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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. Natural cracks that form in rocks due to removal of overburden or due to cooling.
Viscosity
Jointing
The effect of the environment on eruptive style
Continental rift
2. Some rocks develop their magnetization - their ability to produce a magnetic field - at the time that the rocks themselves formed. Such rocks - preserve a record of the Earth's magnetic field at known times in the past.
Peridotite
Paleomagnetism
Euhedral crystal
Hot spots
3. A process occurring when the sea level rises - the coast migrates inland. Through this - an extensive layer of beach forms.
Crystal
Hydration
Luster
Transgression
4. Type of soil; forms from sediment that has been carried in from elsewhere. Include those formed from deposits left by rivers - glaciers - or wind.
Frost wedging
Transported soil
rifting
The effect of viscosity on eruptive style
5. Inorganic limestone; rock composed of crystalline calcium carbonate formed by chemical precipitation.
Xenolith
Magnetic anomaly
ravertine
Why magma rises
6. 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
Magnetic declination
Viscosity
Dike
7. Type of volcanic eruption; produce mainly lava flows - yield low-viscosity basaltic lavas.
Deposition
Effusive eruptions
Alloy
Redbeds
8. Forms a 2885-km-thick layer surrounding the core. In terms of volume - it is the largest part of the Earth. It consists entirely of ultramafic rock - peridotite.
pahoehoe
Abyssal plains
Mineral crystal destruction
Mantle
9. 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
Metamorphic rocks
Gem
Dolostone
10. The ocean floor is diced up by narrow bands of vertical fractures. Lie roughly at right angles to mid-ocean ridges - effectively segmenting the ridges into small pieces.
Inner core
Lava
Relative plate velocity
Fracture zones
11. 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
Mantle
Ultramafic
Crystal lattice
Apparent polar-wander path
12. Layering in metamorphic rocks.
Metamorphic foliation
Turbidity current
Fissure eruptions/lava plateaus
Physical weathering
13. Along much of the perimeter of the Pacific Ocean - the ocean floor reaches astounding depths of 8-12km. These areas define elongate troughs - and they border volcanic arcs - the curving chains of active volcanoes.
Calderas
Volatiles
Deep-ocean trenches
Large Igneous Provinces (LIPs)
14. Mineral group; feldspars - quartz - muscovite - clay minerals.
Light silicates
Tuff
Bathymetry
Fragmental igneous rocks
15. Successive turbidity currents deposit successive graded beds - creating this sequence of strata.
Depositional environment
Turbidite
Stoping
Magnetic reversals
16. 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.
pahoehoe
Physical weathering
Mid-ocean ridges
Subduction
17. Sedimentary rocks made up of minerals that precipitate directly from water solutions.
Light silicates
Continental rift
Soil Horizons
Chemical sedimentary rocks
18. 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.
Bedding
Glass
Relative plate velocity
Euhedral crystal
19. Core division; from a depth of 5155km down to Earth's center at 6371km. A radius of about 1220km - is solid iron-nickel alloy - can reach temperature of 4700 degrees C. Solid in nature because of subjection to greater pressure - keeps atoms from wand
Paleomagnetism
Dunes
Inner core
Batholiths
20. The boundary between two beds is a bedding plane; several beds constitute this structure.
Polymorphs
Strata
Clastic
Mantle plume
21. A layer of sediment in which grain size varies from coarse at the bottom to fine at the top.
Graded bed
Outer core
Ridge-push force
Deposition
22. The conditions in which sediment was deposited. Examples - beach - glacial - and/or river environments.
Basaltic magma
Clastic
Depositional environment
Magnetic declination
23. 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.
Arkose
Glass
Transform plate boundary
Symmetry
24. Physical property of a mineral; a measure of a minerals relative ability to resist scratching - and therefore represents the resistance of bonds in the crystal structure being broken. The atoms or ions in crystals of a hard mineral are more strongly
Dolostone
Facets
Carbonates
Hardness
25. Physical property of a mineral; represents the density of a mineral - as specified by the ratio between the weight of a volume of the mineral and the weight of an equal volume of water a 4 degrees C.
Granite
Specific gravity
Symmetry
Cross beds
26. Physical property of a mineral; different minerals fracture in different ways - depending on the internal arrangement of atoms. If a mineral breaks to form distinct planar surfaces that have a specific orientation in relation to the crystal structure
Streak
Grain sizes
Fracture and cleavage
Loam
27. Layering in sedimentary rocks.
Solid-state diffusion
Regression
Bedding
Viscosity
28. Form when solid materials become hot and transform into liquid - example - molten rock.
Dissolution
Area of igneous activity
Melts
Melting
29. A type of carbonate rock; rocks formed from the calcite or aragonite skeletons of organisms form this biochemical sedimentary rock.
Cement
Felsic
Limestone
Sedimentary rocks
30. Rocks which develop when hot molten rock cools and freezes solid.
Igneous rocks
Area of igneous activity
Fissure eruptions/lava plateaus
Glass
31. Occurs within the asthenosphere - actively drags plates along and attributes partially for the mechanism shifting the plates along the Earth's surface.
Convective flow
Dark Silicates
Coal
Viscosity
32. Mineral crystal formation type; form by type of diffusion - the movement of atoms or ions through a solid to arrange into a new crystal structure; process takes place very slowly.
Mantle plume
Continental drift evidence
Source rock composition
Solid-state diffusion
33. 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
Intermediate
Magma mixing
Halides
Pangaea
34. Perhaps the cause for the large igneous provinces; formations within the mantle - plumes that bring up vastly more hot asthenosphere than normal plumes.
Bedrock
Superplumes
Volatiles
Bed
35. The separated lithosphere into distinct pieces. Twelve major 'pieces' and several minor. Consist of active margins and passive margins between them.
Grain sizes
Plates
Gem
Flood basalts
36. 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.
Bathymetry
Sulfides
Fractional crystallization
Mantle plume
37. Mineral class; consist of pure masses of a single metal - with metallic bonds. Copper and gold can appear in this way.
pahoehoe
Native metals
Effusive eruptions
The effect of viscosity on eruptive style
38. 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
Dike
Magnetic reversals
Intrusive igneous rock
Deep-ocean trenches
39. The crust moves away from the Mid-Atlantic Ridge axis at a rate of 1cm per year. This velocity of sea-floor spreading is determined by the relationship between the paleomagnetic anomaly-stripe's width and the reverse polarity duration - the data reve
Intrusive igneous rock
Lithification
Silicate minerals
Spreading rate
40. 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.
Fracture and cleavage
Fissure eruptions/lava plateaus
Compaction
Phreatomagmatic eruptions
41. Mineral group; olivine group - pyroxene group - amphibole group.
Subduction
Dark Silicates
Strata
Transform fault
42. 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
Plates
The effect of gas pressure on eruptive style
Glassy igneous rocks
Pangaea
43. 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
Soil
rifting
Asthenosphere
44. Type of lava flow; higher silica content - greater viscosity - forms a large mound above the vent out of a volcano.
Andesitic lava flows
Strata
Dipole
Chert
45. 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 lava flows
Biomineralization
Basaltic composition
Asthenosphere
46. The distance that the world's deepest mine-shaft penetrates into the Earth beneath South Africa.
3.5km (2 miles)
Polymorphs
The effect of gas pressure on eruptive style
Continental drift hypothesis
47. Deeper sublayer of the mantle - depth of 660km to 2900km.
Cinder cone
The effect of viscosity on eruptive style
Lower mantle
Crust
48. 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
Reason for Earth's internal heat
Divergent plate boundary
Mineral
Cementation
49. Sedimentary rocks made up of the shells of organisms.
Biochemical sedimentary rocks
Convective flow
Native metals
Depositional environment
50. Physical features of the land surface represented by changes in elevation.
Agrillaceous rocks
Topography
Cinder cone
Color