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Test your basic knowledge |
Geology
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Study First
Subject
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science
Instructions:
Answer 50 questions in 15 minutes.
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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. 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
Turbidite
Graded bed
A-horizon
E-horizon
2. 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
Pyroclastic flows
3.5km (2 miles)
Volcano
3. An insulated - tunnel-like conduit through which lava moves within a flow.
Hot-spot track
Oxides
Lava tube
Ultramafic
4. 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.
Lapilli
Seamount chains
Effusive eruptions
Pyroclastic debris
5. 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.
Melts
Turbidity current
Mantle
Peridotite
6. Volcanoes that exist as isolated points and appear to be independent of movement at a plate boundary - hot-spot volcanoes. Mostly are located on the interior of plates - away from boundaries.
Hot spots
The effect of the environment on eruptive style
Erosion
Sulfates
7. A fine spray of lava instantly freezes to form fine particles of glass.
Ash
Agrillaceous rocks
Xenolith
Hot-spot track
8. An organic sedimentary rock; black - combustible rock consisting of over 50% carbon.
Coal
Grain sizes
Pyroclastic flows
Peridotite
9. A single layer of sediment or sedimentary rock with a recognizable top and bottom.
Bed
Fissure eruptions/lava plateaus
Fragmental igneous rocks
Batholiths
10. Most common mineral on Earth; compose over 95% of the continental crust. Consist of combinations of a fundamental building block called silicon-oxygen tetrahedron - different groups: independent tetrahedra - single chains - double chains - sheet sili
Asthenosphere
Sedimentary Basins
Outcrop
Silicate minerals
11. Forms from a chemical reaction between solid calcite and magnesium-bearing groundwater.
Decompression
Granitic composition
Dolostone
Relative plate velocity
12. Iron (35%) - oxygen (30%) - silicon (15%) - and magnesium (10%) - and the remaining 10% consists of 88 naturally occurring elements.
Melts
Rock composition
Batholiths
Elemental composition of Earth
13. 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
The effect of viscosity on eruptive style
Silicates
Sulfides
Lava
14. If a stoped block does not melt entirely - but rather becomes surrounded by new igneous rock - it becomes this; xeno - meaning foreign.
Agrillaceous rocks
Xenolith
Basaltic magma
Ultramafic
15. 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.
Symmetry
Rock-forming silicate minerals
Zone of accumulation
Carbonate rocks
16. Type of igneous rock composition; composed of light-colored silicates - very rich in felsic (feldspar and silica). Major constituent of continental crust.
Continental rift
Crystalline igneous rocks
Five steps of clastic sedimentary rock formation
Granitic composition
17. A mineral's growth that is uninhibited - has well-formed crystal faces.
Frost wedging
Euhedral crystal
Crystalline igneous rocks
Laccolith
18. 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.
Transgression
Peridotite
Zone of leaching
Cross beds
19. Tree roots that grow into joints can push those joints open in this process.
Regression
Crystal lattice
Root wedging
Rock-forming silicate minerals
20. 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.
Organic sedimentary rocks
Ignimbrite
Silicate minerals
Erosion
21. Type of magma; low in silica - fluid - crystallize at high temperatures.
Basaltic magma
Volcanic blocks/bombs
Volcanic pipes/necks
Felsic - intermediate - mafic - ultramafic
22. 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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23. Elongate submarine mountain ranges whose peaks lie only about 2-2.5km below sea level. Consist of a ridge axis - are roughly symmetrical - and can include escarpments - axial troughs - and valleys. Examples - Mid-Atlantic Ridge - East Pacific Rise -
Mid-ocean ridges
ravertine
A-horizon
Chert
24. Aggregates of mineral crystals or grains - and masses of natural glass; a coherent - naturally occurring solid - consisting of an aggregate of minerals or a mass of glass.
Physical weathering
Rocks
Deposition
Basaltic lava flows
25. 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
Pyroclastic debris
3.5km (2 miles)
Divergent plate boundary
Oxides
26. 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.
650-1100 degrees C
Plutons
Zone of leaching
Crystalline
27. Core division; from a depth of 5155km down to Earth's center at 6371km. A radius of about 1220km - is solid iron-nickel alloy - can reach temperature of 4700 degrees C. Solid in nature because of subjection to greater pressure - keeps atoms from wand
Mineral crystal destruction
Inner core
Glass
Factors of magma cooling time
28. 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.
Magma
Crust
Large Igneous Provinces (LIPs)
Relative plate velocity
29. 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
Dipole
Plutons
Compaction
Fracture zones
30. Chemical weathering during Which minerals dissolve into water.
Relative plate velocity
Carbonate rocks
Siliceous rocks
Dissolution
31. Mineral crystal formation type; form at interfaces between the physical and biological components of the Earth system by this process.
Magnetic anomaly
Zone of accumulation
Biomineralization
Metamorphic foliation
32. Form from grains that break off preexisting rock and become cemented together - or from minerals that precipitate out of a water solution.
Viscosity
Volcanic pipes/necks
Outcrop
Sedimentary rocks
33. Sphere; Surface water along with groundwater - Earth consists of 70% surface water (oceans - lakes - and streams).
Metamorphic foliation
Batholiths
Hydrosphere
Stoping
34. The removal of soil by running water or by wind.
Loam
Soil erosion
Melting
Hydration
35. 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.
Root wedging
Source rock composition
Cementation
Cross beds
36. 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
Columnar jointing
Bed
Salt wedging
Bedding
37. 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.
Siltstone and mudstone
Compaction
Melts
Deposition
38. The four classes of igneous silicate rocks based on the proportion of silicon to iron and magnesium. As the proportion of silicon in a rock increases - the density decreases - thus felsic rocks are less dense than mafic. In order - from greatest to l
Regolith
Mineral
Felsic - intermediate - mafic - ultramafic
Streak
39. Actively slipping segment of a fracture zone between two ocean ridge segments - these faults make a third type of plate boundary - transforms.
O-horizon
Transform fault
Volatiles
12km
40. During this process - water chemically reacts with minerals and breaks them down - working faster in slightly acidic water.
650-1100 degrees C
Geothermal gradient
Biochemical sedimentary rocks
Hydrolysis
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.
Dissolution
Fractional crystallization
Outcrop
3.5km (2 miles)
42. Some rocks develop their magnetization - their ability to produce a magnetic field - at the time that the rocks themselves formed. Such rocks - preserve a record of the Earth's magnetic field at known times in the past.
Cement
Geothermal gradient
Paleomagnetism
Factors of magma cooling time
43. 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.
Transported soil
Soil
Phreatomagmatic eruptions
Bathymetry
44. Fluid basaltic lava extruded from crustal fractures called fissures.
Turbidite
Fissure eruptions/lava plateaus
Plutons
Pangaea
45. 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.
The effect of the environment on eruptive style
Organic chemicals
Cinder cone
Arkose
46. A pluton formation theory; a process during Which magma assimilates wall rock - and blocks of wall rock break off and sink into the magma.
Continental drift hypothesis
Precipitation
Stoping
Polymorphs
47. Perhaps the cause for the large igneous provinces; formations within the mantle - plumes that bring up vastly more hot asthenosphere than normal plumes.
Crystal habit
Outer core
Cinder cone
Superplumes
48. 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
Redbeds
The effect of viscosity on eruptive style
The effect of gas pressure on eruptive style
Glassy igneous rocks
49. 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
Superplumes
Why magma rises
Ripples
triple junction
50. Some minerals have distinctive properties - such as calcite which reacts with dilute hydrochloric acid to produce carbon dioxide. Dolomite also reacts with acid - graphite can make clear markings - magnetite attracts a magnet - halite tastes salty -
Special properties of minerals
Carbonates
Decompression
Mantle