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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. 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
Bathymetry
Cross beds
Silicate minerals
Divergent plate boundary
2. Actively slipping segment of a fracture zone between two ocean ridge segments - these faults make a third type of plate boundary - transforms.
Chemical sedimentary rocks
Transition zone
Transform fault
Granitic magma
3. 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
Heat transfer
A-horizon
650-1100 degrees C
4. Fluid basaltic lava extruded from crustal fractures called fissures.
Tephra
Fissure eruptions/lava plateaus
Assimilation
Salt wedging
5. 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
Crystal lattice
E-horizon
Caliche
Siltstone and mudstone
6. Magma viscosity depends upon temperature - volatile content - and silica content. Hotter magma - more volatiles - and mafic magma all have less viscosity.
7. The ocean floor is diced up by narrow bands of vertical fractures. Lie roughly at right angles to mid-ocean ridges - effectively segmenting the ridges into small pieces.
Fracture zones
Basaltic composition
Andesitic lava flows
Clastic
8. Sublayer of the mantle - depth of 660km.
Bedding
Upper mantle
Paleomagnetism
Abyssal plains
9. A process occurring when sea level falls - the coast migrates seaward.
Crystal
Continental drift hypothesis
Intrusive igneous rock
Regression
10. Chemical weathering during Which minerals dissolve into water.
Granite
Diagenesis
Native metals
Dissolution
11. Physical features of the land surface represented by changes in elevation.
Five steps of clastic sedimentary rock formation
Plate tectonics
Sea-floor spreading
Topography
12. 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
Mantle plume
Facets
Plate tectonics
Five steps of clastic sedimentary rock formation
13. The Earth radiated heat into space and slowly cooled. Eventually - the early formed sea of lava solidified and formed igneous rock. The cumulative effect of radioactivity has been sufficient to slow the cooling of the planet and subsequently allow fo
14. A single - continuous (uninterrupted) piece of a crystalline solid bounded by flat surfaces called crystal faces that grew naturally as the mineral formed. Come in a variety of shapes - cubes - trapezoids - pyramids - octahedrons - hexagonal columns
Andesitic lava flows
Deposition
Crystal
Hot spots
15. 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
Partial melting
Mantle
Flood basalts
Felsic
16. The four classes of igneous silicate rocks based on the proportion of silicon to iron and magnesium. As the proportion of silicon in a rock increases - the density decreases - thus felsic rocks are less dense than mafic. In order - from greatest to l
Organic chemicals
ravertine
Felsic - intermediate - mafic - ultramafic
Andesitic lava flows
17. 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
Turbidite
Convergent plate boundary
Extrusive igneous rock
Dike
18. Cause of melting; the variation in temperature with depth is expressed in the geotherm; because pressure prevents melting - a decrease in pressure can permit melting. Specifically - if the pressure affecting hot mantle rock decreases while the temper
Hydrosphere
3.5km (2 miles)
Decompression
Frost wedging
19. An organic sedimentary rock; black - combustible rock consisting of over 50% carbon.
Mafic
Cinder cone
Coal
B-horizon
20. A felsic rock with large grains. Intrusive - phaneritic igneous rock.
Granite
triple junction
Conchoidal fractures
Convergent plate boundary
21. Coarse pyroclastic debris - apple to refrigerator-sized fragments. Chunks of preexisting igneous rock or large lava blobs which discharge from volcanic eruptions.
Root wedging
Apparent polar-wander path
Hydrolysis
Volcanic blocks/bombs
22. The base of the soil profile; consists of material derived from the substrate that's been chemically weathered and broken apart - but has not yet undergone leaching or accumulation.
Cross beds
Arkose
Solid-state diffusion
C-horizon
23. A name for any kind of unconsolidated debris that covers bedrock. Includes both soil and accumulations of sediment that have not evolved into soil.
a'a'
Regolith
Luster
Clastic
24. Mineral crystal formation type; form from a solution - meaning that atoms - molecules - or ions dissolved in water bond together out of water.
Convective flow
Precipitation
Subsidence
Graded bed
25. A sedimentary bed that has developed a reddish color. The red comes from a film of iron oxide (hematite) that forms on grain surfaces.
Melting
Agrillaceous rocks
Dolostone
Redbeds
26. Type of rock; accumulated sand bars - within are mineral grains of quartz and feldspar - this sediment if buried and lithified.
Continental shelf
Arkose
Soil Horizons
Decompression
27. Occurs within the asthenosphere - actively drags plates along and attributes partially for the mechanism shifting the plates along the Earth's surface.
Volcano
Native metals
Solid-state diffusion
Convective flow
28. 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.
Metamorphic rocks
Special properties of minerals
Alloy
Oxides
29. Perhaps the cause for the large igneous provinces; formations within the mantle - plumes that bring up vastly more hot asthenosphere than normal plumes.
Dolostone
Crystalline igneous rocks
Superplumes
Sea-floor spreading
30. The burial and lithification of angular or rounded clasts form these types of rocks.
Divergent plate boundary
Conglomerate
Weathering
Asthenosphere
31. Mineral crystal formation type; form from a solidification of a melt - meaning the freezing of a liquid.
Physical weathering
Glassy igneous rocks
Melting
The core
32. An insulated - tunnel-like conduit through which lava moves within a flow.
Basaltic magma
Color
Rock texture
Lava tube
33. 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.
34. Sedimentary rocks made up of the shells of organisms.
Turbidity current
Biochemical sedimentary rocks
Frost wedging
Reason for Earth's internal heat
35. 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 -
Effusive eruptions
Special properties of minerals
atmospheres (atm)
Phreatomagmatic eruptions
36. Carbon-containing compounds that either occur in living organisms - or have characteristics that resemble the molecules within living organisms. Examples - oil - protein - plastic - fat - and rubber.
Rock texture
Subsidence
Ridge-push force
Organic chemicals
37. A mafic rock with large grains. Intrusive - phaneritic igneous rock.
Gabbro
Clastic sedimentary rocks
The effect of gas pressure on eruptive style
Tephra
38. Rock made by the freezing of magma underground - after it has pushed its way (intruded) into preexisting rock of the crust.
Divergent plate boundary
Sulfates
Intrusive igneous rock
Soil erosion
39. Chemical weathering occurring in warm - wet climates can produce a layer of rotten rock - over 100km thick.
Lithification
Batholiths
Factors classifying clastic sedimentary rocks
Saprolite
40. An intrusion starting to inject between layers but then dome upwards - creating this blister-shaped intrusion.
Solid-state diffusion
Laccolith
Ignimbrite
O-horizon
41. 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
Lapilli
Mantle
Dipole
Precipitation
42. Clast size - clast composition - angularity and sphericity - sorting - and character of cement.
Chemical sedimentary rocks
Factors classifying clastic sedimentary rocks
Conglomerate
Diagenesis
43. Physical property of a mineral; different minerals fracture in different ways - depending on the internal arrangement of atoms. If a mineral breaks to form distinct planar surfaces that have a specific orientation in relation to the crystal structure
Dissolution
Chemical sedimentary rocks
Fracture and cleavage
Magma mixing
44. Layering in metamorphic rocks.
The effect of the environment on eruptive style
Metamorphic foliation
Ignimbrite
Crystal
45. A layer of sediment in which grain size varies from coarse at the bottom to fine at the top.
Graded bed
Saprolite
Crystalline igneous rocks
Continental drift hypothesis
46. Cause of melting; when magma rises up from the mantle into the crust - it brings heat with it which raises the temperature of the surrounding crustal rock - and in some cases melting occurs.
a'a'
Frost wedging
Heat transfer
Oxides
47. The display of the pattern of atoms or ions within a mineral. Meaning that the shape of one part of a mineral is a mirror image of the shape of another part.
Magnetic anomaly
Residual soil
Loam
Symmetry
48. Forms when clots of lava fly into the air in lava fountains and then freeze to form solid chunks before hitting the ground. Some forms when the explosion of a volcano shatters preexisting rock and ejects the fragments over the countryside.
Sandstone
Sulfates
Decompression
Pyroclastic debris
49. Measure of pressure or push in units of force - per unit area. 1 atm = 1.04 kilograms per square centimeter.
Marine magnetic anomaly
atmospheres (atm)
Shield volcano
Intermediate
50. 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
Transported soil
Tephra
Basaltic magma
collision