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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. Type of volcano; built from ejected lava fragments - cone shaped piles of tephra - steep slope angle - smaller in size - frequently occur in groups - deep craters.
Cross beds
Tuff
E-horizon
Cinder cone
2. 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.
Loam
Andesitic lava flows
Luster
Glass
3. A proposition in 1960 - by Princeton University professor Harry Hess - that continents drift apart because new ocean floor forms between them by this process.
Pyroclastic debris
Cinder cone
Sea-floor spreading
Outer core
4. 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
Fissure eruptions/lava plateaus
Chemical sedimentary rocks
Mineral crystal destruction
Salt wedging
5. Refers to the chemical reactions that alter or destroy minerals when rock comes in contact with water solutions or air.
Lava
Factors of magma cooling time
Conchoidal fractures
Chemical weathering
6. 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
Volcano
Hardness
12km
Residual soil
7. Magma type; contains about 66% to 76% silica. Name reflects the occurrence of feldspar and quartz in rocks formed in this magma.
Rhyolitic lava flows
Soil Horizons
Felsic
Chert
8. 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.
Bed
Mafic
Apparent polar-wander path
Pangaea
9. A sheet of tuff formed from a pyroclastic flow.
Cinder cone
Felsic - intermediate - mafic - ultramafic
Loam
Ignimbrite
10. Mineral class; the molecule CO23 serves as the anionic group. Elements like calcium or magnesium bond to this group. Examples - calcite and dolomite.
Carbonates
Sedimentary rocks
Organic sedimentary rocks
Luster
11. Type of lava flow; mafic - low viscosity - extremely hot - flows very quickly.
The core
Turbidity current
Upper mantle
Basaltic lava flows
12. Sublayer of the mantle - depth of 660km.
E-horizon
Shield volcano
Hardness
Upper mantle
13. 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.
Pyroclastic debris
Transported soil
Chemical sedimentary rocks
Granite
14. An insulated - tunnel-like conduit through which lava moves within a flow.
Intrusive igneous rock
Melts
Lava tube
Ash
15. Distinguishing feature of magma; the process where magma changes composition as it cools because formation and sinking of crystals preferentially remove certain atoms from the magma.
Zone of accumulation
Fractional crystallization
Salt wedging
Tuff
16. Chemical precipitates; salt deposits formed as a consequence of evaporation. Examples - rock salt and gypsum.
Caliche
Jointing
Columnar jointing
Evaporites
17. 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.
Granite
Heat transfer
Rock texture
Sedimentary Basins
18. 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.
Fracture zones
Soil Horizons
Why magma rises
B-horizon
19. Successive turbidity currents deposit successive graded beds - creating this sequence of strata.
Pangaea
Turbidite
Sandstone
Cementation
20. A single - continuous (uninterrupted) piece of a crystalline solid bounded by flat surfaces called crystal faces that grew naturally as the mineral formed. Come in a variety of shapes - cubes - trapezoids - pyramids - octahedrons - hexagonal columns
Seamount chains
Crystal
12km
Reason for Earth's internal heat
21. The burial and lithification of angular or rounded clasts form these types of rocks.
Strata
Conglomerate
Magnetic reversals
Thermal expansion
22. Contributes to formation of soil; occurs when rainwater percolates through the debris and carries dissolved ions and clay flakes downward - This is the region where the downward transport occurs.
Sandstone
Chert
Zone of leaching
Agrillaceous rocks
23. 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.
Fragmental igneous rocks
Mid-ocean ridges
Basaltic composition
Chert
24. The removal of soil by running water or by wind.
Shield volcano
Magma mixing
Soil erosion
Phreatomagmatic eruptions
25. 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
Mantle plume
Relative plate velocity
3.5km (2 miles)
The core
26. Type of volcanic eruption; produce mainly lava flows - yield low-viscosity basaltic lavas.
Chemical sedimentary rocks
Ridge-push force
Sedimentary Basins
Effusive eruptions
27. A mafic rock with small grains. Extrusive - aphanitic igneous rock.
Fracture zones
Saprolite
Stoping
Basalt
28. Physical property of a mineral; refers to the way a mineral surface scatters light. Metallic versus non-metallic in nature.
Igneous rocks
Luster
O-horizon
Transform plate boundary
29. Type of sedimentary rock; rocks whose grains are stuck together by cement.
Factors of magma cooling time
Hydration
Lithification
Clastic
30. A reference to the supposed position of the Earth's magnetic pole at a time in the past.
12km
Paleopole
Cementation
Glass
31. 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.
Metamorphic rocks
Large Igneous Provinces (LIPs)
Assimilation
rifting
32. Active hot-spot volcanoes commonly occur at the end of a chain of dead volcanoes.
a'a'
Hot-spot track
Mantle
Lapilli
33. The separated lithosphere into distinct pieces. Twelve major 'pieces' and several minor. Consist of active margins and passive margins between them.
Plates
Regression
Pyroclastic flows
Phreatomagmatic eruptions
34. A submarine suspension of sediment.
Turbidity current
Diagenesis
O-horizon
Continental rift
35. Rocks which develop when hot molten rock cools and freezes solid.
Sea-floor spreading
Jointing
Igneous rocks
Hydrolysis
36. In degrees Celsius - the high temperatures at which igneous rocks freeze; the freezing of liquid melt to form solid igneous rock represents the same phenomenon as the freezing of water - except at much higher temperatures.
650-1100 degrees C
Mantle
Crystalline igneous rocks
Hydration
37. Rock made by the freezing of magma underground - after it has pushed its way (intruded) into preexisting rock of the crust.
Basalt
Intrusive igneous rock
Dike
Rock texture
38. Clast size - clast composition - angularity and sphericity - sorting - and character of cement.
Biomineralization
Ignimbrite
12km
Factors classifying clastic sedimentary rocks
39. Form from grains that break off preexisting rock and become cemented together - or from minerals that precipitate out of a water solution.
Hardness
Compaction
Alloy
Sedimentary rocks
40. 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.
atmospheres (atm)
3.5km (2 miles)
Heat transfer
Explosive eruptions
41. 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
Rhyolitic lava flows
Residual soil
Factors of magma cooling time
42. Type of lava flow; a lava flow with warm - pasty surfaces wrinkling into smooth - glassy - rope-like bridges.
Soil Horizons
pahoehoe
Continental drift evidence
Glassy igneous rocks
43. A mineral's growth that is uninhibited - has well-formed crystal faces.
Crystal habit
Euhedral crystal
Transported soil
Transform fault
44. Type of sedimentary soil/rock; Calcite in a pedocal soil accumulates in the B-horizon and may cement soil together - creating this solid mass.
Caliche
Dark Silicates
Rock composition
Continental rift
45. 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.
Basaltic composition
Laccolith
Compaction
Strata
46. Physical property of a mineral; refers to the color of a powder produced by pulverizing the mineral. Provides a fairly reliable clue to the mineral's identity - since the color of the mineral powder tends to be less variable than the color of the who
Arkose
Continental rift
Streak
Crystal
47. The broad - relatively flat regions of the ocean that lie at a depth of about 4-5km below sea level.
Arkose
Magnetic declination
Abyssal plains
Caliche
48. Process where new divergent boundaries form when a continent splits and separates into two continents.
Lava domes
Arkose
rifting
Felsic - intermediate - mafic - ultramafic
49. A sediment-filled depression; in an area where the lithosphere has subsided.
Sedimentary Basins
Stratagraphic formation
Carbonates
Biomineralization
50. Sedimentary rocks consisting of carbon-rich relicts of plants.
Dark Silicates
Light silicates
Organic sedimentary rocks
Basaltic lava flows