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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 distance that the world's deepest mine-shaft penetrates into the Earth beneath South Africa.
Fractional crystallization
Intrusive igneous rock
Solid-state diffusion
3.5km (2 miles)
2. Type of volcano; broad and slightly domed - primarily made of basaltic lava - large and erupt large volumes of lava. Form from either low viscosity basaltic lava or from large pyroclastic sheets.
Light silicates
Weathering
Shield volcano
Alloy
3. 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.
Agrillaceous rocks
Phreatomagmatic eruptions
Fracture zones
Relative plate velocity
4. Deeper sublayer of the mantle - depth of 660km to 2900km.
Subsidence
Alloy
Continental rift
Lower mantle
5. Mineral crystal formation type; form from a solution - meaning that atoms - molecules - or ions dissolved in water bond together out of water.
Oxidation
Dolostone
Mafic
Precipitation
6. A fine spray of lava instantly freezes to form fine particles of glass.
C-horizon
Luster
Plates
Ash
7. The removal of soil by running water or by wind.
Soil erosion
Peridotite
Extrusive igneous rock
Bedding
8. 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.
ravertine
Ultramafic
Soil Horizons
Lithification
9. 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
Dike
Factors of magma cooling time
Silicates
10. 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.
Phreatomagmatic eruptions
Topography
Magnetic reversals
Dolostone
11. Sedimentary rocks consisting of carbon-rich relicts of plants.
Transform fault
Organic sedimentary rocks
Pangaea
Effusive eruptions
12. A reference to the supposed position of the Earth's magnetic pole at a time in the past.
Magma
Glass
Paleopole
Abyssal plains
13. Pea to plum-sized fragments of pyroclastic debris - consists of pumice or scoria fragments.
Pangaea
Lapilli
Volatiles
Thermal expansion
14. Sea-floor spreading proponents - Hess and others realized that in order for the circumference of the Earth to remain constant through time - ocean floor must eventually sink back into the mantle. This sinking process consumes the ocean floor between
Seamount chains
Subduction
Large Igneous Provinces (LIPs)
Regolith
15. 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
Crystal
Regression
Depositional environment
16. Mineral group; feldspars - quartz - muscovite - clay minerals.
Native metals
Light silicates
Magma mixing
Continental shelf
17. 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
Calderas
Intermediate
Factors of magma cooling time
18. Mineral class; the anion within these types of minerals is a halogen ion (such as chlorine or fluorine).
Halides
Jointing
Clastic sedimentary rocks
Earth's atmosphere
19. 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
Zone of leaching
Volatiles
3.5km (2 miles)
20. 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.
Oxides
The effect of the environment on eruptive style
Glass
Ripples
21. 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.
Ignimbrite
Extrusive igneous rock
Siltstone and mudstone
Fumerolic mineralization
22. 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.
Gem
Siltstone and mudstone
Dike
Silicates
23. Layering in sedimentary rocks.
Volcanic pipes/necks
Bedding
Differential weathering
Organic sedimentary rocks
24. The most common minerals in the Earth. Contain silica (SiO2) mixed in varying proportions with other elements (typically iron - magnesium - aluminum - calcium - potassium - and sodium).
Ignimbrite
Dipole
Siliceous rocks
Silicate minerals
25. Mineral class; consist of a metal cation bonded to a sulfide anion. Examples - galena and pyrite. Many have a metallic luster. Can also be considered ores with high proportions of metal within the mineral.
Melts
Sulfides
Salt wedging
Basaltic magma
26. A place where three plate boundaries intersect at a point.
Composite cone (stratovolcano)
Agrillaceous rocks
Volcanic pipes/necks
triple junction
27. Four settings: in volcanic arcs bordering deep-ocean trenches - isolated hot spots - within continental rifts - and along mid-ocean ridges.
Flood basalts
Crystal structure
Area of igneous activity
Shield volcano
28. 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.
Specific gravity
Hot spots
Oxidation
Polymorphs
29. 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.
Coal
Magnetic inclination
Silicates
Granitic magma
30. 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
Fracture zones
Metamorphic rocks
Fractional crystallization
Magnetic reversals
31. Layer that lies below the lithosphere - and is the portion of the mantle in which rock can flow (slowly; 10-15cm per year) despite still being solid. Entirely within the mantle and lies below a depth of 100-150km.
Lower mantle
collision
Asthenosphere
Mafic
32. Materials that easily transform into gas at the relatively low temperatures found at the Earth's surface.
Stratagraphic formation
Volatiles
Color
Silicate minerals
33. 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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34. 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
Deep-ocean trenches
Zone of accumulation
Lava tube
35. Type of lava flow; surface layer of the lava freezes and then breaks up due to the continued movement of lava underneath - becomes a jumble of sharp - angular fragments - yielding a rubbly flow.
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36. Blocks of rock that are solid and durable but composed of rough quartz sand grains cemented together.
Sandstone
Metamorphic foliation
Intrusive igneous rock
Abyssal plains
37. Actively slipping segment of a fracture zone between two ocean ridge segments - these faults make a third type of plate boundary - transforms.
Transform fault
Weathering
Depositional environment
Sea-floor spreading
38. A vent at Which melt from inside the Earth spews onto the planet's surface. Erupt.
Precipitation
Erosion
Volcano
Peridotite
39. The distance of the deepest well ever drilled - hole in northern Russia. Penetrates only about 0.03% of the Earth.
Hydration
Turbidity current
Thermal expansion
12km
40. 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
Source rock composition
Dolostone
Felsic - intermediate - mafic - ultramafic
Fumerolic mineralization
41. Type of soil; forms in tropical regions where abundant rainfall drenches the land during the rainy season - and the soil dries during the dry season.
Mineral
Why magma rises
pahoehoe
Laterite
42. Core division; between 2900 and 5155km deep. Liquid iron alloy - it exists as a liquid because the temperature here is so high that even the great pressures squeezing the region cannot lock atoms into a solid framework. This liquid iron alloy is able
Rhyolitic lava flows
Outer core
Organic chemicals
Salt wedging
43. 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
Melts
Volatiles
Large Igneous Provinces (LIPs)
Hardness
44. Rocks whose crystals interlock with each other.
Transform fault
Earth's atmosphere
Crystalline
Decompression
45. A sedimentary bed that has developed a reddish color. The red comes from a film of iron oxide (hematite) that forms on grain surfaces.
Redbeds
Chemical weathering
Calderas
Lower mantle
46. Rock formations still attached to the Earth's crust.
Igneous rocks
Silicate minerals
Heat transfer
Bedrock
47. 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.
C-horizon
Differential weathering
Coal
Abyssal plains
48. Chemical weathering during Which minerals dissolve into water.
Frost wedging
Dissolution
Granitic composition
Erosion
49. Type of rock; accumulated sand bars - within are mineral grains of quartz and feldspar - this sediment if buried and lithified.
rifting
Mafic
Erosion
Arkose
50. Mineral crystal formation type; form from a solidification of a melt - meaning the freezing of a liquid.
Melting
Streak
Magnetic declination
Ignimbrite