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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. Chemical weathering occurring in warm - wet climates can produce a layer of rotten rock - over 100km thick.
Superplumes
Convergent plate boundary
Laterite
Saprolite
2. A fine spray of lava instantly freezes to form fine particles of glass.
Ash
Transition zone
Turbidite
Marine magnetic anomaly
3. Hot basaltic lava that erupts with such low viscosity that it can flow tens to hundreds of kilometers across the landscape.
Paleopole
Abyssal plains
Intermediate
Flood basalts
4. A name for any kind of unconsolidated debris that covers bedrock. Includes both soil and accumulations of sediment that have not evolved into soil.
Silicates
Residual soil
Regolith
Peridotite
5. 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
Continental rift
Salt wedging
3.5km (2 miles)
Basaltic composition
6. A mafic rock with large grains. Intrusive - phaneritic igneous rock.
Saprolite
Gabbro
Flood basalts
12km
7. On a gem are the ground and polished surfaces made with a certain type of machine.
Composite cone (stratovolcano)
Magnetic reversals
Chemical sedimentary rocks
Facets
8. 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
Weathering
The effect of the environment on eruptive style
E-horizon
Evaporites
9. When different rocks in an outcrop undergo weathering at different rates.
Dolostone
Deposition
Color
Differential weathering
10. The removal of soil by running water or by wind.
Paleopole
Soil erosion
Hardness
Pyroclastic debris
11. Four settings: in volcanic arcs bordering deep-ocean trenches - isolated hot spots - within continental rifts - and along mid-ocean ridges.
Slab-pull force
Glass
Apparent polar-wander path
Area of igneous activity
12. Physical property of a mineral; refers to the color of a powder produced by pulverizing the mineral. Provides a fairly reliable clue to the mineral's identity - since the color of the mineral powder tends to be less variable than the color of the who
Streak
Granitic composition
Euhedral crystal
Pyroclastic debris
13. Mineral group; feldspars - quartz - muscovite - clay minerals.
Light silicates
Siltstone and mudstone
Ridge-push force
Granite
14. Mineral crystal formation type; form from a solidification of a melt - meaning the freezing of a liquid.
Volatiles
Igneous rocks
Melting
Biochemical sedimentary rocks
15. Type of magma; low in silica - fluid - crystallize at high temperatures.
Volcanic blocks/bombs
Volatiles
Conchoidal fractures
Basaltic magma
16. Low-viscosity (basaltic) lava flows out of a volcano easily - whereas high-viscosity (andesitic and rhyolitic) lava can clog and build pressure within a volcano. Basaltic eruptions are typically effusive and produce shield volcanoes - whereas rhyolit
The effect of viscosity on eruptive style
collision
Oxidation
Graded bed
17. The transformation of loose sediment into solid rock.
A-horizon
Ridge-push force
Fracture and cleavage
Lithification
18. Equant - meaning that they have the same dimensions in all directions. Or inequant - meaning their dimensions are not the same in all directions.
Turbidite
Limestone
Grain sizes
Upper mantle
19. In degrees Celsius - the high temperatures at which igneous rocks freeze; the freezing of liquid melt to form solid igneous rock represents the same phenomenon as the freezing of water - except at much higher temperatures.
Lithification
Hydrosphere
Basaltic magma
650-1100 degrees C
20. 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.
Biomineralization
Fractional crystallization
Compaction
Stoping
21. 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.
Loam
Volcano
Plutons
Granite
22. Places with particularly voluminous quantities of magma erupting or intruding.
Large Igneous Provinces (LIPs)
Mantle plume
Luster
Hot-spot track
23. 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.
Dike
Sulfides
Lava tube
Source rock composition
24. 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.
Evaporites
Continental drift hypothesis
Limestone
650-1100 degrees C
25. A column of very hot rock that flows upward until it reaches the base of the lithosphere. In this model - such deep-mantle plumes form because heat rising from the Earth's core is warming rock at the base of the mantle. A possible explanation to the
Why magma rises
Mantle plume
Stratagraphic formation
Composite cone (stratovolcano)
26. Form from grains that break off preexisting rock and become cemented together - or from minerals that precipitate out of a water solution.
Cement
Why magma rises
Sedimentary rocks
Felsic
27. 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
Redbeds
Inner core
Agrillaceous rocks
Assimilation
28. A type of carbonate rock; rocks formed from the calcite or aragonite skeletons of organisms form this biochemical sedimentary rock.
Rock texture
O-horizon
Organic sedimentary rocks
Limestone
29. 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.
Effusive eruptions
Zone of leaching
Five steps of clastic sedimentary rock formation
Facets
30. When water is trapped in a joint freezes - it forces the joint open and may cause the joint to grow.
Hot spots
Frost wedging
Area of igneous activity
Facets
31. 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.
Glassy igneous rocks
Streak
Chemical sedimentary rocks
Polymorphs
32. During the final stages of cooling - lava flows contract and may fracture into roughly hexagonal columns.
Transported soil
Columnar jointing
Mafic
Basalt
33. Mineral crystal formation type; form at interfaces between the physical and biological components of the Earth system by this process.
Sandstone
Biomineralization
Convective flow
Basaltic magma
34. Type of soil; forms from sediment that has been carried in from elsewhere. Include those formed from deposits left by rivers - glaciers - or wind.
Glass
Transported soil
Lava
Sulfides
35. 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.
Organic sedimentary rocks
Diagenesis
Sedimentary rocks
Siliceous rocks
36. Theory confirmed by 1968 - geologists had developed the complete model of continental drift - sea-floor spreading - and subduction. Within this model - Earth's lithosphere consists of about 20 distinct pieces - or plates - that move relative to each
Earth's atmosphere
Plate tectonics
Deep-ocean trenches
Mid-ocean ridges
37. 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
Dunes
Magnetic anomaly
Melting
Divergent plate boundary
38. Refers to the proportions of different chemicals making up the rock - and thus the proportion chemicals affects the proportions of different minerals constituting the rock.
Hot-spot track
Magnetic inclination
Dunes
Rock composition
39. Built up deposit of volcanic bombs and lapilli - known as volcanic agglomerate.
Why magma rises
Stoping
Tuff
Volatiles
40. Chemical precipitates; salt deposits formed as a consequence of evaporation. Examples - rock salt and gypsum.
Andesitic lava flows
Biomineralization
Extrusive igneous rock
Evaporites
41. Biochemical sedimentary rock; it's made from cryptocrystalline quartz. Examples - flint and jasper.
Continental drift hypothesis
Organic chemicals
Chert
Five steps of clastic sedimentary rock formation
42. Farther down from a zone of leaching - new mineral crystals precipitate directly out of the water or form when the water reacts with debris - this the region where the new minerals and clay collect.
Andesitic lava flows
Silicates
Mafic
Zone of accumulation
43. Weathering - erosion - transportation - deposition - and lithification.
Rock layering
Jointing
Oxidation
Five steps of clastic sedimentary rock formation
44. 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
Biomineralization
Biochemical sedimentary rocks
Native metals
Dipole
45. Mineral class; consist of pure masses of a single metal - with metallic bonds. Copper and gold can appear in this way.
Bed
Native metals
Calderas
Saprolite
46. Two different minerals which have the same composition but have different crystal structures.
Polymorphs
Elemental composition of Earth
Dike
Saprolite
47. Places where intrusive igneous rock creates tabular intrusions cutting across rock that does not have layering - this nearly vertical - wall-like tabular intrusions is formed. Cut across layering within the earth.
Siltstone and mudstone
Ripples
Dike
Decompression
48. A thick accumulation of sediment (10-15km) - the surface of this sediment layer is this broad - shallow region.
Fracture zones
Special properties of minerals
Continental shelf
Paleopole
49. Highest soil horizon; consists almost entirely of organic matter and contains barely any mineral matter. Surface level has 'litter' and deeper it contains 'humus'. Part of the zone of leaching.
Paleomagnetism
O-horizon
Flood basalts
Lava domes
50. Sedimentary rock composed of calcite or dolomite.
Melts
Euhedral crystal
Carbonate rocks
Pyroclastic flows