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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. Sedimentary rock composed of clay.
Agrillaceous rocks
Lava tube
Laterite
Slab-pull force
2. After sand has lost its feldspar composition due to weathering over time - sediment composed entirely of quartz grains gets buried and lithified to form this type of rock.
Quartz sandstone
Marine magnetic anomaly
Lithification
Pyroclastic debris
3. 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
atmospheres (atm)
Chert
Transform plate boundary
collision
4. A submarine suspension of sediment.
Spreading rate
Turbidity current
Sill
Transform plate boundary
5. 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
Viscosity
Color
Glass
Dike
6. Measure of pressure or push in units of force - per unit area. 1 atm = 1.04 kilograms per square centimeter.
Reason for Earth's internal heat
Dipole
atmospheres (atm)
Alloy
7. Refers to the chemical reactions that alter or destroy minerals when rock comes in contact with water solutions or air.
Tuff
Chemical weathering
Cinder cone
Mineral
8. Hot basaltic lava that erupts with such low viscosity that it can flow tens to hundreds of kilometers across the landscape.
Facets
Flood basalts
Batholiths
Shield volcano
9. 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.
Halides
Explosive eruptions
Large Igneous Provinces (LIPs)
Sill
10. A type of carbonate rock; rocks formed from the calcite or aragonite skeletons of organisms form this biochemical sedimentary rock.
Limestone
Differential weathering
Soil erosion
Crystal
11. A reference to the pattern structure of a mineral. A material in which atoms are fixed in an orderly pattern - a crystalline solid.
Physical weathering
Crystal lattice
Transform fault
Inner core
12. Mineral group; olivine group - pyroxene group - amphibole group.
Magnetic reversals
Granitic magma
Subsidence
Dark Silicates
13. Deeper sublayer of the mantle - depth of 660km to 2900km.
Loam
Mineral
Lithification
Lower mantle
14. Chemical weathering during Which minerals dissolve into water.
Soil Horizons
Strata
Dissolution
Divergent plate boundary
15. Mineral crystal formation type; form from a solidification of a melt - meaning the freezing of a liquid.
Rhyolitic lava flows
Dolostone
Fracture zones
Melting
16. 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.
Lower mantle
Chemical sedimentary rocks
Symmetry
Basalt
17. Distinct internal laminations within a ripple or dune that are inclined at an angle to the boundary of the main sedimentary layer. Form as a consequence of the evolution of dunes or ripples.
Luster
Cross beds
Igneous rocks
Ridge-push force
18. The transformation of loose sediment into solid rock.
Crystal lattice
Basaltic lava flows
Hot-spot track
Lithification
19. Volcanoes that exist as isolated points and appear to be independent of movement at a plate boundary - hot-spot volcanoes. Mostly are located on the interior of plates - away from boundaries.
Soil erosion
The core
Rock composition
Hot spots
20. 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
Regolith
The effect of viscosity on eruptive style
Melting
Fragmental igneous rocks
21. 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
Strata
Symmetry
Oxides
Mantle plume
22. By melting - dissolving - or other chemical reactions.
12km
Granitic composition
Mineral crystal destruction
Frost wedging
23. Mineral crystal formation type; form from a solution - meaning that atoms - molecules - or ions dissolved in water bond together out of water.
Precipitation
Viscosity
Continental drift evidence
Silicate minerals
24. Along much of the perimeter of the Pacific Ocean - the ocean floor reaches astounding depths of 8-12km. These areas define elongate troughs - and they border volcanic arcs - the curving chains of active volcanoes.
Lava domes
Basaltic lava flows
Sedimentary Basins
Deep-ocean trenches
25. Sedimentary rock composed of quartz.
Volatiles
Plutons
Siliceous rocks
Lapilli
26. An intrusion starting to inject between layers but then dome upwards - creating this blister-shaped intrusion.
Earth's atmosphere
The core
Magnetic anomaly
Laccolith
27. A place where three plate boundaries intersect at a point.
triple junction
Special properties of minerals
Tephra
Subsidence
28. Rock made by the freezing of magma underground - after it has pushed its way (intruded) into preexisting rock of the crust.
Outer core
Fissure eruptions/lava plateaus
Heat transfer
Intrusive igneous rock
29. 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.
Special properties of minerals
Cementation
Calderas
Glass
30. The combination of processes that separate rock or regolith from its substrate and carry it away. Involves abrasion - plucking - scouring - and dissolution - and is caused by air - water or ice.
Basaltic composition
Intermediate
Continental rift
Erosion
31. The intrusion of numerous plutons in a region - produces a vast composite body that may be several hundred kilometers long and over 100km wide; an immense body of igneous rock.
Fracture zones
Batholiths
650-1100 degrees C
Transported soil
32. Some rocks develop their magnetization - their ability to produce a magnetic field - at the time that the rocks themselves formed. Such rocks - preserve a record of the Earth's magnetic field at known times in the past.
Loam
Paleomagnetism
Transported soil
collision
33. Chemical precipitates; salt deposits formed as a consequence of evaporation. Examples - rock salt and gypsum.
Organic chemicals
Large Igneous Provinces (LIPs)
Evaporites
Fumerolic mineralization
34. 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
atmospheres (atm)
Fumerolic mineralization
Divergent plate boundary
Transition zone
35. The most common minerals in the Earth. Contain silica (SiO2) mixed in varying proportions with other elements (typically iron - magnesium - aluminum - calcium - potassium - and sodium).
Silicate minerals
Rhyolitic lava flows
O-horizon
Factors of magma cooling time
36. Similar to ripples - but are much larger. Small ripples often form on the surface of these structures.
Granite
The core
Lava tube
Dunes
37. 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.
Magnetic inclination
Thermal expansion
Weathering
Explosive eruptions
38. Because different soil-forming processes operate at different depths - soils typically develop into these distinct zones. These zones can be arranged vertically into a soil profile.
Soil Horizons
Subduction
Peridotite
Dark Silicates
39. A reaction during which an element loses electrons - commonly takes place when elements combine with oxygen.
Oxidation
Partial melting
Metamorphic rocks
Five steps of clastic sedimentary rock formation
40. Blocks of rock that are solid and durable but composed of rough quartz sand grains cemented together.
Mineral
Sandstone
Clastic sedimentary rocks
Special properties of minerals
41. 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.
Facets
Turbidity current
Cinder cone
Magnetic declination
42. Lava flow; associated with felsic magma - consists of ash and pumice fragments - material is propelled from the vent at a high speed.
Pyroclastic flows
Source rock composition
Calderas
Dark Silicates
43. 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.
Polymorphs
Lava tube
Heat transfer
Strata
44. Type of volcanic eruption; produce mainly lava flows - yield low-viscosity basaltic lavas.
650-1100 degrees C
Assimilation
Effusive eruptions
Igneous rocks
45. The speed of the movements of the plates with respect to the speed of the other plates' movements. Absolute plate velocity is a measure of the movement of any plates relative to a fixed point in the mantle.
Relative plate velocity
Divergent plate boundary
Solid-state diffusion
Dissolution
46. Form when solid materials become hot and transform into liquid - example - molten rock.
Topography
Organic chemicals
Elemental composition of Earth
Melts
47. The difference between the expected strength of the Earth's main field at a certain location and the actual measure strength of the magnetic field at that location. Places where the field strength is stronger that expected are positive anomalies - an
Elemental composition of Earth
Carbonates
Magnetic anomaly
Symmetry
48. Type of lava flow; mafic - low viscosity - extremely hot - flows very quickly.
Compaction
C-horizon
Mafic
Basaltic lava flows
49. Layering in metamorphic rocks.
Hardness
Metamorphic foliation
Bathymetry
Xenolith
50. 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.
Carbonate rocks
Calderas
Fracture zones
Reason for Earth's internal heat