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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. Sublayer of the mantle - depth of 660km.
Upper mantle
Glass
Asthenosphere
Bathymetry
2. Mineral class; the anion within these types of minerals is a halogen ion (such as chlorine or fluorine).
Divergent plate boundary
Halides
Zone of leaching
Soil erosion
3. 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
Transition zone
Relative plate velocity
Why magma rises
Mantle
4. The layering nature of sedimentary rocks - surface features of layers formed during deposition - and the arrangement of grains within layers.
Volcanic pipes/necks
Biomineralization
Sedimentary structure
Oxides
5. Fracture type; smoothly curving - clamshell-shaped surfaces; typically formed in quartz.
Explosive eruptions
Conchoidal fractures
Effusive eruptions
C-horizon
6. The absorption of water into the crystal structure of minerals - causes some minerals to expand.
Sulfides
Geothermal gradient
Hydration
Bathymetry
7. The process by which sediment settles out of the transporting medium.
Deposition
Biochemical sedimentary rocks
Extrusive igneous rock
Crystalline
8. Along much of the perimeter of the Pacific Ocean - the ocean floor reaches astounding depths of 8-12km. These areas define elongate troughs - and they border volcanic arcs - the curving chains of active volcanoes.
3.5km (2 miles)
Deep-ocean trenches
Mineral
Basaltic lava flows
9. A reference to the supposed position of the Earth's magnetic pole at a time in the past.
Compaction
Rock composition
Hardness
Paleopole
10. A naturally occurring solid - formed by geologic processes - has a crystalline structure and a definable chemical composition - and is generally inorganic.
Zone of leaching
Hydrolysis
Deposition
Mineral
11. 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
Plate tectonics
Outcrop
Basalt
12. 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.
Pangaea
Glassy igneous rocks
Asthenosphere
Lithosphere
13. 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 -
Abyssal plains
Soil
Transform plate boundary
Mid-ocean ridges
14. 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
Dike
Loam
Outer core
Felsic - intermediate - mafic - ultramafic
15. 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.
Euhedral crystal
Transform plate boundary
C-horizon
Color
16. An ultramafic rock with large grains. intrusive - phaneritic igneous rock.
Lava domes
Peridotite
Continental drift evidence
Rhyolitic lava flows
17. 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.
Hardness
Agrillaceous rocks
Stoping
Assimilation
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.
Melts
atmospheres (atm)
Glass
Bedding
19. 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.
Mafic
Magnetic declination
Silicate minerals
Siltstone and mudstone
20. 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.
Sill
Pyroclastic debris
Effusive eruptions
Convergent plate boundary
21. Highest soil horizon; consists almost entirely of organic matter and contains barely any mineral matter. Surface level has 'litter' and deeper it contains 'humus'. Part of the zone of leaching.
Physical weathering
O-horizon
Basaltic composition
Mantle
22. 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
3.5km (2 miles)
Metals
Viscosity
The core
23. Occurs within the asthenosphere - actively drags plates along and attributes partially for the mechanism shifting the plates along the Earth's surface.
Luster
Quartz sandstone
Convective flow
Five steps of clastic sedimentary rock formation
24. Places where intrusive igneous rock creates tabular intrusions cutting across rock that does not have layering - this nearly vertical - wall-like tabular intrusions is formed. Cut across layering within the earth.
Asthenosphere
Dike
Chemical sedimentary rocks
Physical weathering
25. Layering in metamorphic rocks.
Oxidation
Subsidence
The effect of the environment on eruptive style
Metamorphic foliation
26. Process where a convergent boundary ceases to exist when a piece of buoyant lithosphere - such as a continent or island arc - moves into the subduction zone. Yield some of the most spectacular mountains/mountain ranges on the planet including the Him
650-1100 degrees C
Rhyolitic lava flows
collision
Oxidation
27. A name for any kind of unconsolidated debris that covers bedrock. Includes both soil and accumulations of sediment that have not evolved into soil.
Oxidation
Regolith
Physical weathering
Asthenosphere
28. 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.
Depositional environment
Redbeds
Quartz sandstone
Bathymetry
29. A sedimentary bed that has developed a reddish color. The red comes from a film of iron oxide (hematite) that forms on grain surfaces.
Apparent polar-wander path
Regression
Basaltic magma
Redbeds
30. Measure of pressure or push in units of force - per unit area. 1 atm = 1.04 kilograms per square centimeter.
Deposition
Plate tectonics
Subduction
atmospheres (atm)
31. 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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32. 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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33. Rocks that consist of mineral crystals that intergrow when the melt solidifies - interlocking structure. Examples - granite and rhyolite.
Mantle
Crystalline
Subduction
Crystalline igneous rocks
34. 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.
Divergent plate boundary
Laccolith
Carbonate rocks
Fracture zones
35. Cause of melting; when magma rises up from the mantle into the crust - it brings heat with it which raises the temperature of the surrounding crustal rock - and in some cases melting occurs.
Rock texture
Cementation
Heat transfer
Hydration
36. A submarine suspension of sediment.
Ash
Dipole
Ultramafic
Turbidity current
37. Magma type; contains about 52% to 66% silica. Name indicates that these magmas have a composition between that of felsic and mafic magma.
Slab-pull force
650-1100 degrees C
Plutons
Intermediate
38. 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).
rifting
Silicate minerals
Crystalline
Ash
39. 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.
Color
Why magma rises
Dolostone
Continental rift
40. The compiled data from many marine cruises which defined a distinctive - striped and alternating bands of paleomagnetism.
Transition zone
Marine magnetic anomaly
Continental shelf
Convective flow
41. Rocks which develop when hot molten rock cools and freezes solid.
Igneous rocks
Crystal
Organic sedimentary rocks
Thermal expansion
42. Sedimentary rock consisting of cemented together solid fragments and grains derived from preexisting rocks.
Clastic sedimentary rocks
Soil erosion
Phreatomagmatic eruptions
Sulfates
43. Type of rock; accumulated sand bars - within are mineral grains of quartz and feldspar - this sediment if buried and lithified.
Hydration
Luster
Arkose
Abyssal plains
44. Physical features of the land surface represented by changes in elevation.
Topography
Transform fault
Sulfides
Dunes
45. 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.
Root wedging
Basaltic lava flows
Mantle
Apparent polar-wander path
46. 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
Lithosphere
Convergent plate boundary
Chemical weathering
Apparent polar-wander path
47. Refers to the arrangement of grains in a rock; that is - the way the grains connect each other and whether inequant grains are aligned parallel to one another.
Magma mixing
Rock texture
Dipole
Reason for Earth's internal heat
48. A vent at Which melt from inside the Earth spews onto the planet's surface. Erupt.
Sedimentary structure
Volcano
Special properties of minerals
Siltstone and mudstone
49. Process occurring after sediment has been compacted - can then be bounded together to make coherent sedimentary rock. Binding material consists of minerals (commonly quartz or calcite).
Continental drift hypothesis
Cementation
Upper mantle
Flood basalts
50. 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
Explosive eruptions
Xenolith
Continental drift evidence