of feldspar and quartz in rocks formed in this magma.
Precipitation
Felsic
Sea-floor spreading
Fumerolic mineralization
4. 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
Silicates
Magma's speed of flow
Turbidity current
Deposition
5. Distinguishing feature of magma; the process where magma changes composition as it cools because formation and sinking of crystals preferentially remove certain atoms from the magma.
Fractional crystallization
Sandstone
Jointing
Marine magnetic anomaly
6. A fine spray of lava instantly freezes to form fine particles of glass.
Felsic - intermediate - mafic - ultramafic
Ash
Subduction
Oxides
7. Times when the Earth's magnetic field flips from normal to reversed polarity - or vice versa. When the Earth has reversed polarity - the south magnetic pole lies near the north geographic pole - and the north magnetic pole lies near the south geograp
Outcrop
Magnetic reversals
Saprolite
Metals
8. Chemical weathering during Which minerals dissolve into water.
Zone of leaching
Seamount chains
Crystal structure
Dissolution
9. The speed of the movements of the plates with respect to the speed of the other plates' movements. Absolute plate velocity is a measure of the movement of any plates relative to a fixed point in the mantle.
E-horizon
Plates
Basaltic lava flows
Relative plate velocity
10. The absorption of water into the crystal structure of minerals - causes some minerals to expand.
Hydration
The effect of the environment on eruptive style
Organic chemicals
Crystal
11. 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.
Basaltic lava flows
Physical weathering
Lapilli
The effect of the environment on eruptive style
12. 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
pahoehoe
Fumerolic mineralization
Divergent plate boundary
Batholiths
13. On a gem are the ground and polished surfaces made with a certain type of machine.
Facets
Crystal structure
Crystal lattice
Oxidation
14. 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
Reason for Earth's internal heat
The effect of gas pressure on eruptive style
Transition zone
Columnar jointing
15. A felsic rock with large grains. Intrusive - phaneritic igneous rock.
Evaporites
Igneous rocks
Rocks
Granite
16. Forms from a chemical reaction between solid calcite and magnesium-bearing groundwater.
Dolostone
Sea-floor spreading
Plates
Source rock composition
17. Mineral crystal formation type; from directly from a vapor - occurs around volcanic vents or around geysers. At such locations - volcanic gases or steam enter the atmosphere and cool - so certain elements cannot remain in gaseous form.
Fumerolic mineralization
Differential weathering
Dike
Lava tube
18. Rock formations still attached to the Earth's crust.
Hot spots
Bedrock
Shield volcano
Oxidation
19. Distinguishing feature of magma; Because not all minerals melt by the same amount under given conditions - and because chemical reactions take place during melting - the magma that forms as a rock begins to melt does not have the same composition as
Partial melting
Viscosity
Regolith
Igneous rocks
20. A term used for all the physical - chemical - and biological processes that transform sediment into sedimentary rock and that alter characteristics of sedimentary rock one the rock has formed.
Diagenesis
Melts
Andesitic lava flows
Magnetic anomaly
21. 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
Lava domes
Bedrock
Seamount chains
22. 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).
Cementation
Metals
A-horizon
Graded bed
23. Actively slipping segment of a fracture zone between two ocean ridge segments - these faults make a third type of plate boundary - transforms.
Bedding
Transform fault
Crystal lattice
Continental shelf
24. Molten rock that has flowed out onto Earth's surface.
collision
Sulfates
Lava
Basalt
25. Because different soil-forming processes operate at different depths - soils typically develop into these distinct zones. These zones can be arranged vertically into a soil profile.
Hydration
Tuff
Soil Horizons
Outcrop
26. 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
Salt wedging
Facets
Hydrosphere
Crystal lattice
27. An exposure of bedrock.
Transgression
The effect of viscosity on eruptive style
Outcrop
Ultramafic
28. A type of soil consisting of about 10-30% clay and the rest silt and sand. Pores remain between grains so that water and air can pass through and roots can easily penetrate.
Sulfides
Loam
Earth's atmosphere
Factors classifying clastic sedimentary rocks
29. 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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30. Successive turbidity currents deposit successive graded beds - creating this sequence of strata.
Root wedging
Assimilation
Turbidite
Andesitic lava flows
31. Sedimentary rock consisting of cemented together solid fragments and grains derived from preexisting rocks.
Clastic sedimentary rocks
Relative plate velocity
Metals
Regression
32. Irregular or blob-shaped intrusions that range in size from tens of meters across to tens of kilometers across.
Plutons
Redbeds
a'a'
Biochemical sedimentary rocks
33. A sedimentary bed that has developed a reddish color. The red comes from a film of iron oxide (hematite) that forms on grain surfaces.
Salt wedging
Soil erosion
Soil
Redbeds
34. Sedimentary rocks consisting of carbon-rich relicts of plants.
Fracture zones
Root wedging
Organic sedimentary rocks
Lava tube
35. A type of carbonate rock; rocks formed from the calcite or aragonite skeletons of organisms form this biochemical sedimentary rock.
Peridotite
Limestone
Elemental composition of Earth
Redbeds
36. Pea to plum-sized fragments of pyroclastic debris - consists of pumice or scoria fragments.
Lapilli
Melting
Deposition
Paleomagnetism
37. Mineral class; consist of pure masses of a single metal - with metallic bonds. Copper and gold can appear in this way.
Intrusive igneous rock
Magma
Native metals
Regolith
38. Lava flowing on dry land cools more slowly that lava erupting underwater.
The effect of the environment on eruptive style
Convergent plate boundary
Ripples
Magnetic declination
39. 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.
Rhyolitic lava flows
Magma mixing
Mantle
Magma's speed of flow
40. 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.
collision
Differential weathering
Area of igneous activity
Cinder cone
41. 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.
Slab-pull force
Pangaea
Shield volcano
Conglomerate
42. A single - continuous (uninterrupted) piece of a crystalline solid bounded by flat surfaces called crystal faces that grew naturally as the mineral formed. Come in a variety of shapes - cubes - trapezoids - pyramids - octahedrons - hexagonal columns
Crystal
Mid-ocean ridges
Ultramafic
Factors of magma cooling time
43. When silt and clay accumulate in the flat areas bordering a stream - lagoon - or delta - the silt when lithified becomes this type of sediment. And the mud - when lithified - becomes another type of sediment - also known as shale.
Siltstone and mudstone
Luster
Fracture zones
Continental drift evidence
44. Sedimentary rock composed of clay.
Factors of magma cooling time
Factors classifying clastic sedimentary rocks
Agrillaceous rocks
Ripples
45. 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).
Transition zone
Chemical sedimentary rocks
Silicate minerals
Why magma rises
46. During the final stages of cooling - lava flows contract and may fracture into roughly hexagonal columns.
Caliche
Columnar jointing
Transform plate boundary
Why magma rises
47. Soil section below the A-horizon; a soil level that has undergone substantial leaching but has not yet mixed with organic material. Because it lacks organic materials - this horizon tends to be lighter than the A-horizon. Part of the zone of leaching
Thermal expansion
E-horizon
Volatiles
Luster
48. Volcanic landform; bulbous mass of congealed lava - associated with explosive eruptions of gas-rich magma.
Peridotite
Continental drift hypothesis
Saprolite
Lava domes
49. 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
Abyssal plains
Saprolite
Dipole
Sandstone
50. A sediment-filled depression; in an area where the lithosphere has subsided.
Rock layering
Hardness
Sedimentary Basins
Cement