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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. Distinguishing feature of magma; the composition of the melt reflects the composition of the solid from which it was derived. Not all magmas form from the same source rock - therefore not all magmas have the same compositions.
Glassy igneous rocks
Pyroclastic flows
Source rock composition
Crust
2. Forms a 2885-km-thick layer surrounding the core. In terms of volume - it is the largest part of the Earth. It consists entirely of ultramafic rock - peridotite.
Weathering
The effect of gas pressure on eruptive style
Dunes
Mantle
3. 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.
Volcanic pipes/necks
Silicates
Magnetic inclination
Compaction
4. Rock formations still attached to the Earth's crust.
Deep-ocean trenches
Bedrock
Mineral
Metals
5. Pea to plum-sized fragments of pyroclastic debris - consists of pumice or scoria fragments.
Residual soil
Crystal habit
Lapilli
Carbonates
6. A type of carbonate rock; rocks formed from the calcite or aragonite skeletons of organisms form this biochemical sedimentary rock.
Limestone
Lithosphere
Bedrock
Glass
7. A thick accumulation of sediment (10-15km) - the surface of this sediment layer is this broad - shallow region.
Relative plate velocity
Continental shelf
Ultramafic
Convective flow
8. Perhaps the cause for the large igneous provinces; formations within the mantle - plumes that bring up vastly more hot asthenosphere than normal plumes.
pahoehoe
Soil erosion
Superplumes
Crystalline
9. 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
Dunes
Outer core
Partial melting
Dolostone
10. 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.
Heat transfer
Fractional crystallization
Hydrolysis
Facets
11. An envelope of gas surrounding Earth consisting of 78% nitrogen (N2) and 28% oxygen (O2) - with minor amounts 1% of argon - carbon dioxide - methane - etc. And 99% of the gas in the atmosphere lies below 50km.
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12. Refers to the chemical reactions that alter or destroy minerals when rock comes in contact with water solutions or air.
Flood basalts
Chemical weathering
Basalt
Batholiths
13. Four settings: in volcanic arcs bordering deep-ocean trenches - isolated hot spots - within continental rifts - and along mid-ocean ridges.
Silicate minerals
Magnetic anomaly
Area of igneous activity
Lava domes
14. 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.
Soil erosion
Cross beds
Metamorphic rocks
Andesitic lava flows
15. 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
Residual soil
Metals
E-horizon
16. The conditions in which sediment was deposited. Examples - beach - glacial - and/or river environments.
Biochemical sedimentary rocks
Pangaea
Magma
Depositional environment
17. A fine spray of lava instantly freezes to form fine particles of glass.
Hot spots
Ignimbrite
Pyroclastic debris
Ash
18. A proposition in 1960 - by Princeton University professor Harry Hess - that continents drift apart because new ocean floor forms between them by this process.
Peridotite
Sea-floor spreading
Rock composition
Alloy
19. Rocks that forms by the freezing of lava above ground - after it spills out (extrudes) onto the surface of the Earth and comes into contact with the atmosphere or ocean.
Laccolith
Extrusive igneous rock
Saprolite
Siltstone and mudstone
20. Natural bond connecting rocks; mineral material that precipitates from water and fills the space between grains.
Intrusive igneous rock
Hot spots
Cement
Fracture and cleavage
21. 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.
Loam
Magnetic declination
Silicate minerals
Special properties of minerals
22. Mineral class; the fundamental component within these types of minerals in the Earth's crust is the silicon-oxygen tetrahedron anionic group - a silicon atom surrounded by four oxygen atoms that are arranged to define the corners of a tetrahedron - a
Bedding
Chemical sedimentary rocks
Diagenesis
Silicates
23. Active hot-spot volcanoes commonly occur at the end of a chain of dead volcanoes.
Luster
Melts
Transform fault
Hot-spot track
24. Type of lava flow; mafic - low viscosity - extremely hot - flows very quickly.
Basaltic lava flows
Divergent plate boundary
Fumerolic mineralization
Halides
25. 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
Crystalline
Turbidity current
Basalt
Why magma rises
26. Clast size - clast composition - angularity and sphericity - sorting - and character of cement.
A-horizon
Factors classifying clastic sedimentary rocks
Spreading rate
Strata
27. Mineral crystal formation type; form from a solidification of a melt - meaning the freezing of a liquid.
Melting
Dark Silicates
Paleopole
pahoehoe
28. Created from preexisting rocks which undergo changes - such as the growth of new minerals in response to pressure and heat - and/or as a result of squashing - stretching - or shear.
Metamorphic rocks
Differential weathering
Factors of magma cooling time
Phreatomagmatic eruptions
29. A place where three plate boundaries intersect at a point.
Jointing
Carbonate rocks
Magma
triple junction
30. Center of the Earth - consists mainly of iron alloy.
E-horizon
The core
Erosion
Glassy igneous rocks
31. Forms from a chemical reaction between solid calcite and magnesium-bearing groundwater.
B-horizon
Basaltic composition
Sedimentary Basins
Dolostone
32. A process occurring when the sea level rises - the coast migrates inland. Through this - an extensive layer of beach forms.
Crystal habit
Lava domes
Transgression
Organic sedimentary rocks
33. Actively slipping segment of a fracture zone between two ocean ridge segments - these faults make a third type of plate boundary - transforms.
Crystalline
Physical weathering
Transform fault
Sulfates
34. Occurs within the asthenosphere - actively drags plates along and attributes partially for the mechanism shifting the plates along the Earth's surface.
Convective flow
Lava tube
Agrillaceous rocks
Rhyolitic lava flows
35. A pluton formation theory; a process during Which magma assimilates wall rock - and blocks of wall rock break off and sink into the magma.
Agrillaceous rocks
Ridge-push force
Stoping
Volatiles
36. Mineral class; the molecule CO23 serves as the anionic group. Elements like calcium or magnesium bond to this group. Examples - calcite and dolomite.
Extrusive igneous rock
Stoping
Carbonates
Heat transfer
37. The Earth radiated heat into space and slowly cooled. Eventually - the early formed sea of lava solidified and formed igneous rock. The cumulative effect of radioactivity has been sufficient to slow the cooling of the planet and subsequently allow fo
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38. Irregular or blob-shaped intrusions that range in size from tens of meters across to tens of kilometers across.
Superplumes
Plutons
Solid-state diffusion
Transported soil
39. Type of volcanic eruption; produce mainly lava flows - yield low-viscosity basaltic lavas.
Metamorphic rocks
Effusive eruptions
rifting
Mantle
40. Coarse pyroclastic debris - apple to refrigerator-sized fragments. Chunks of preexisting igneous rock or large lava blobs which discharge from volcanic eruptions.
Earth's atmosphere
Luster
Turbidity current
Volcanic blocks/bombs
41. A sediment-filled depression; in an area where the lithosphere has subsided.
Transform plate boundary
Heat transfer
Sedimentary Basins
Hot-spot track
42. 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
Organic chemicals
Euhedral crystal
Magnetic anomaly
Partial melting
43. The way in which the atoms are packed together within a mineral by chemical bonds. Five difference types of bonding can occur - covalent - ionic - metallic - Van der Waal's - and hydrogen.
Rocks
Crystal structure
Differential weathering
Dike
44. 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.
Erosion
Bedrock
Tephra
Biomineralization
45. Two different minerals which have the same composition but have different crystal structures.
Transported soil
Rock composition
Polymorphs
Regression
46. Physical property of a mineral; results from the way a mineral interacts with light. A mineral absorbs certain wavelengths - so the color seen represents the color wavelengths the mineral did not absorb.
Fissure eruptions/lava plateaus
Asthenosphere
Color
Continental shelf
47. 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
Pyroclastic flows
Pyroclastic debris
Crystal habit
Hot spots
48. 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
Rock-forming silicate minerals
Crust
Divergent plate boundary
Dunes
49. Farther down from a zone of leaching - new mineral crystals precipitate directly out of the water or form when the water reacts with debris - this the region where the new minerals and clay collect.
Zone of accumulation
Calderas
Cinder cone
Upper mantle
50. Volcanic landform; pipes are short conduits that connect a magma chamber to the surface.
Calderas
Luster
Volcanic pipes/necks
Pangaea