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Test your basic knowledge |
Geology
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Subject
:
science
Instructions:
Answer 50 questions in 15 minutes.
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Match each statement with the correct term.
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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. A reference to the pattern structure of a mineral. A material in which atoms are fixed in an orderly pattern - a crystalline solid.
Light silicates
Crystal lattice
Stratagraphic formation
Rock composition
2. 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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3. A sheet of tuff formed from a pyroclastic flow.
Ignimbrite
Volatiles
Basaltic lava flows
Organic chemicals
4. 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
Lava tube
Graded bed
Outer core
Crystal
5. Mineral group; olivine group - pyroxene group - amphibole group.
Volcano
Mineral
Crystalline igneous rocks
Dark Silicates
6. A mixture containing more than one type of metal atom. Example - bronze is a mixture of copper and tin.
Chemical sedimentary rocks
Igneous rocks
Alloy
Special properties of minerals
7. 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.
Lava domes
Crystalline igneous rocks
Shield volcano
Crystal structure
8. Layering in sedimentary rocks.
Rock-forming silicate minerals
Viscosity
Bedding
Reason for Earth's internal heat
9. When different rocks in an outcrop undergo weathering at different rates.
Specific gravity
Stoping
Differential weathering
Graded bed
10. 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.
Cinder cone
Glassy igneous rocks
Laccolith
O-horizon
11. The crust moves away from the Mid-Atlantic Ridge axis at a rate of 1cm per year. This velocity of sea-floor spreading is determined by the relationship between the paleomagnetic anomaly-stripe's width and the reverse polarity duration - the data reve
Cinder cone
Spreading rate
Facets
Ridge-push force
12. Volcanic landform; steep walled depression at the summit - size exceeds one kilometer in diameter.
Glassy igneous rocks
Calderas
Basaltic magma
Grain sizes
13. Physical property of a mineral; refers to the way a mineral surface scatters light. Metallic versus non-metallic in nature.
Bedding
The effect of gas pressure on eruptive style
Luster
Outer core
14. Carbon-containing compounds that either occur in living organisms - or have characteristics that resemble the molecules within living organisms. Examples - oil - protein - plastic - fat - and rubber.
Hydration
Basaltic composition
Grain sizes
Organic chemicals
15. Refers to the processes that break up and corrode solid rock - eventually transforming it into sediment. Physical and chemical variations.
Deposition
Basalt
Weathering
Lithosphere
16. 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.
Lava domes
Crystal structure
Superplumes
Diagenesis
17. 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.
Mineral crystal destruction
The effect of the environment on eruptive style
Fragmental igneous rocks
Root wedging
18. 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.
Dunes
Glass
Fracture zones
Magma's speed of flow
19. A rock made of solid mass of glass - or of tiny crystals surrounded by glass. Reflect light as glass does and tend to break conchoidally. Examples - obsidian - tachylite - pumice.
Fractional crystallization
Rock composition
Root wedging
Glassy igneous rocks
20. 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.
Crystal structure
Asthenosphere
Relative plate velocity
Magnetic inclination
21. Two different minerals which have the same composition but have different crystal structures.
Granitic composition
Turbidite
Polymorphs
Streak
22. Rocks which develop when hot molten rock cools and freezes solid.
Igneous rocks
Superplumes
Ultramafic
Evaporites
23. An ultramafic rock with large grains. intrusive - phaneritic igneous rock.
Rock composition
The effect of the environment on eruptive style
Peridotite
Conglomerate
24. 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.
Plates
Turbidity current
Sedimentary rocks
Magnetic declination
25. Perhaps the cause for the large igneous provinces; formations within the mantle - plumes that bring up vastly more hot asthenosphere than normal plumes.
Superplumes
Felsic
Reason for Earth's internal heat
Siliceous rocks
26. Molten rock that has flowed out onto Earth's surface.
Mineral crystal destruction
Inner core
Lava
Columnar jointing
27. Mineral crystal formation type; form by type of diffusion - the movement of atoms or ions through a solid to arrange into a new crystal structure; process takes place very slowly.
Salt wedging
Solid-state diffusion
Mineral crystal destruction
Convergent plate boundary
28. A place where three plate boundaries intersect at a point.
triple junction
Cementation
Fragmental igneous rocks
Zone of leaching
29. During the final stages of cooling - lava flows contract and may fracture into roughly hexagonal columns.
Granitic magma
Transition zone
Columnar jointing
Factors classifying clastic sedimentary rocks
30. Unconsolidated deposits of pyroclastic grains - regardless of size - that have been erupted from a volcano constitute these pyroclastic deposits.
Tephra
Elemental composition of Earth
Caliche
3.5km (2 miles)
31. A reference to the supposed position of the Earth's magnetic pole at a time in the past.
Quartz sandstone
Paleopole
Deposition
Paleomagnetism
32. Type of lava flow; mafic - low viscosity - extremely hot - flows very quickly.
Granitic composition
Weathering
Basaltic lava flows
Volcanic blocks/bombs
33. A plate boundary at which one plate slips along the side of another plate. No new plate is formed and no old plate is consumed. But the grinding between the plates generates frequent and destructive earthquakes.
Transition zone
Transform plate boundary
Granitic magma
Lava tube
34. A sedimentary bed that has developed a reddish color. The red comes from a film of iron oxide (hematite) that forms on grain surfaces.
E-horizon
Transform fault
collision
Redbeds
35. Magma type; contains only about 38% to 45% silica. Extreme form of mafic magma.
Divergent plate boundary
Ultramafic
Tephra
Continental drift hypothesis
36. Volcanic landform; bulbous mass of congealed lava - associated with explosive eruptions of gas-rich magma.
Stoping
Lava domes
Dipole
Mineral crystal destruction
37. 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.
Why magma rises
Fracture zones
Strata
Salt wedging
38. Type of igneous rock composition; composed of light-colored silicates - very rich in felsic (feldspar and silica). Major constituent of continental crust.
Continental shelf
Granitic composition
Clastic
Special properties of minerals
39. Refers to the proportions of different chemicals making up the rock - and thus the proportion chemicals affects the proportions of different minerals constituting the rock.
Metamorphic foliation
Relative plate velocity
Rock composition
Mafic
40. 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.
Mantle
Calderas
Basaltic lava flows
Plate tectonics
41. 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.
Bedrock
C-horizon
Silicates
Fractional crystallization
42. The broad - relatively flat regions of the ocean that lie at a depth of about 4-5km below sea level.
Cross beds
Chemical sedimentary rocks
Abyssal plains
Magma
43. Pea to plum-sized fragments of pyroclastic debris - consists of pumice or scoria fragments.
Lapilli
Coal
Turbidity current
Turbidite
44. A process occurring when the sea level rises - the coast migrates inland. Through this - an extensive layer of beach forms.
Transgression
Oxides
Evaporites
Hydration
45. The force that subducting plates apply to oceanic lithosphere at a convergent boundary - arises simply because lithosphere formed 10 million years ago is denser than asthenosphere - so it can sink into the asthenosphere. Thus once an oceanic plate st
Luster
Fumerolic mineralization
Intermediate
Slab-pull force
46. Form from grains that break off preexisting rock and become cemented together - or from minerals that precipitate out of a water solution.
Sedimentary rocks
Organic sedimentary rocks
Hot-spot track
Crystal lattice
47. 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.
Bathymetry
Heat transfer
Stratagraphic formation
Magnetic anomaly
48. Coarse pyroclastic debris - apple to refrigerator-sized fragments. Chunks of preexisting igneous rock or large lava blobs which discharge from volcanic eruptions.
Lapilli
Volcanic blocks/bombs
Rhyolitic lava flows
Assimilation
49. The base of the soil profile; consists of material derived from the substrate that's been chemically weathered and broken apart - but has not yet undergone leaching or accumulation.
Clastic
C-horizon
Shield volcano
Area of igneous activity
50. Type of sedimentary soil/rock; Calcite in a pedocal soil accumulates in the B-horizon and may cement soil together - creating this solid mass.
Divergent plate boundary
Turbidity current
Five steps of clastic sedimentary rock formation
Caliche
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