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Test your basic knowledge |
Geology
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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. Volcanic landform; bulbous mass of congealed lava - associated with explosive eruptions of gas-rich magma.
Evaporites
Coal
Facets
Lava domes
2. Molten rock that has flowed out onto Earth's surface.
Thermal expansion
Lava
Oxidation
Diagenesis
3. The absorption of water into the crystal structure of minerals - causes some minerals to expand.
Fractional crystallization
Lithosphere
Mid-ocean ridges
Hydration
4. Mineral class; consist of a metal cation bonded to a sulfide anion. Examples - galena and pyrite. Many have a metallic luster. Can also be considered ores with high proportions of metal within the mineral.
Sulfides
Heat transfer
pahoehoe
Frost wedging
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
Oxidation
Columnar jointing
Viscosity
Rhyolitic lava flows
6. 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.
Explosive eruptions
Turbidite
Weathering
Specific gravity
7. 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.
Saprolite
Frost wedging
Batholiths
Plate tectonics
8. The burial and lithification of angular or rounded clasts form these types of rocks.
Continental drift evidence
Conglomerate
Rock-forming silicate minerals
Hydrolysis
9. 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.
Sandstone
Halides
Deposition
Rock texture
10. Refers to the processes that break up and corrode solid rock - eventually transforming it into sediment. Physical and chemical variations.
Weathering
Igneous rocks
Laterite
Mid-ocean ridges
11. A place where three plate boundaries intersect at a point.
triple junction
Luster
Continental rift
E-horizon
12. Places with particularly voluminous quantities of magma erupting or intruding.
Large Igneous Provinces (LIPs)
Five steps of clastic sedimentary rock formation
Fracture zones
Zone of accumulation
13. A process occurring when the sea level rises - the coast migrates inland. Through this - an extensive layer of beach forms.
Rock composition
Carbonate rocks
Bathymetry
Transgression
14. 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.
Tephra
Dike
Thermal expansion
Rhyolitic lava flows
15. 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.
Abyssal plains
Composite cone (stratovolcano)
Area of igneous activity
Frost wedging
16. Deeper sublayer of the mantle - depth of 660km to 2900km.
Lower mantle
Symmetry
Flood basalts
Area of igneous activity
17. A process occurring when sea level falls - the coast migrates seaward.
Bed
Diagenesis
Regression
Sulfides
18. 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.
Mantle plume
Magnetic inclination
Sandstone
Laterite
19. 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.
Magnetic inclination
Cross beds
Ripples
Basalt
20. 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
Magnetic anomaly
Why magma rises
B-horizon
Divergent plate boundary
21. 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
Soil
Granitic magma
Apparent polar-wander path
22. 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
Andesitic lava flows
Crystal habit
Plate tectonics
3.5km (2 miles)
23. A felsic rock with large grains. Intrusive - phaneritic igneous rock.
Convective flow
Sill
Magnetic reversals
Granite
24. Sedimentary rocks made up of minerals that precipitate directly from water solutions.
Conchoidal fractures
Chemical sedimentary rocks
Transition zone
Source rock composition
25. 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
Stoping
Dipole
Zone of leaching
Seamount chains
26. Unconsolidated deposits of pyroclastic grains - regardless of size - that have been erupted from a volcano constitute these pyroclastic deposits.
Metals
3.5km (2 miles)
Tephra
Oxidation
27. 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.
Hydrolysis
Rock-forming silicate minerals
Bedrock
Intermediate
28. Type of volcanic eruption; produce mainly lava flows - yield low-viscosity basaltic lavas.
Batholiths
Rock layering
Effusive eruptions
Organic sedimentary rocks
29. 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.
Biomineralization
Deep-ocean trenches
Pyroclastic debris
Organic chemicals
30. Mineral class; the anion within these types of minerals is a halogen ion (such as chlorine or fluorine).
Regolith
Upper mantle
Bed
Halides
31. If a stoped block does not melt entirely - but rather becomes surrounded by new igneous rock - it becomes this; xeno - meaning foreign.
Granitic composition
Xenolith
Granitic magma
Basaltic composition
32. 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
Salt wedging
Mid-ocean ridges
Mantle plume
Elemental composition of Earth
33. 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.
Silicate minerals
Organic chemicals
Sulfides
Crust
34. Blocks of rock that are solid and durable but composed of rough quartz sand grains cemented together.
Rhyolitic lava flows
Diagenesis
Sandstone
Seamount chains
35. Sedimentary rock composed of calcite or dolomite.
Carbonate rocks
Lava tube
Sea-floor spreading
Turbidite
36. Active hot-spot volcanoes commonly occur at the end of a chain of dead volcanoes.
Clastic
Continental rift
Inner core
Hot-spot track
37. Mineral crystal formation type; form from a solution - meaning that atoms - molecules - or ions dissolved in water bond together out of water.
collision
Glass
Precipitation
Clastic
38. The fit of the continents - locations of past glaciations - the distribution of equatorial climatic belts - the distribution of fossils - and matching geologic units.
Magma mixing
Continental drift evidence
Fracture zones
Felsic
39. Hot basaltic lava that erupts with such low viscosity that it can flow tens to hundreds of kilometers across the landscape.
Flood basalts
Upper mantle
Organic chemicals
Basaltic magma
40. The process by which sediment settles out of the transporting medium.
Deposition
C-horizon
Fragmental igneous rocks
Sedimentary structure
41. 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
Melts
pahoehoe
Silicate minerals
Divergent plate boundary
42. 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.
Superplumes
Felsic - intermediate - mafic - ultramafic
Glass
Granite
43. 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.
Physical weathering
Sulfides
Rhyolitic lava flows
Assimilation
44. 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
Sill
Magnetic reversals
Fracture zones
Light silicates
45. Sedimentary rock composed of clay.
Fragmental igneous rocks
Basaltic composition
Magnetic reversals
Agrillaceous rocks
46. 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.
Diagenesis
Siliceous rocks
Redbeds
Soil Horizons
47. Rocks with a fragmental texture consist of igneous fragments that are packed together - welded together - or cemented together after having solidified. Examples - pyroclastic rocks such as tuff or breccia.
Plutons
Tuff
Zone of accumulation
Fragmental igneous rocks
48. Materials that easily transform into gas at the relatively low temperatures found at the Earth's surface.
Transgression
Volatiles
Cement
Solid-state diffusion
49. A reference to the pattern structure of a mineral. A material in which atoms are fixed in an orderly pattern - a crystalline solid.
Paleomagnetism
Crystal lattice
O-horizon
Viscosity
50. 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.
Soil Horizons
Specific gravity
Dunes
Soil erosion