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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. 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
Compaction
E-horizon
Chemical weathering
Clastic sedimentary rocks
2. 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
Decompression
Xenolith
The effect of gas pressure on eruptive style
Granite
3. Places with particularly voluminous quantities of magma erupting or intruding.
Large Igneous Provinces (LIPs)
Sea-floor spreading
Superplumes
Columnar jointing
4. Magma type; contains about 45% to 52% silica. Named because it produces rock containing abundant mafic minerals - magnesium and iron combinations.
Mafic
Agrillaceous rocks
Transform plate boundary
Depositional environment
5. Elongate submarine mountain ranges whose peaks lie only about 2-2.5km below sea level. Consist of a ridge axis - are roughly symmetrical - and can include escarpments - axial troughs - and valleys. Examples - Mid-Atlantic Ridge - East Pacific Rise -
Mid-ocean ridges
Mineral crystal destruction
Slab-pull force
Sea-floor spreading
6. 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
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7. Refers to the arrangement of grains in a rock; that is - the way the grains connect each other and whether inequant grains are aligned parallel to one another.
Hydrolysis
Rock texture
Cross beds
Area of igneous activity
8. Lava flow; associated with felsic magma - consists of ash and pumice fragments - material is propelled from the vent at a high speed.
Conglomerate
Pyroclastic flows
Basaltic magma
Streak
9. 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
Conglomerate
Subduction
Magma mixing
Turbidity current
10. Type of volcanic eruption; produce mainly lava flows - yield low-viscosity basaltic lavas.
Dolostone
Redbeds
Effusive eruptions
Fracture zones
11. The boundary between two beds is a bedding plane; several beds constitute this structure.
B-horizon
Strata
Diagenesis
Lapilli
12. Rocks that consist of mineral crystals that intergrow when the melt solidifies - interlocking structure. Examples - granite and rhyolite.
Oxides
Alloy
Crystalline igneous rocks
Mafic
13. Mineral group; feldspars - quartz - muscovite - clay minerals.
Metals
Mineral
Light silicates
Salt wedging
14. Consists of rock and sediment that has been modified by physical and chemical interaction with organic material and rainwater - over time - to produce a substrate that can support the growth of plants.
Soil
Halides
Fracture zones
Volcanic blocks/bombs
15. 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).
Assimilation
Cementation
Grain sizes
Factors classifying clastic sedimentary rocks
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
C-horizon
Euhedral crystal
Apparent polar-wander path
17. 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.
Volatiles
Oxides
Rhyolitic lava flows
Compaction
18. Volcanic landform; bulbous mass of congealed lava - associated with explosive eruptions of gas-rich magma.
Native metals
Lava domes
Depositional environment
Cross beds
19. 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.
Solid-state diffusion
Crystal
Siltstone and mudstone
Basaltic magma
20. 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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21. Tree roots that grow into joints can push those joints open in this process.
Sedimentary rocks
Pyroclastic debris
Root wedging
Paleomagnetism
22. Factors; the depth of the intrusion - the deeper - the more slowly it cools. The shape and size of a magma body - the greater the surface area - the faster it cools. The presence of circulating groundwater - water passing through cools magma faster.
Factors of magma cooling time
12km
Divergent plate boundary
Rocks
23. Outer surface level of Earth; composed of granite - basalt - and gabbro. Continental: mostly about 35-40km thick . Oceanic: about 7-10km thick. Oxygen - by far the most abundant element.
Dissolution
Ultramafic
E-horizon
Crust
24. 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
collision
Silicate minerals
Differential weathering
25. The supercontinent; existence proposed by Wegener - suggested that the supercontinent later fragmented into separate continents that then drifted apart - moving slowly to their present positions.
Fractional crystallization
Pangaea
Metals
Continental shelf
26. Blocks of rock that are solid and durable but composed of rough quartz sand grains cemented together.
Felsic
Sandstone
Slab-pull force
Granite
27. Mineral crystal formation type; form at interfaces between the physical and biological components of the Earth system by this process.
Rock layering
A-horizon
Subduction
Biomineralization
28. 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.
Andesitic lava flows
Glassy igneous rocks
Symmetry
Sill
29. The burial and lithification of angular or rounded clasts form these types of rocks.
A-horizon
Conglomerate
Large Igneous Provinces (LIPs)
Transgression
30. Measure of pressure or push in units of force - per unit area. 1 atm = 1.04 kilograms per square centimeter.
Graded bed
Granitic composition
atmospheres (atm)
Zone of accumulation
31. Cause of melting; magma can also form at locations where chemicals called volatiles mix with hot mantle rock. Elements such as water and carbon dioxide mix with hot rock - helping to break chemical bonds - so that if you add volatiles to a solid - ho
Clastic
Deposition
Felsic - intermediate - mafic - ultramafic
Volatiles
32. Active hot-spot volcanoes commonly occur at the end of a chain of dead volcanoes.
Diagenesis
Hot-spot track
Silicate minerals
Alloy
33. Type of magma; high silica content - viscous - liquid at temperatures as low as 700 degrees C.
Plutons
Abyssal plains
Rock composition
Granitic magma
34. A reaction during which an element loses electrons - commonly takes place when elements combine with oxygen.
Metamorphic rocks
Oxidation
Turbidite
Dolostone
35. Type of lava flow; mafic - low viscosity - extremely hot - flows very quickly.
Mineral crystal destruction
pahoehoe
Luster
Basaltic lava flows
36. Process that occurs after the sediment has been buried - pressure cause by the overburden squeezes out water and air that had been trapped between clasts - and the clasts press together tightly.
Magma mixing
Transgression
The effect of viscosity on eruptive style
Compaction
37. Aggregates of mineral crystals or grains - and masses of natural glass; a coherent - naturally occurring solid - consisting of an aggregate of minerals or a mass of glass.
Convective flow
Bed
Rocks
Organic chemicals
38. A linear belt in which continental lithosphere pulls apart - the lithosphere stretches horizontally.
Dolostone
12km
Dark Silicates
Continental rift
39. Magma type; contains only about 38% to 45% silica. Extreme form of mafic magma.
Ultramafic
Conchoidal fractures
Ignimbrite
Differential weathering
40. Actively slipping segment of a fracture zone between two ocean ridge segments - these faults make a third type of plate boundary - transforms.
Source rock composition
Coal
Transform fault
Halides
41. During this process - water chemically reacts with minerals and breaks them down - working faster in slightly acidic water.
Color
Plate tectonics
Hydrolysis
Loam
42. Distinguishing feature of magma; the process where magma sits in a magma chamber before completely solidifying - it may incorporate chemicals derived from the walls rocks of the chamber.
Flood basalts
Assimilation
Felsic - intermediate - mafic - ultramafic
Ridge-push force
43. Molten rock that has flowed out onto Earth's surface.
Pangaea
Transition zone
Lava
Magma
44. A fine spray of lava instantly freezes to form fine particles of glass.
O-horizon
Sea-floor spreading
Ash
Specific gravity
45. By melting - dissolving - or other chemical reactions.
Magnetic inclination
Mineral crystal destruction
Basalt
Zone of accumulation
46. A submarine suspension of sediment.
Turbidity current
Magnetic reversals
Clastic
Stratagraphic formation
47. 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
Siltstone and mudstone
Heat transfer
Redbeds
Silicates
48. 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.
The core
Rock composition
Oxidation
Superplumes
49. The absorption of water into the crystal structure of minerals - causes some minerals to expand.
Magnetic anomaly
Hydration
Relative plate velocity
Strata
50. Rocks whose crystals interlock with each other.
Crystalline
Dolostone
Source rock composition
Regolith