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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. 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
rifting
Magnetic anomaly
Laterite
Rock texture
2. 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.
Native metals
Deep-ocean trenches
Chemical sedimentary rocks
Zone of leaching
3. An ultramafic rock with large grains. intrusive - phaneritic igneous rock.
E-horizon
Peridotite
Dunes
Diagenesis
4. A reference to the pattern structure of a mineral. A material in which atoms are fixed in an orderly pattern - a crystalline solid.
Crystal lattice
Magnetic anomaly
Mantle plume
Crystal
5. Mineral crystal formation type; from directly from a vapor - occurs around volcanic vents or around geysers. At such locations - volcanic gases or steam enter the atmosphere and cool - so certain elements cannot remain in gaseous form.
Fumerolic mineralization
Differential weathering
Color
Siliceous rocks
6. Lava flowing on dry land cools more slowly that lava erupting underwater.
Large Igneous Provinces (LIPs)
Hot-spot track
The effect of the environment on eruptive style
Area of igneous activity
7. Fluid basaltic lava extruded from crustal fractures called fissures.
Fissure eruptions/lava plateaus
Igneous rocks
Ignimbrite
Subduction
8. Rocks which develop when hot molten rock cools and freezes solid.
Magnetic anomaly
Igneous rocks
Explosive eruptions
Caliche
9. Deeper sublayer of the mantle - depth of 660km to 2900km.
Magma's speed of flow
ravertine
Lower mantle
Salt wedging
10. Two different minerals which have the same composition but have different crystal structures.
Magma
Rock layering
Polymorphs
Rhyolitic lava flows
11. 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.
Cementation
Magma mixing
Limestone
Rhyolitic lava flows
12. 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.
Magnetic declination
Gem
Magnetic reversals
Soil Horizons
13. 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.
Mineral crystal destruction
Asthenosphere
Relative plate velocity
Metals
14. Active hot-spot volcanoes commonly occur at the end of a chain of dead volcanoes.
Rock texture
Hot-spot track
Tephra
Redbeds
15. Chemical precipitates; salt deposits formed as a consequence of evaporation. Examples - rock salt and gypsum.
Evaporites
Asthenosphere
Euhedral crystal
The effect of the environment on eruptive style
16. 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
Turbidity current
Subduction
Soil Horizons
E-horizon
17. Places with particularly voluminous quantities of magma erupting or intruding.
Rocks
Ignimbrite
Partial melting
Large Igneous Provinces (LIPs)
18. A naturally occurring solid - formed by geologic processes - has a crystalline structure and a definable chemical composition - and is generally inorganic.
Decompression
Mineral
Paleomagnetism
Chert
19. Physical property of a mineral; refers to the way a mineral surface scatters light. Metallic versus non-metallic in nature.
Volcano
Andesitic lava flows
Conglomerate
Luster
20. Type of igneous rock composition; composed of dark silicates and calcium-rich feldspar - referred to as mafic (magnesium and iron). Make up the ocean floor/volcanic islands.
Zone of leaching
Laterite
Basaltic composition
collision
21. Sedimentary rock composed of clay.
Plate tectonics
Rock layering
Agrillaceous rocks
Chert
22. In addition to islands that rise above sea level - seamounts have been detected (isolated submarine mountains) - once volcanoes but no longer erupt.
Partial melting
Seamount chains
Mineral crystal destruction
Limestone
23. 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
Tuff
Subsidence
Convergent plate boundary
Relative plate velocity
24. Cause of melting; the variation in temperature with depth is expressed in the geotherm; because pressure prevents melting - a decrease in pressure can permit melting. Specifically - if the pressure affecting hot mantle rock decreases while the temper
Plates
Decompression
Siliceous rocks
Zone of accumulation
25. Natural bond connecting rocks; mineral material that precipitates from water and fills the space between grains.
Bathymetry
Cement
Specific gravity
Sedimentary rocks
26. Rocks whose crystals interlock with each other.
Specific gravity
Crystalline
Pyroclastic debris
Frost wedging
27. During the final stages of cooling - lava flows contract and may fracture into roughly hexagonal columns.
Columnar jointing
Differential weathering
Transition zone
Quartz sandstone
28. 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.
Explosive eruptions
Batholiths
Intrusive igneous rock
Facets
29. Distinguishing feature of magma; Because not all minerals melt by the same amount under given conditions - and because chemical reactions take place during melting - the magma that forms as a rock begins to melt does not have the same composition as
Magnetic inclination
Partial melting
Pyroclastic debris
Lower mantle
30. 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.
Biomineralization
Chemical sedimentary rocks
Continental drift evidence
Thermal expansion
31. Biochemical sedimentary rock; it's made from cryptocrystalline quartz. Examples - flint and jasper.
Chert
Solid-state diffusion
Columnar jointing
Polymorphs
32. Type of sedimentary soil/rock; Calcite in a pedocal soil accumulates in the B-horizon and may cement soil together - creating this solid mass.
Andesitic lava flows
Crystalline
Granite
Caliche
33. 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.
Stratagraphic formation
Hardness
Divergent plate boundary
Oxides
34. 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
Magnetic reversals
Light silicates
Hydrolysis
Sandstone
35. A sediment-filled depression; in an area where the lithosphere has subsided.
Transgression
Plate tectonics
Volcano
Sedimentary Basins
36. A process occurring when the sea level rises - the coast migrates inland. Through this - an extensive layer of beach forms.
Dark Silicates
Apparent polar-wander path
Transgression
Physical weathering
37. Perhaps the cause for the large igneous provinces; formations within the mantle - plumes that bring up vastly more hot asthenosphere than normal plumes.
O-horizon
Lava domes
Superplumes
Cementation
38. A fine spray of lava instantly freezes to form fine particles of glass.
Special properties of minerals
Mid-ocean ridges
Ash
Peridotite
39. Chemical weathering during Which minerals dissolve into water.
Dissolution
Crystal habit
Pangaea
Magnetic inclination
40. 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.
Transgression
Sedimentary Basins
Silicate minerals
Quartz sandstone
41. 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.
Turbidity current
Effusive eruptions
Siltstone and mudstone
Silicates
42. Similar to ripples - but are much larger. Small ripples often form on the surface of these structures.
Dunes
12km
Hardness
Pyroclastic flows
43. Rock made by the freezing of magma underground - after it has pushed its way (intruded) into preexisting rock of the crust.
Intrusive igneous rock
Sulfides
Sill
pahoehoe
44. Inorganic limestone; rock composed of crystalline calcium carbonate formed by chemical precipitation.
Sedimentary rocks
Transgression
ravertine
Euhedral crystal
45. 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
Apparent polar-wander path
Igneous rocks
The effect of viscosity on eruptive style
Sulfides
46. 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.
Laccolith
Geothermal gradient
Mid-ocean ridges
Bathymetry
47. Materials that easily transform into gas at the relatively low temperatures found at the Earth's surface.
Volatiles
Graded bed
Diagenesis
Glass
48. An exposure of bedrock.
Outcrop
Basaltic lava flows
Symmetry
Stoping
49. Type of volcanic eruption; takes place when water gains access to the hot rock around the magma chamber and suddenly transforms into steam - a pyroclastic eruption involving the reaction of water with magma.
Turbidite
Phreatomagmatic eruptions
Cinder cone
Residual soil
50. Process where new divergent boundaries form when a continent splits and separates into two continents.
Halides
Cross beds
Ultramafic
rifting