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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. Sphere; Surface water along with groundwater - Earth consists of 70% surface water (oceans - lakes - and streams).
Dark Silicates
Partial melting
Hydrosphere
Depositional environment
2. 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.
Polymorphs
Basaltic composition
Siltstone and mudstone
Specific gravity
3. 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.
Hot-spot track
Biomineralization
Oxides
Elemental composition of Earth
4. Solids composed of metal atoms (such as iron - aluminum - copper - and tin). Within this type of solid - outer electrons are able to flow freely.
Deposition
Streak
Metals
Crystalline igneous rocks
5. Type of lava flow; higher silica content - greater viscosity - forms a large mound above the vent out of a volcano.
Crystal lattice
atmospheres (atm)
Andesitic lava flows
Slab-pull force
6. Molten rock that has flowed out onto Earth's surface.
Deposition
Lava
The effect of gas pressure on eruptive style
Mineral
7. Sedimentary rock composed of clay.
Relative plate velocity
Agrillaceous rocks
Stoping
The effect of the environment on eruptive style
8. A process occurring when the sea level rises - the coast migrates inland. Through this - an extensive layer of beach forms.
Subduction
Clastic
Decompression
Transgression
9. Biochemical sedimentary rock; it's made from cryptocrystalline quartz. Examples - flint and jasper.
Reason for Earth's internal heat
Pyroclastic debris
Fractional crystallization
Chert
10. The absorption of water into the crystal structure of minerals - causes some minerals to expand.
Deposition
Lava domes
Dolostone
Hydration
11. Refers to the arrangement of grains in a rock; that is - the way the grains connect each other and whether inequant grains are aligned parallel to one another.
Diagenesis
Fractional crystallization
Rock texture
Granitic magma
12. Lava flowing on dry land cools more slowly that lava erupting underwater.
The effect of the environment on eruptive style
Partial melting
rifting
Lava
13. Chemical weathering occurring in warm - wet climates can produce a layer of rotten rock - over 100km thick.
Bed
Explosive eruptions
Saprolite
Limestone
14. A process occurring when sea level falls - the coast migrates seaward.
Differential weathering
Depositional environment
Glass
Regression
15. Actively slipping segment of a fracture zone between two ocean ridge segments - these faults make a third type of plate boundary - transforms.
Laccolith
Ripples
Chemical weathering
Transform fault
16. Type of lava flow; mafic - low viscosity - extremely hot - flows very quickly.
Specific gravity
Salt wedging
Basaltic lava flows
Marine magnetic anomaly
17. 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.
Grain sizes
Compaction
Transported soil
Magnetic reversals
18. An insulated - tunnel-like conduit through which lava moves within a flow.
Oxidation
Lava tube
Streak
The core
19. Magma type; contains only about 38% to 45% silica. Extreme form of mafic magma.
C-horizon
Ultramafic
Basalt
Silicate minerals
20. The broad - relatively flat regions of the ocean that lie at a depth of about 4-5km below sea level.
Oxides
Magnetic inclination
Abyssal plains
Carbonates
21. Mineral crystal formation type; form at interfaces between the physical and biological components of the Earth system by this process.
Ripples
Grain sizes
collision
Biomineralization
22. Fluid basaltic lava extruded from crustal fractures called fissures.
12km
Plate tectonics
Fissure eruptions/lava plateaus
Plates
23. 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
Hydration
Oxidation
Granitic magma
Volatiles
24. Sedimentary rocks made up of the shells of organisms.
Streak
Biochemical sedimentary rocks
Silicates
Pyroclastic debris
25. The force that subducting plates apply to oceanic lithosphere at a convergent boundary - arises simply because lithosphere formed 10 million years ago is denser than asthenosphere - so it can sink into the asthenosphere. Thus once an oceanic plate st
Convective flow
Chemical sedimentary rocks
Melts
Slab-pull force
26. 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.
Sandstone
Relative plate velocity
Sulfates
Magnetic declination
27. 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.
Hydrosphere
Fissure eruptions/lava plateaus
Sulfides
rifting
28. 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
Polymorphs
Lava tube
Chert
29. 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
Weathering
Streak
Spreading rate
rifting
30. Mineral crystal formation type; form from a solidification of a melt - meaning the freezing of a liquid.
Gabbro
Dipole
rifting
Melting
31. A layer of sediment in which grain size varies from coarse at the bottom to fine at the top.
Transform fault
Hot-spot track
Graded bed
Calderas
32. Outer surface level of Earth; composed of granite - basalt - and gabbro. Continental: mostly about 35-40km thick . Oceanic: about 7-10km thick. Oxygen - by far the most abundant element.
Ripples
Crust
Lithosphere
Diagenesis
33. 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
Soil
Oxidation
Viscosity
Oxides
34. 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.
Clastic
Specific gravity
Melting
Transition zone
35. Magma type; contains about 66% to 76% silica. Name reflects the occurrence of feldspar and quartz in rocks formed in this magma.
Oxides
Earth's atmosphere
Felsic
Clastic
36. The way in which the atoms are packed together within a mineral by chemical bonds. Five difference types of bonding can occur - covalent - ionic - metallic - Van der Waal's - and hydrogen.
Crystal structure
Organic sedimentary rocks
Chemical weathering
Euhedral crystal
37. Built up deposit of volcanic bombs and lapilli - known as volcanic agglomerate.
Tuff
Zone of accumulation
The core
Chemical sedimentary rocks
38. 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
Convergent plate boundary
Coal
Siliceous rocks
Bedrock
39. Mineral class; the anion within these types of minerals is a halogen ion (such as chlorine or fluorine).
Oxidation
Organic chemicals
Halides
ravertine
40. Process where new divergent boundaries form when a continent splits and separates into two continents.
Flood basalts
Siliceous rocks
Area of igneous activity
rifting
41. 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.
Plate tectonics
Strata
Batholiths
Sedimentary structure
42. A cut and finished stone ready to be used in jewelry. Examples - diamond - ruby - sapphire - emerald.
Gem
Regression
Dunes
Dipole
43. 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.
Flood basalts
Caliche
Color
Subsidence
44. The conditions in which sediment was deposited. Examples - beach - glacial - and/or river environments.
Transgression
Oxides
Magma's speed of flow
Depositional environment
45. Sedimentary rock consisting of cemented together solid fragments and grains derived from preexisting rocks.
Phreatomagmatic eruptions
Effusive eruptions
Clastic sedimentary rocks
Laccolith
46. 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
Inner core
Flood basalts
Silicate minerals
Basalt
47. Type of lava flow; a lava flow with warm - pasty surfaces wrinkling into smooth - glassy - rope-like bridges.
Alloy
The effect of the environment on eruptive style
Carbonate rocks
pahoehoe
48. Places with particularly voluminous quantities of magma erupting or intruding.
Sea-floor spreading
Agrillaceous rocks
Thermal expansion
Large Igneous Provinces (LIPs)
49. Hot basaltic lava that erupts with such low viscosity that it can flow tens to hundreds of kilometers across the landscape.
Sulfides
Flood basalts
A-horizon
Diagenesis
50. Similar to ripples - but are much larger. Small ripples often form on the surface of these structures.
Fumerolic mineralization
rifting
Chert
Dunes