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Test your basic knowledge |
Geology
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Study First
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. A term used for all the physical - chemical - and biological processes that transform sediment into sedimentary rock and that alter characteristics of sedimentary rock one the rock has formed.
Ridge-push force
Diagenesis
Explosive eruptions
Strata
2. If a stoped block does not melt entirely - but rather becomes surrounded by new igneous rock - it becomes this; xeno - meaning foreign.
Turbidite
Melting
a'a'
Xenolith
3. A single layer of sediment or sedimentary rock with a recognizable top and bottom.
Bed
E-horizon
Carbonate rocks
Sea-floor spreading
4. Volcanic landform; steep walled depression at the summit - size exceeds one kilometer in diameter.
Calderas
Crystal structure
Biomineralization
Organic sedimentary rocks
5. Irregular or blob-shaped intrusions that range in size from tens of meters across to tens of kilometers across.
Dipole
Euhedral crystal
Rock-forming silicate minerals
Plutons
6. 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.
Composite cone (stratovolcano)
Halides
Superplumes
Organic chemicals
7. Type of volcanic eruption; produce mainly lava flows - yield low-viscosity basaltic lavas.
Dolostone
Magma's speed of flow
Effusive eruptions
Regolith
8. 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
Composite cone (stratovolcano)
Why magma rises
Subsidence
Native metals
9. Four settings: in volcanic arcs bordering deep-ocean trenches - isolated hot spots - within continental rifts - and along mid-ocean ridges.
Area of igneous activity
Diagenesis
Chert
Continental drift evidence
10. An intrusion starting to inject between layers but then dome upwards - creating this blister-shaped intrusion.
Dark Silicates
Glass
Carbonate rocks
Laccolith
11. 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
E-horizon
Clastic
Volatiles
C-horizon
12. 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
Metamorphic rocks
The core
Subduction
13. The record of paleomagnetism revealed that the location of Earth's magnetic poles had been changing through geologic time. This 'wandering' meant that Earth's magnetic poles do not move with respect to fixed continents. Rather - continents move relat
Lithosphere
collision
Convergent plate boundary
Apparent polar-wander path
14. Mineral class; consist of pure masses of a single metal - with metallic bonds. Copper and gold can appear in this way.
Crystal habit
Earth's atmosphere
Native metals
Ash
15. 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
Sulfates
Earth's atmosphere
Depositional environment
Volatiles
16. An exposure of bedrock.
Conchoidal fractures
Outcrop
Salt wedging
Bed
17. A reference to the supposed position of the Earth's magnetic pole at a time in the past.
Volcanic pipes/necks
Strata
Paleopole
Igneous rocks
18. Layering in metamorphic rocks.
Mineral
Rock-forming silicate minerals
Metamorphic foliation
Gem
19. Sedimentary rocks made up of the shells of organisms.
Biochemical sedimentary rocks
Soil erosion
Lava
Intermediate
20. 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.
Melting
Source rock composition
Thermal expansion
Basaltic composition
21. Refers to the processes that break up and corrode solid rock - eventually transforming it into sediment. Physical and chemical variations.
Plates
Weathering
Magma
Ultramafic
22. 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
Depositional environment
Basaltic lava flows
Felsic - intermediate - mafic - ultramafic
pahoehoe
23. Type of lava flow; mafic - low viscosity - extremely hot - flows very quickly.
Conglomerate
Weathering
Basaltic lava flows
Precipitation
24. 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.
Symmetry
Transform plate boundary
Fragmental igneous rocks
Chemical weathering
25. Form from grains that break off preexisting rock and become cemented together - or from minerals that precipitate out of a water solution.
Decompression
Magma's speed of flow
Continental shelf
Sedimentary rocks
26. 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.
Mineral crystal destruction
Spreading rate
Clastic
Explosive eruptions
27. A sedimentary bed that has developed a reddish color. The red comes from a film of iron oxide (hematite) that forms on grain surfaces.
The core
Arkose
Carbonates
Redbeds
28. 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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29. Blocks of rock that are solid and durable but composed of rough quartz sand grains cemented together.
Elemental composition of Earth
Ignimbrite
Sandstone
Rock composition
30. The bottom portion of the upper mantle - the interval lying between 400km and 660km deep. Here within the Earth - the character of the mantle undergoes a series of abrupt changes.
Transition zone
Quartz sandstone
Soil erosion
Ripples
31. 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
Rock texture
Laterite
Why magma rises
Silicate minerals
32. During this process - water chemically reacts with minerals and breaks them down - working faster in slightly acidic water.
Clastic
Topography
Ridge-push force
Hydrolysis
33. Rocks that consist of mineral crystals that intergrow when the melt solidifies - interlocking structure. Examples - granite and rhyolite.
Dunes
Glass
Granitic composition
Crystalline igneous rocks
34. 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
Conchoidal fractures
Pangaea
Coal
Mantle plume
35. Sublayer of the mantle - depth of 660km.
Transform plate boundary
Chert
Upper mantle
Phreatomagmatic eruptions
36. Built up deposit of volcanic bombs and lapilli - known as volcanic agglomerate.
Tuff
Lapilli
a'a'
Chemical weathering
37. Molten rock beneath Earth's surface.
Magma
Residual soil
Loam
Root wedging
38. Form when solid materials become hot and transform into liquid - example - molten rock.
Fragmental igneous rocks
Melts
Depositional environment
Carbonates
39. A submarine suspension of sediment.
Turbidity current
Fissure eruptions/lava plateaus
Melting
Metamorphic rocks
40. Type of lava flow; the most viscous of any lava flow because it is the most silicic and the coolest in nature. Tends to accumulate in a lava dome above the vent or in short and bulbous flows 1 to 2 km long.
Area of igneous activity
Biomineralization
Rhyolitic lava flows
Native metals
41. A vent at Which melt from inside the Earth spews onto the planet's surface. Erupt.
Hardness
Cinder cone
Siltstone and mudstone
Volcano
42. 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.
Pangaea
Crystal structure
Area of igneous activity
Oxidation
43. 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.
Abyssal plains
Agrillaceous rocks
Carbonate rocks
Soil
44. Fracture type; smoothly curving - clamshell-shaped surfaces; typically formed in quartz.
Conchoidal fractures
Dissolution
a'a'
Graded bed
45. 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.
Weathering
Magnetic declination
Bed
Bedding
46. Occurs within the asthenosphere - actively drags plates along and attributes partially for the mechanism shifting the plates along the Earth's surface.
Crust
Convective flow
Coal
Turbidite
47. 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.
Mantle plume
Apparent polar-wander path
Crystalline igneous rocks
Composite cone (stratovolcano)
48. 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.
Magnetic anomaly
Rock-forming silicate minerals
Luster
Cementation
49. Magma type; contains about 45% to 52% silica. Named because it produces rock containing abundant mafic minerals - magnesium and iron combinations.
Mafic
Evaporites
Topography
Volatiles
50. 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
Ridge-push force
B-horizon
Batholiths