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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. 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.
Lava
Spreading rate
Phreatomagmatic eruptions
Crystal
2. Biochemical sedimentary rock; it's made from cryptocrystalline quartz. Examples - flint and jasper.
Transported soil
Area of igneous activity
Lower mantle
Chert
3. An organic sedimentary rock; black - combustible rock consisting of over 50% carbon.
Coal
Flood basalts
Metals
Granitic magma
4. 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
Compaction
Sulfates
Large Igneous Provinces (LIPs)
5. A mixture containing more than one type of metal atom. Example - bronze is a mixture of copper and tin.
Glass
Strata
Alloy
Basaltic lava flows
6. The absorption of water into the crystal structure of minerals - causes some minerals to expand.
Rock layering
Cinder cone
Continental rift
Hydration
7. If a stoped block does not melt entirely - but rather becomes surrounded by new igneous rock - it becomes this; xeno - meaning foreign.
Xenolith
Basaltic lava flows
Deposition
Dipole
8. Type of soil; forms from sediment that has been carried in from elsewhere. Include those formed from deposits left by rivers - glaciers - or wind.
Conglomerate
Continental rift
Transported soil
Clastic sedimentary rocks
9. Chemical precipitates; salt deposits formed as a consequence of evaporation. Examples - rock salt and gypsum.
Chemical sedimentary rocks
Siliceous rocks
atmospheres (atm)
Evaporites
10. Physical property of a mineral; refers to the way a mineral surface scatters light. Metallic versus non-metallic in nature.
Magma
Luster
Bed
Plate tectonics
11. 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
Slab-pull force
Tephra
Gem
Depositional environment
12. Magma viscosity depends upon temperature - volatile content - and silica content. Hotter magma - more volatiles - and mafic magma all have less viscosity.
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13. Relatively small - elongated ridges that form on a bed surface at right angles to the direction of the current flow of the rock.
Plate tectonics
Felsic - intermediate - mafic - ultramafic
Ripples
Granite
14. Type of volcano; most are adjacent to the Pacific - larger in size - interbedded lavas and pyroclastics - consist of alternating layers of lava and tephra - most violent type of activity - may produce nuee ardente or lahars.
Composite cone (stratovolcano)
Crystal lattice
Transform fault
The core
15. A reference to the supposed position of the Earth's magnetic pole at a time in the past.
Melts
Carbonate rocks
Five steps of clastic sedimentary rock formation
Paleopole
16. Volcanic landform; steep walled depression at the summit - size exceeds one kilometer in diameter.
Calderas
Turbidite
Relative plate velocity
Ridge-push force
17. Heat from an intense surface fire bakes and expands the outer layer of the rock. On cooling - the layer contracts - causing the outer part of the rock spall - or break off in sheet-like pieces.
Luster
Mid-ocean ridges
Native metals
Thermal expansion
18. A mineral's growth that is uninhibited - has well-formed crystal faces.
Euhedral crystal
Hot spots
Rock texture
Upper mantle
19. The burial and lithification of angular or rounded clasts form these types of rocks.
Lava tube
Plate tectonics
Magnetic anomaly
Conglomerate
20. 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.
Cinder cone
Bedding
Symmetry
a'a'
21. 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.
Basaltic composition
O-horizon
Source rock composition
Paleomagnetism
22. 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.
Residual soil
rifting
Cinder cone
Paleomagnetism
23. A process occurring when sea level falls - the coast migrates seaward.
Regression
Tephra
Silicate minerals
Clastic sedimentary rocks
24. A reference to the sinking of the lithosphere; allows for sediment to accumulate in regions where this occurs.
Stoping
Why magma rises
Subsidence
Continental shelf
25. Type of lava flow; higher silica content - greater viscosity - forms a large mound above the vent out of a volcano.
Carbonate rocks
Andesitic lava flows
Specific gravity
Soil
26. 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
Ignimbrite
Specific gravity
Metals
27. Inorganic limestone; rock composed of crystalline calcium carbonate formed by chemical precipitation.
Root wedging
Xenolith
Andesitic lava flows
ravertine
28. 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
Rock composition
The effect of gas pressure on eruptive style
Crystal lattice
Lithosphere
29. Layering in metamorphic rocks.
Glassy igneous rocks
Metamorphic foliation
Rock-forming silicate minerals
Spreading rate
30. A pluton formation theory; a process during Which magma assimilates wall rock - and blocks of wall rock break off and sink into the magma.
Spreading rate
Divergent plate boundary
Stoping
Diagenesis
31. A fine spray of lava instantly freezes to form fine particles of glass.
Ash
Bedrock
Agrillaceous rocks
Gabbro
32. Hot basaltic lava that erupts with such low viscosity that it can flow tens to hundreds of kilometers across the landscape.
Pangaea
Facets
Flood basalts
Subduction
33. Type of sedimentary rock; rocks whose grains are stuck together by cement.
Granitic composition
Clastic
Chemical weathering
Silicates
34. A layer of sediment in which grain size varies from coarse at the bottom to fine at the top.
Volatiles
Plates
Graded bed
Oxides
35. The rate of increase in temperature - decreases with increasing depth. The dashed lines represent the solidus and liquidus for mantle rock (peridotite). The solidus line defines the conditions of pressure and temperature at Which mantle rock begins t
Magnetic declination
Geothermal gradient
Calderas
Stoping
36. Lava flow; associated with felsic magma - consists of ash and pumice fragments - material is propelled from the vent at a high speed.
atmospheres (atm)
Turbidite
Crystal habit
Pyroclastic flows
37. Rigid outer layer of Earth - 100-150km thick. Consists of the crust plus the uppermost part of the mantle.
Hot-spot track
Lithosphere
Metals
Carbonate rocks
38. Two different minerals which have the same composition but have different crystal structures.
The effect of viscosity on eruptive style
Crystalline
Polymorphs
Chemical sedimentary rocks
39. 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
Soil Horizons
Soil
Polymorphs
Streak
40. Type of sedimentary soil/rock; Calcite in a pedocal soil accumulates in the B-horizon and may cement soil together - creating this solid mass.
Intrusive igneous rock
Dissolution
Hydrolysis
Caliche
41. 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.
Sill
Mafic
Magnetic declination
Shield volcano
42. The fit of the continents - locations of past glaciations - the distribution of equatorial climatic belts - the distribution of fossils - and matching geologic units.
Batholiths
Granite
Bedrock
Continental drift evidence
43. 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.
Sill
Factors classifying clastic sedimentary rocks
Mantle
Intrusive igneous rock
44. 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
Effusive eruptions
Why magma rises
Alloy
Hardness
45. Distinguishing feature of magma; the composition of the melt reflects the composition of the solid from which it was derived. Not all magmas form from the same source rock - therefore not all magmas have the same compositions.
Source rock composition
Frost wedging
Upper mantle
Bed
46. The conditions in which sediment was deposited. Examples - beach - glacial - and/or river environments.
Strata
Fracture zones
Residual soil
Depositional environment
47. When different rocks in an outcrop undergo weathering at different rates.
Regression
Erosion
Assimilation
Differential weathering
48. An exposure of bedrock.
Gabbro
Five steps of clastic sedimentary rock formation
Outcrop
Lithification
49. The boundary between two beds is a bedding plane; several beds constitute this structure.
Fractional crystallization
Rhyolitic lava flows
Strata
Bedding
50. Clast size - clast composition - angularity and sphericity - sorting - and character of cement.
Factors classifying clastic sedimentary rocks
Dolostone
Rhyolitic lava flows
Caliche