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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. Relatively small - elongated ridges that form on a bed surface at right angles to the direction of the current flow of the rock.
Ripples
Biomineralization
Basaltic lava flows
Earth's atmosphere
2. 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.
Laterite
Oxides
Rocks
Magnetic declination
3. The intrusion of numerous plutons in a region - produces a vast composite body that may be several hundred kilometers long and over 100km wide; an immense body of igneous rock.
Grain sizes
Batholiths
Siltstone and mudstone
Fractional crystallization
4. 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.
Basaltic composition
Magnetic declination
Strata
Special properties of minerals
5. 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.
Rock-forming silicate minerals
Alloy
Pyroclastic debris
Jointing
6. Sedimentary rock composed of clay.
Hydrosphere
Agrillaceous rocks
Stoping
Superplumes
7. Sedimentary rock composed of calcite or dolomite.
Carbonate rocks
Magnetic inclination
Soil Horizons
Tuff
8. Volcanic landform; bulbous mass of congealed lava - associated with explosive eruptions of gas-rich magma.
Topography
Siliceous rocks
Calderas
Lava domes
9. Successive turbidity currents deposit successive graded beds - creating this sequence of strata.
Oxidation
Silicates
Sill
Turbidite
10. 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.
Frost wedging
Precipitation
Sulfides
Subduction
11. Sedimentary rocks consisting of carbon-rich relicts of plants.
Calderas
Magma mixing
Crust
Organic sedimentary rocks
12. Magma type; contains about 52% to 66% silica. Name indicates that these magmas have a composition between that of felsic and mafic magma.
Intermediate
Five steps of clastic sedimentary rock formation
Explosive eruptions
Hydrosphere
13. A linear belt in which continental lithosphere pulls apart - the lithosphere stretches horizontally.
Rock-forming silicate minerals
Frost wedging
Volcanic blocks/bombs
Continental rift
14. Rock formations still attached to the Earth's crust.
Grain sizes
Lithosphere
Bedrock
Weathering
15. 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.
Marine magnetic anomaly
Facets
Transform plate boundary
Apparent polar-wander path
16. 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
Bedrock
E-horizon
O-horizon
Coal
17. 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
Inner core
The core
Depositional environment
Magnetic reversals
18. Type of sedimentary soil/rock; Calcite in a pedocal soil accumulates in the B-horizon and may cement soil together - creating this solid mass.
Partial melting
Deep-ocean trenches
Precipitation
Caliche
19. Blocks of rock that are solid and durable but composed of rough quartz sand grains cemented together.
Dike
Basalt
Sandstone
Soil Horizons
20. An organic sedimentary rock; black - combustible rock consisting of over 50% carbon.
Continental drift evidence
Pangaea
Coal
Specific gravity
21. Unconsolidated deposits of pyroclastic grains - regardless of size - that have been erupted from a volcano constitute these pyroclastic deposits.
Volcano
Composite cone (stratovolcano)
Tephra
Special properties of minerals
22. The broad - relatively flat regions of the ocean that lie at a depth of about 4-5km below sea level.
Abyssal plains
Lava
Volcanic blocks/bombs
Sedimentary Basins
23. The record of paleomagnetism revealed that the location of Earth's magnetic poles had been changing through geologic time. This 'wandering' meant that Earth's magnetic poles do not move with respect to fixed continents. Rather - continents move relat
Asthenosphere
C-horizon
Apparent polar-wander path
Rock texture
24. 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.
Organic chemicals
Metamorphic rocks
Magma's speed of flow
Granitic magma
25. Similar to ripples - but are much larger. Small ripples often form on the surface of these structures.
Dunes
Heat transfer
Light silicates
Mantle plume
26. The most important mineral group; comprise the most rock-forming minerals - they are very abundant due to large % of silicon and oxygen in Earth's crust. Examples - oxygen - silica - aluminum.
Heat transfer
Light silicates
Hardness
Rock-forming silicate minerals
27. Lava flowing on dry land cools more slowly that lava erupting underwater.
The effect of the environment on eruptive style
Siliceous rocks
Facets
Magma mixing
28. 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.
Dike
Halides
Ripples
Assimilation
29. When different rocks in an outcrop undergo weathering at different rates.
Differential weathering
B-horizon
Coal
Chemical weathering
30. Mineral crystal formation type; from directly from a vapor - occurs around volcanic vents or around geysers. At such locations - volcanic gases or steam enter the atmosphere and cool - so certain elements cannot remain in gaseous form.
Fumerolic mineralization
Regolith
Flood basalts
Special properties of minerals
31. 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.
Physical weathering
Oxides
Deep-ocean trenches
Soil Horizons
32. 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
Crystal
Rocks
Crust
Dipole
33. Type of lava flow; higher silica content - greater viscosity - forms a large mound above the vent out of a volcano.
Transported soil
Andesitic lava flows
Native metals
Glass
34. A vent at Which melt from inside the Earth spews onto the planet's surface. Erupt.
Transform fault
Crystal
Volcano
Zone of leaching
35. Physical property of a mineral; refers to the way a mineral surface scatters light. Metallic versus non-metallic in nature.
Thermal expansion
Sedimentary structure
Earth's atmosphere
Luster
36. The resistance to flow of magma. Reflects its distinct silica content - for silica tends to polymerize - meaning it links up to form long - chainlike molecules whose presence slows down the flowing ability of magma. Thus felsic magmas flow less easil
Lava
Basalt
a'a'
Viscosity
37. Type of lava flow; the most viscous of any lava flow because it is the most silicic and the coolest in nature. Tends to accumulate in a lava dome above the vent or in short and bulbous flows 1 to 2 km long.
Flood basalts
Strata
Rhyolitic lava flows
Tephra
38. A cut and finished stone ready to be used in jewelry. Examples - diamond - ruby - sapphire - emerald.
Conglomerate
Continental shelf
Gem
Silicates
39. The burial and lithification of angular or rounded clasts form these types of rocks.
Conglomerate
Grain sizes
Bedrock
Cinder cone
40. Rocks whose crystals interlock with each other.
Carbonate rocks
Metals
Thermal expansion
Crystalline
41. 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
Mafic
Redbeds
Transgression
42. 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
12km
Convergent plate boundary
Spreading rate
Streak
43. 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
Salt wedging
Glass
Dunes
Flood basalts
44. 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.
Dissolution
The effect of gas pressure on eruptive style
Asthenosphere
Regression
45. A single layer of sediment or sedimentary rock with a recognizable top and bottom.
rifting
Bed
3.5km (2 miles)
Weathering
46. 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
Marine magnetic anomaly
Silicates
Pyroclastic flows
Transform fault
47. Iron (35%) - oxygen (30%) - silicon (15%) - and magnesium (10%) - and the remaining 10% consists of 88 naturally occurring elements.
Elemental composition of Earth
Continental drift evidence
Residual soil
Shield volcano
48. The display of the pattern of atoms or ions within a mineral. Meaning that the shape of one part of a mineral is a mirror image of the shape of another part.
Oxides
Granitic composition
Continental shelf
Symmetry
49. Sedimentary rocks made up of minerals that precipitate directly from water solutions.
Polymorphs
Chemical sedimentary rocks
Basaltic magma
Abyssal plains
50. A mineral's growth that is uninhibited - has well-formed crystal faces.
Euhedral crystal
Glass
Mid-ocean ridges
Quartz sandstone