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Test your basic knowledge |
Geology
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Subject
:
science
Instructions:
Answer 50 questions in 15 minutes.
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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. Occurs within the asthenosphere - actively drags plates along and attributes partially for the mechanism shifting the plates along the Earth's surface.
Hot spots
Convective flow
Why magma rises
Ultramafic
2. Type of sedimentary soil/rock; Calcite in a pedocal soil accumulates in the B-horizon and may cement soil together - creating this solid mass.
Five steps of clastic sedimentary rock formation
Native metals
Caliche
Agrillaceous rocks
3. Pea to plum-sized fragments of pyroclastic debris - consists of pumice or scoria fragments.
Rock texture
Factors classifying clastic sedimentary rocks
Decompression
Lapilli
4. Chemical weathering occurring in warm - wet climates can produce a layer of rotten rock - over 100km thick.
Color
Grain sizes
Saprolite
Sulfates
5. 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.
Organic chemicals
Dike
Clastic sedimentary rocks
Mantle plume
6. 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
Chert
atmospheres (atm)
Viscosity
Silicates
7. Four settings: in volcanic arcs bordering deep-ocean trenches - isolated hot spots - within continental rifts - and along mid-ocean ridges.
12km
Area of igneous activity
Specific gravity
Lava tube
8. 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.
Basaltic composition
Five steps of clastic sedimentary rock formation
Sulfides
Fractional crystallization
9. A layer of sediment in which grain size varies from coarse at the bottom to fine at the top.
Geothermal gradient
Dunes
Graded bed
Subsidence
10. Develops because mid-ocean ridges lie at a higher elevation than the adjacent abyssal plains of the ocean. The surface of the sea floor overall slopes away from the ridge axis. Gravity causes the elevated lithosphere at the ridge axis to push on the
Ridge-push force
Sea-floor spreading
Stratagraphic formation
Evaporites
11. A fine spray of lava instantly freezes to form fine particles of glass.
Ash
Depositional environment
Magma mixing
Divergent plate boundary
12. The resistance to flow of magma. Reflects its distinct silica content - for silica tends to polymerize - meaning it links up to form long - chainlike molecules whose presence slows down the flowing ability of magma. Thus felsic magmas flow less easil
Carbonate rocks
Viscosity
ravertine
Lapilli
13. 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.
Factors of magma cooling time
Conglomerate
C-horizon
Volcanic pipes/necks
14. The most important mineral group; comprise the most rock-forming minerals - they are very abundant due to large % of silicon and oxygen in Earth's crust. Examples - oxygen - silica - aluminum.
Halides
Rock-forming silicate minerals
Bedrock
Polymorphs
15. Mineral crystal formation type; form by type of diffusion - the movement of atoms or ions through a solid to arrange into a new crystal structure; process takes place very slowly.
Spreading rate
Solid-state diffusion
Bedding
Magma
16. A vent at Which melt from inside the Earth spews onto the planet's surface. Erupt.
Redbeds
Volcano
Rock composition
Intrusive igneous rock
17. 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.
Metamorphic rocks
Bedding
Magnetic inclination
Convective flow
18. The transformation of loose sediment into solid rock.
Dike
Biomineralization
Lithification
Saprolite
19. 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.
Upper mantle
Salt wedging
Phreatomagmatic eruptions
Magnetic inclination
20. 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
Dipole
Cinder cone
Subsidence
Deposition
21. A reference to the pattern structure of a mineral. A material in which atoms are fixed in an orderly pattern - a crystalline solid.
Subsidence
Granitic magma
Ridge-push force
Crystal lattice
22. 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.
Extrusive igneous rock
Sedimentary structure
A-horizon
Pyroclastic debris
23. A felsic rock with large grains. Intrusive - phaneritic igneous rock.
Granite
Extrusive igneous rock
Assimilation
Spreading rate
24. 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.
Turbidite
Intrusive igneous rock
O-horizon
Calderas
25. Chemical precipitates; salt deposits formed as a consequence of evaporation. Examples - rock salt and gypsum.
Clastic sedimentary rocks
Evaporites
Euhedral crystal
Magma's speed of flow
26. Actively slipping segment of a fracture zone between two ocean ridge segments - these faults make a third type of plate boundary - transforms.
Mid-ocean ridges
Mineral
Transform fault
Sea-floor spreading
27. Sedimentary rock composed of calcite or dolomite.
Carbonate rocks
Rhyolitic lava flows
Transform fault
Hydrosphere
28. 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.
Superplumes
Silicate minerals
Phreatomagmatic eruptions
Mantle
29. 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
Magma mixing
Polymorphs
Rhyolitic lava flows
Bedrock
30. When silt and clay accumulate in the flat areas bordering a stream - lagoon - or delta - the silt when lithified becomes this type of sediment. And the mud - when lithified - becomes another type of sediment - also known as shale.
Siltstone and mudstone
Sedimentary structure
E-horizon
Assimilation
31. Rocks that forms by the freezing of lava above ground - after it spills out (extrudes) onto the surface of the Earth and comes into contact with the atmosphere or ocean.
Graded bed
Extrusive igneous rock
Pyroclastic flows
Lithification
32. Type of lava flow; mafic - low viscosity - extremely hot - flows very quickly.
Oxidation
Basaltic lava flows
Superplumes
The effect of the environment on eruptive style
33. Magma type; contains about 45% to 52% silica. Named because it produces rock containing abundant mafic minerals - magnesium and iron combinations.
Dipole
collision
Salt wedging
Mafic
34. Subsoil - ions and clay leached and transported down from above accumulate here. As a result - new minerals form - and clay fills open spaces. Part of the zone of accumulation.
Hydration
B-horizon
Crystal habit
Intermediate
35. By melting - dissolving - or other chemical reactions.
Crystal
Quartz sandstone
Transform fault
Mineral crystal destruction
36. 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
Magnetic inclination
collision
Xenolith
Subduction
37. A mafic rock with small grains. Extrusive - aphanitic igneous rock.
Clastic
Alloy
Basalt
Soil Horizons
38. 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
Salt wedging
Turbidity current
Viscosity
Crystalline
39. A plate boundary at which two plates move apart from one another by process of sea-floor spreading. Mid-ocean ridges or simply a ridge. New crust is formed at ridges through the buoyant rising of magma from beneath the surface and solidifies to creat
Volcanic pipes/necks
Divergent plate boundary
Graded bed
Mafic
40. Form when solid materials become hot and transform into liquid - example - molten rock.
Continental drift hypothesis
Sedimentary Basins
Melts
The effect of gas pressure on eruptive style
41. Lava flow; associated with felsic magma - consists of ash and pumice fragments - material is propelled from the vent at a high speed.
Crystal habit
Pyroclastic flows
Biochemical sedimentary rocks
Limestone
42. A mixture containing more than one type of metal atom. Example - bronze is a mixture of copper and tin.
Phreatomagmatic eruptions
Extrusive igneous rock
Outer core
Alloy
43. Active hot-spot volcanoes commonly occur at the end of a chain of dead volcanoes.
Hot-spot track
Frost wedging
Cementation
Arkose
44. Inorganic limestone; rock composed of crystalline calcium carbonate formed by chemical precipitation.
Mineral
ravertine
Alloy
12km
45. 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
Lithification
Superplumes
Plate tectonics
Volcanic blocks/bombs
46. Sedimentary rocks made up of minerals that precipitate directly from water solutions.
Chemical sedimentary rocks
Special properties of minerals
The core
Metamorphic rocks
47. Irregular or blob-shaped intrusions that range in size from tens of meters across to tens of kilometers across.
Basaltic magma
Fracture zones
Polymorphs
Plutons
48. Rock made by the freezing of magma underground - after it has pushed its way (intruded) into preexisting rock of the crust.
Intrusive igneous rock
Siliceous rocks
Ridge-push force
Jointing
49. Similar to ripples - but are much larger. Small ripples often form on the surface of these structures.
12km
Lava domes
Dunes
Dark Silicates
50. 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
Magnetic reversals
Rock layering
Stoping
Turbidite
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