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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. An insulated - tunnel-like conduit through which lava moves within a flow.
Lava tube
Tephra
Convergent plate boundary
Superplumes
2. The transformation of loose sediment into solid rock.
Relative plate velocity
Lithification
Organic chemicals
Residual soil
3. Contributes to formation of soil; occurs when rainwater percolates through the debris and carries dissolved ions and clay flakes downward - This is the region where the downward transport occurs.
Regolith
Ridge-push force
Zone of leaching
Area of igneous activity
4. The conditions in which sediment was deposited. Examples - beach - glacial - and/or river environments.
Topography
Light silicates
Marine magnetic anomaly
Depositional environment
5. Mineral class; consist of pure masses of a single metal - with metallic bonds. Copper and gold can appear in this way.
Weathering
Native metals
Strata
Redbeds
6. An exposure of bedrock.
Outcrop
Basaltic magma
a'a'
Rocks
7. A distinctive sequence of strata traced across a fairly large region. For example - a region may contain a succession of alternating sandstone and shale beds deposited by rivers - overlain by beds of marine limestone deposited later.
Pyroclastic flows
ravertine
Coal
Stratagraphic formation
8. 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
Continental rift
Magma's speed of flow
Magnetic reversals
Carbonates
9. The distance of the deepest well ever drilled - hole in northern Russia. Penetrates only about 0.03% of the Earth.
12km
Glassy igneous rocks
Lava
Thermal expansion
10. Molten rock beneath Earth's surface.
Hot-spot track
Magma
Metamorphic rocks
Redbeds
11. A thick accumulation of sediment (10-15km) - the surface of this sediment layer is this broad - shallow region.
Asthenosphere
Continental shelf
Felsic - intermediate - mafic - ultramafic
Fractional crystallization
12. Magma type; contains about 45% to 52% silica. Named because it produces rock containing abundant mafic minerals - magnesium and iron combinations.
Geothermal gradient
Color
Rock layering
Mafic
13. The freely pivoting up and down compass needle's angle of tilt relative to the location upon the Earth's surface. At the equator - the specialized magnetic needle would position horizontally and at a magnetic pole it would point straight down.
Convective flow
Magnetic inclination
Sill
Xenolith
14. Mineral group; feldspars - quartz - muscovite - clay minerals.
Light silicates
Evaporites
Fragmental igneous rocks
Granitic composition
15. Process where a convergent boundary ceases to exist when a piece of buoyant lithosphere - such as a continent or island arc - moves into the subduction zone. Yield some of the most spectacular mountains/mountain ranges on the planet including the Him
Ignimbrite
E-horizon
collision
Chemical sedimentary rocks
16. 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
Five steps of clastic sedimentary rock formation
Cross beds
Volatiles
Conglomerate
17. Biochemical sedimentary rock; it's made from cryptocrystalline quartz. Examples - flint and jasper.
Crystalline
Batholiths
Chert
Regression
18. The separated lithosphere into distinct pieces. Twelve major 'pieces' and several minor. Consist of active margins and passive margins between them.
Dolostone
Plates
Paleomagnetism
Tuff
19. Four settings: in volcanic arcs bordering deep-ocean trenches - isolated hot spots - within continental rifts - and along mid-ocean ridges.
Area of igneous activity
Heat transfer
Magma
Rhyolitic lava flows
20. A mafic rock with small grains. Extrusive - aphanitic igneous rock.
Basalt
Large Igneous Provinces (LIPs)
Bedding
Evaporites
21. 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
Zone of leaching
Soil Horizons
Batholiths
22. 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
Hydrolysis
Arkose
Why magma rises
Magnetic anomaly
23. Refers to the chemical reactions that alter or destroy minerals when rock comes in contact with water solutions or air.
Rock-forming silicate minerals
The effect of the environment on eruptive style
Composite cone (stratovolcano)
Chemical weathering
24. A felsic rock with large grains. Intrusive - phaneritic igneous rock.
Pyroclastic debris
Root wedging
12km
Granite
25. 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
The effect of gas pressure on eruptive style
triple junction
Convergent plate boundary
Gem
26. A reference to the pattern structure of a mineral. A material in which atoms are fixed in an orderly pattern - a crystalline solid.
Turbidite
Crystal lattice
Elemental composition of Earth
Area of igneous activity
27. Volcanoes that exist as isolated points and appear to be independent of movement at a plate boundary - hot-spot volcanoes. Mostly are located on the interior of plates - away from boundaries.
Depositional environment
Polymorphs
Clastic
Hot spots
28. The shape of the sea floor surface. Investigation of the sea-floor revealed the presence of several important features: mid-ocean ridges - deep-ocean trenches - seamount chains - and fracture zones.
Bathymetry
Native metals
Fracture and cleavage
Melting
29. A rock made of solid mass of glass - or of tiny crystals surrounded by glass. Reflect light as glass does and tend to break conchoidally. Examples - obsidian - tachylite - pumice.
Organic chemicals
Glassy igneous rocks
Caliche
Fissure eruptions/lava plateaus
30. Mineral crystal formation type; form from a solution - meaning that atoms - molecules - or ions dissolved in water bond together out of water.
Solid-state diffusion
Phreatomagmatic eruptions
Precipitation
Polymorphs
31. 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
Hydrosphere
Salt wedging
Agrillaceous rocks
Spreading rate
32. 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.
Volcanic pipes/necks
Source rock composition
Turbidite
Rock texture
33. Sphere; Surface water along with groundwater - Earth consists of 70% surface water (oceans - lakes - and streams).
Stratagraphic formation
Hydrosphere
Pyroclastic flows
Subsidence
34. 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
Apparent polar-wander path
Topography
Depositional environment
Mantle
35. Distinct internal laminations within a ripple or dune that are inclined at an angle to the boundary of the main sedimentary layer. Form as a consequence of the evolution of dunes or ripples.
E-horizon
Cross beds
Clastic sedimentary rocks
Sedimentary Basins
36. Equant - meaning that they have the same dimensions in all directions. Or inequant - meaning their dimensions are not the same in all directions.
Cement
Strata
Sedimentary structure
Grain sizes
37. Alfred Wegener's suggestion that the positions of the continents change through time as they drift away from each other. The flaw was that he lacked a plausible moving mechanism.
Area of igneous activity
Siltstone and mudstone
Physical weathering
Continental drift hypothesis
38. 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
Hot-spot track
Fracture zones
Why magma rises
Apparent polar-wander path
39. 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.
Glassy igneous rocks
3.5km (2 miles)
Plutons
Basaltic composition
40. Sedimentary rock composed of calcite or dolomite.
Crystal
Carbonate rocks
Lithosphere
Turbidity current
41. A mafic rock with large grains. Intrusive - phaneritic igneous rock.
Dolostone
650-1100 degrees C
Gabbro
Magma mixing
42. Places with particularly voluminous quantities of magma erupting or intruding.
Large Igneous Provinces (LIPs)
Glassy igneous rocks
Conchoidal fractures
a'a'
43. Center of the Earth - consists mainly of iron alloy.
Evaporites
Paleopole
Volcanic pipes/necks
The core
44. Elongate submarine mountain ranges whose peaks lie only about 2-2.5km below sea level. Consist of a ridge axis - are roughly symmetrical - and can include escarpments - axial troughs - and valleys. Examples - Mid-Atlantic Ridge - East Pacific Rise -
Seamount chains
Metamorphic foliation
Mid-ocean ridges
Marine magnetic anomaly
45. 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.
Glass
Sulfates
Salt wedging
Crystal
46. By melting - dissolving - or other chemical reactions.
Transgression
triple junction
Mineral crystal destruction
Intrusive igneous rock
47. 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
Evaporites
Oxidation
Fractional crystallization
48. 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.
Mineral
Ignimbrite
Crust
Depositional environment
49. 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.
Volatiles
Clastic
Mafic
Quartz sandstone
50. Lava flow; associated with felsic magma - consists of ash and pumice fragments - material is propelled from the vent at a high speed.
Evaporites
Precipitation
Regolith
Pyroclastic flows