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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. Pea to plum-sized fragments of pyroclastic debris - consists of pumice or scoria fragments.
Reason for Earth's internal heat
Tephra
Lapilli
Crystalline
2. Core division; between 2900 and 5155km deep. Liquid iron alloy - it exists as a liquid because the temperature here is so high that even the great pressures squeezing the region cannot lock atoms into a solid framework. This liquid iron alloy is able
Oxides
Outer core
Soil erosion
rifting
3. Form when solid materials become hot and transform into liquid - example - molten rock.
Granitic magma
Ignimbrite
Melts
Phreatomagmatic eruptions
4. 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.
Color
Turbidity current
Grain sizes
Rock composition
5. The broad - relatively flat regions of the ocean that lie at a depth of about 4-5km below sea level.
Abyssal plains
Rocks
Continental shelf
Metamorphic rocks
6. Type of lava flow; surface layer of the lava freezes and then breaks up due to the continued movement of lava underneath - becomes a jumble of sharp - angular fragments - yielding a rubbly flow.
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7. Relatively small - elongated ridges that form on a bed surface at right angles to the direction of the current flow of the rock.
Fissure eruptions/lava plateaus
Andesitic lava flows
Ripples
Metamorphic foliation
8. 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
Lava
Crystal habit
collision
Strata
9. Mineral class; the fundamental component within these types of minerals in the Earth's crust is the silicon-oxygen tetrahedron anionic group - a silicon atom surrounded by four oxygen atoms that are arranged to define the corners of a tetrahedron - a
Sea-floor spreading
Igneous rocks
ravertine
Silicates
10. 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).
Clastic
Clastic sedimentary rocks
Crystal habit
Cementation
11. An envelope of gas surrounding Earth consisting of 78% nitrogen (N2) and 28% oxygen (O2) - with minor amounts 1% of argon - carbon dioxide - methane - etc. And 99% of the gas in the atmosphere lies below 50km.
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12. Sea-floor spreading proponents - Hess and others realized that in order for the circumference of the Earth to remain constant through time - ocean floor must eventually sink back into the mantle. This sinking process consumes the ocean floor between
Composite cone (stratovolcano)
Organic chemicals
Subduction
Relative plate velocity
13. Layering in metamorphic rocks.
Metamorphic foliation
Hardness
Turbidite
Factors of magma cooling time
14. Rocks whose crystals interlock with each other.
Andesitic lava flows
Crystalline
Columnar jointing
Apparent polar-wander path
15. Type of volcano; broad and slightly domed - primarily made of basaltic lava - large and erupt large volumes of lava. Form from either low viscosity basaltic lava or from large pyroclastic sheets.
Redbeds
Heat transfer
Shield volcano
Regression
16. 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
Lava domes
Soil Horizons
Magma mixing
Peridotite
17. Successive turbidity currents deposit successive graded beds - creating this sequence of strata.
Large Igneous Provinces (LIPs)
Turbidite
Luster
Granite
18. Distinguishing feature of magma; Because not all minerals melt by the same amount under given conditions - and because chemical reactions take place during melting - the magma that forms as a rock begins to melt does not have the same composition as
Magma's speed of flow
Partial melting
Compaction
Depositional environment
19. 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.
B-horizon
Intrusive igneous rock
Volatiles
Cross beds
20. Some minerals have distinctive properties - such as calcite which reacts with dilute hydrochloric acid to produce carbon dioxide. Dolomite also reacts with acid - graphite can make clear markings - magnetite attracts a magnet - halite tastes salty -
Special properties of minerals
Mineral crystal destruction
Tuff
Caliche
21. When different rocks in an outcrop undergo weathering at different rates.
Symmetry
triple junction
Differential weathering
Pangaea
22. Because different soil-forming processes operate at different depths - soils typically develop into these distinct zones. These zones can be arranged vertically into a soil profile.
Organic sedimentary rocks
Ignimbrite
Felsic - intermediate - mafic - ultramafic
Soil Horizons
23. 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.
Silicate minerals
Assimilation
Thermal expansion
Intrusive igneous rock
24. A submarine suspension of sediment.
Paleopole
Viscosity
Turbidity current
Lapilli
25. Process where new divergent boundaries form when a continent splits and separates into two continents.
Continental drift hypothesis
rifting
Biochemical sedimentary rocks
Flood basalts
26. 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.
Arkose
Oxides
Carbonates
Phreatomagmatic eruptions
27. 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.
Laccolith
Partial melting
C-horizon
Rock layering
28. 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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29. Mineral class; the anion within these types of minerals is a halogen ion (such as chlorine or fluorine).
Crust
Halides
rifting
Peridotite
30. Chemical weathering during Which minerals dissolve into water.
Fragmental igneous rocks
Fractional crystallization
Dissolution
Volcano
31. Type of volcanic eruption; pyroclastic - produce clouds and avalanches of pyroclastic debris. Gas expands in the rising magma - cannot escape. The pressure becomes so great that it blasts the lava - and volcanic rock - out of the volcano.
Ridge-push force
Differential weathering
Lava
Explosive eruptions
32. Natural cracks that form in rocks due to removal of overburden or due to cooling.
Crystalline igneous rocks
Euhedral crystal
Felsic - intermediate - mafic - ultramafic
Jointing
33. Most common mineral on Earth; compose over 95% of the continental crust. Consist of combinations of a fundamental building block called silicon-oxygen tetrahedron - different groups: independent tetrahedra - single chains - double chains - sheet sili
Silicate minerals
Dunes
Cinder cone
Zone of leaching
34. 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.
The effect of the environment on eruptive style
Color
O-horizon
Crystalline igneous rocks
35. Forms from a chemical reaction between solid calcite and magnesium-bearing groundwater.
O-horizon
Chemical weathering
Felsic - intermediate - mafic - ultramafic
Dolostone
36. 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.
Glass
Flood basalts
Organic chemicals
The effect of viscosity on eruptive style
37. 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
Salt wedging
Mantle plume
Ridge-push force
Turbidite
38. The absorption of water into the crystal structure of minerals - causes some minerals to expand.
Hydration
Biomineralization
Pangaea
Hardness
39. Sedimentary rocks consisting of carbon-rich relicts of plants.
Gem
Gabbro
Organic sedimentary rocks
Sedimentary structure
40. Form from grains that break off preexisting rock and become cemented together - or from minerals that precipitate out of a water solution.
Sedimentary rocks
Carbonate rocks
Oxidation
ravertine
41. 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
Continental drift hypothesis
Mafic
Fractional crystallization
The effect of viscosity on eruptive style
42. Occurs within the asthenosphere - actively drags plates along and attributes partially for the mechanism shifting the plates along the Earth's surface.
Convective flow
Basaltic composition
Effusive eruptions
Mineral crystal destruction
43. Coarse pyroclastic debris - apple to refrigerator-sized fragments. Chunks of preexisting igneous rock or large lava blobs which discharge from volcanic eruptions.
Volcanic blocks/bombs
Relative plate velocity
The effect of the environment on eruptive style
Dark Silicates
44. Solids composed of metal atoms (such as iron - aluminum - copper - and tin). Within this type of solid - outer electrons are able to flow freely.
Metals
Rocks
Soil
Laccolith
45. 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.
Pyroclastic debris
Composite cone (stratovolcano)
Dissolution
Dipole
46. Equant - meaning that they have the same dimensions in all directions. Or inequant - meaning their dimensions are not the same in all directions.
Outcrop
Slab-pull force
Facets
Grain sizes
47. A reference to the supposed position of the Earth's magnetic pole at a time in the past.
Gabbro
Oxides
Paleopole
Frost wedging
48. Rigid outer layer of Earth - 100-150km thick. Consists of the crust plus the uppermost part of the mantle.
Graded bed
Lithosphere
Regolith
collision
49. Sedimentary rocks made up of minerals that precipitate directly from water solutions.
Chemical sedimentary rocks
Volcanic pipes/necks
Deposition
Paleopole
50. Sedimentary rocks made up of the shells of organisms.
C-horizon
ravertine
Biochemical sedimentary rocks
Salt wedging