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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. 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.
triple junction
Organic sedimentary rocks
Paleopole
Crust
2. A reference to the supposed position of the Earth's magnetic pole at a time in the past.
Paleopole
Root wedging
Melts
Magma
3. Volcanic landform; pipes are short conduits that connect a magma chamber to the surface.
Volcanic pipes/necks
Viscosity
Compaction
Inner core
4. A place where three plate boundaries intersect at a point.
Lava tube
triple junction
Marine magnetic anomaly
Magnetic reversals
5. 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
Conchoidal fractures
Precipitation
Peridotite
Slab-pull force
6. The shape of the sea floor surface. Investigation of the sea-floor revealed the presence of several important features: mid-ocean ridges - deep-ocean trenches - seamount chains - and fracture zones.
Loam
Flood basalts
Bathymetry
Plates
7. A type of soil consisting of about 10-30% clay and the rest silt and sand. Pores remain between grains so that water and air can pass through and roots can easily penetrate.
Zone of accumulation
Granitic composition
Chemical sedimentary rocks
Loam
8. Forms from a chemical reaction between solid calcite and magnesium-bearing groundwater.
Gem
Dolostone
The effect of viscosity on eruptive style
Transported soil
9. 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.
Organic chemicals
Intrusive igneous rock
Outer core
Rhyolitic lava flows
10. 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
Transgression
The core
Fragmental igneous rocks
Viscosity
11. 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.
12km
Crystal lattice
Glass
Streak
12. Occurs within the asthenosphere - actively drags plates along and attributes partially for the mechanism shifting the plates along the Earth's surface.
Polymorphs
Chemical weathering
Convective flow
Depositional environment
13. Layer that lies below the lithosphere - and is the portion of the mantle in which rock can flow (slowly; 10-15cm per year) despite still being solid. Entirely within the mantle and lies below a depth of 100-150km.
Caliche
pahoehoe
Asthenosphere
Arkose
14. Equant - meaning that they have the same dimensions in all directions. Or inequant - meaning their dimensions are not the same in all directions.
Grain sizes
B-horizon
Lava domes
Erosion
15. During this process - water chemically reacts with minerals and breaks them down - working faster in slightly acidic water.
Hydrolysis
Magma
Oxides
Regolith
16. Physical property of a mineral; refers to the shape (morphology) of a single crystal with well-formed crystal faces - or to the character of an aggregate of many well-formed crystals that grew together as a group. Depends on the internal arrangement
Plates
Crystal habit
Granitic magma
Crystal
17. Sphere; Surface water along with groundwater - Earth consists of 70% surface water (oceans - lakes - and streams).
Spreading rate
Hydrosphere
Magnetic inclination
Shield volcano
18. A mineral's growth that is uninhibited - has well-formed crystal faces.
Euhedral crystal
Soil
Chemical weathering
Crystal lattice
19. 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.
Carbonates
Zone of leaching
Apparent polar-wander path
Rock-forming silicate minerals
20. Tree roots that grow into joints can push those joints open in this process.
C-horizon
Divergent plate boundary
Root wedging
Biomineralization
21. Rocks that consist of mineral crystals that intergrow when the melt solidifies - interlocking structure. Examples - granite and rhyolite.
Paleomagnetism
Crystalline igneous rocks
Metamorphic foliation
Depositional environment
22. Physical property of a mineral; represents the density of a mineral - as specified by the ratio between the weight of a volume of the mineral and the weight of an equal volume of water a 4 degrees C.
B-horizon
Peridotite
Specific gravity
Mafic
23. 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
Hydration
Fracture and cleavage
Magnetic declination
Silicates
24. Center of the Earth - consists mainly of iron alloy.
Convergent plate boundary
Loam
The core
Coal
25. Lava flow; associated with felsic magma - consists of ash and pumice fragments - material is propelled from the vent at a high speed.
Deep-ocean trenches
Volcano
Soil Horizons
Pyroclastic flows
26. Mineral crystal formation type; form at interfaces between the physical and biological components of the Earth system by this process.
Biomineralization
Ultramafic
Fumerolic mineralization
Mantle
27. Core division; from a depth of 5155km down to Earth's center at 6371km. A radius of about 1220km - is solid iron-nickel alloy - can reach temperature of 4700 degrees C. Solid in nature because of subjection to greater pressure - keeps atoms from wand
Inner core
Hydrosphere
Fractional crystallization
atmospheres (atm)
28. Rocks whose crystals interlock with each other.
Granite
Evaporites
Subsidence
Crystalline
29. Type of magma; low in silica - fluid - crystallize at high temperatures.
Magnetic inclination
Ash
Rock layering
Basaltic magma
30. Chemical weathering occurring in warm - wet climates can produce a layer of rotten rock - over 100km thick.
Saprolite
Organic sedimentary rocks
Mafic
Geothermal gradient
31. A proposition in 1960 - by Princeton University professor Harry Hess - that continents drift apart because new ocean floor forms between them by this process.
Clastic
Sea-floor spreading
Convergent plate boundary
B-horizon
32. 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.
Decompression
Rock texture
Convergent plate boundary
Dipole
33. A layer of sediment in which grain size varies from coarse at the bottom to fine at the top.
Strata
Fragmental igneous rocks
Paleopole
Graded bed
34. Rock formations still attached to the Earth's crust.
Hot spots
Organic chemicals
Deposition
Bedrock
35. 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
Convergent plate boundary
Subsidence
Volcano
Superplumes
36. 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
Decompression
Paleopole
Siliceous rocks
37. Physical property of a mineral; a measure of a minerals relative ability to resist scratching - and therefore represents the resistance of bonds in the crystal structure being broken. The atoms or ions in crystals of a hard mineral are more strongly
Calderas
Hardness
The effect of the environment on eruptive style
Saprolite
38. Places with particularly voluminous quantities of magma erupting or intruding.
Graded bed
A-horizon
Inner core
Large Igneous Provinces (LIPs)
39. A pluton formation theory; a process during Which magma assimilates wall rock - and blocks of wall rock break off and sink into the magma.
Stoping
Lava tube
Ignimbrite
Differential weathering
40. Type of sedimentary rock; rocks whose grains are stuck together by cement.
Evaporites
Plate tectonics
Lava
Clastic
41. An organic sedimentary rock; black - combustible rock consisting of over 50% carbon.
Crystal habit
Regression
Coal
Rock layering
42. 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
Granitic magma
Area of igneous activity
Relative plate velocity
43. A cut and finished stone ready to be used in jewelry. Examples - diamond - ruby - sapphire - emerald.
Graded bed
3.5km (2 miles)
Gem
Organic sedimentary rocks
44. A nearly horizontal - tabletop-shaped tabular intrusion - parallel to layering within the earth.
Sill
Magma
Transgression
Regolith
45. Inorganic limestone; rock composed of crystalline calcium carbonate formed by chemical precipitation.
Rock layering
ravertine
Superplumes
Outcrop
46. Similar to ripples - but are much larger. Small ripples often form on the surface of these structures.
Dunes
Zone of leaching
Physical weathering
Fractional crystallization
47. 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.
Lava domes
Solid-state diffusion
Dike
O-horizon
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.
Felsic - intermediate - mafic - ultramafic
Carbonate rocks
Decompression
Pyroclastic debris
49. Solids composed of metal atoms (such as iron - aluminum - copper - and tin). Within this type of solid - outer electrons are able to flow freely.
Dunes
Luster
Magma
Metals
50. Sedimentary rocks made up of the shells of organisms.
Biochemical sedimentary rocks
Rock layering
Glassy igneous rocks
Silicate minerals