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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. During the final stages of cooling - lava flows contract and may fracture into roughly hexagonal columns.
Chemical sedimentary rocks
Paleomagnetism
Columnar jointing
Volcano
2. A process occurring when sea level falls - the coast migrates seaward.
Chemical weathering
Regression
Basaltic lava flows
Caliche
3. 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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4. 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
Heat transfer
Inner core
Outer core
Lava
5. When water is trapped in a joint freezes - it forces the joint open and may cause the joint to grow.
Frost wedging
Volcanic blocks/bombs
Precipitation
Lithification
6. Deeper sublayer of the mantle - depth of 660km to 2900km.
Fracture and cleavage
Deep-ocean trenches
Sill
Lower mantle
7. A submarine suspension of sediment.
collision
Turbidity current
Biomineralization
Apparent polar-wander path
8. 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
collision
Slab-pull force
Hot-spot track
Flood basalts
9. 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.
Chemical sedimentary rocks
Paleomagnetism
Agrillaceous rocks
a'a'
10. A column of very hot rock that flows upward until it reaches the base of the lithosphere. In this model - such deep-mantle plumes form because heat rising from the Earth's core is warming rock at the base of the mantle. A possible explanation to the
Oxidation
Factors classifying clastic sedimentary rocks
Mantle plume
Cement
11. Perhaps the cause for the large igneous provinces; formations within the mantle - plumes that bring up vastly more hot asthenosphere than normal plumes.
Superplumes
Dolostone
Hot spots
Silicate minerals
12. An ultramafic rock with large grains. intrusive - phaneritic igneous rock.
Magnetic reversals
Regression
Peridotite
Mantle plume
13. Type of volcano; most are adjacent to the Pacific - larger in size - interbedded lavas and pyroclastics - consist of alternating layers of lava and tephra - most violent type of activity - may produce nuee ardente or lahars.
Sedimentary structure
Coal
Volcanic pipes/necks
Composite cone (stratovolcano)
14. 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
Hardness
rifting
Oxides
Bed
15. Subsoil - ions and clay leached and transported down from above accumulate here. As a result - new minerals form - and clay fills open spaces. Part of the zone of accumulation.
Dark Silicates
B-horizon
Magnetic reversals
Halides
16. Cause of melting; magma can also form at locations where chemicals called volatiles mix with hot mantle rock. Elements such as water and carbon dioxide mix with hot rock - helping to break chemical bonds - so that if you add volatiles to a solid - ho
Sulfates
Frost wedging
atmospheres (atm)
Volatiles
17. A sediment-filled depression; in an area where the lithosphere has subsided.
Sedimentary Basins
Granitic composition
Transition zone
Bedding
18. An organic sedimentary rock; black - combustible rock consisting of over 50% carbon.
Chemical weathering
rifting
Coal
Laterite
19. Center of the Earth - consists mainly of iron alloy.
Carbonates
Conglomerate
The core
Apparent polar-wander path
20. Outer surface level of Earth; composed of granite - basalt - and gabbro. Continental: mostly about 35-40km thick . Oceanic: about 7-10km thick. Oxygen - by far the most abundant element.
Polymorphs
Rhyolitic lava flows
Dolostone
Crust
21. Rocks which develop when hot molten rock cools and freezes solid.
Crystal lattice
Laterite
Igneous rocks
Facets
22. A place where three plate boundaries intersect at a point.
Root wedging
triple junction
Transform fault
Source rock composition
23. 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.
Diagenesis
Dark Silicates
Symmetry
Salt wedging
24. Type of magma; low in silica - fluid - crystallize at high temperatures.
Crystalline
Basaltic magma
Mantle plume
Dolostone
25. Type of rock; accumulated sand bars - within are mineral grains of quartz and feldspar - this sediment if buried and lithified.
Chert
Arkose
Biomineralization
collision
26. 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
Facets
Dipole
Differential weathering
Fractional crystallization
27. Volcanic landform; pipes are short conduits that connect a magma chamber to the surface.
C-horizon
Gabbro
Volcanic pipes/necks
12km
28. Distinguishing feature of magma; Because not all minerals melt by the same amount under given conditions - and because chemical reactions take place during melting - the magma that forms as a rock begins to melt does not have the same composition as
Mafic
Tuff
Marine magnetic anomaly
Partial melting
29. 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
Fragmental igneous rocks
Continental drift evidence
Divergent plate boundary
Fumerolic mineralization
30. 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.
Melts
Assimilation
Extrusive igneous rock
Source rock composition
31. 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.
Ultramafic
Fissure eruptions/lava plateaus
Limestone
Sulfides
32. 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.
Residual soil
Source rock composition
Volcano
Specific gravity
33. Active hot-spot volcanoes commonly occur at the end of a chain of dead volcanoes.
Hot-spot track
Extrusive igneous rock
B-horizon
Felsic
34. Type of lava flow; mafic - low viscosity - extremely hot - flows very quickly.
Transform plate boundary
Ridge-push force
Hydrosphere
Basaltic lava flows
35. 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
rifting
Sedimentary Basins
Clastic
36. Relatively small - elongated ridges that form on a bed surface at right angles to the direction of the current flow of the rock.
Basaltic magma
Alloy
Ripples
Carbonate rocks
37. Type of sedimentary rock; rocks whose grains are stuck together by cement.
rifting
Apparent polar-wander path
Root wedging
Clastic
38. Some rock bodies appear to contain distinct formations - defined either by bands of different compositions or textures - or by the alignment of inequant grains so that they trend parallel to one another.
3.5km (2 miles)
Rock layering
Soil
Bedrock
39. Unconsolidated deposits of pyroclastic grains - regardless of size - that have been erupted from a volcano constitute these pyroclastic deposits.
Asthenosphere
Tephra
Granitic magma
Hydrolysis
40. Process that occurs after the sediment has been buried - pressure cause by the overburden squeezes out water and air that had been trapped between clasts - and the clasts press together tightly.
Crystal structure
Plutons
Basaltic lava flows
Compaction
41. The separated lithosphere into distinct pieces. Twelve major 'pieces' and several minor. Consist of active margins and passive margins between them.
Plutons
Continental drift hypothesis
Carbonate rocks
Plates
42. 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
Viscosity
Ignimbrite
Divergent plate boundary
Tephra
43. 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.
atmospheres (atm)
Magma's speed of flow
Organic chemicals
Volcanic pipes/necks
44. 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
Rocks
Physical weathering
Outer core
45. Develops because mid-ocean ridges lie at a higher elevation than the adjacent abyssal plains of the ocean. The surface of the sea floor overall slopes away from the ridge axis. Gravity causes the elevated lithosphere at the ridge axis to push on the
Felsic
Special properties of minerals
Sedimentary Basins
Ridge-push force
46. The distance of the deepest well ever drilled - hole in northern Russia. Penetrates only about 0.03% of the Earth.
12km
Mineral
Granitic magma
Subduction
47. The layering nature of sedimentary rocks - surface features of layers formed during deposition - and the arrangement of grains within layers.
Sedimentary structure
Sulfides
Convergent plate boundary
Andesitic lava flows
48. 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.
Assimilation
Special properties of minerals
The effect of viscosity on eruptive style
Asthenosphere
49. Sedimentary rocks consisting of carbon-rich relicts of plants.
Dark Silicates
Organic sedimentary rocks
Salt wedging
The effect of viscosity on eruptive style
50. Theory confirmed by 1968 - geologists had developed the complete model of continental drift - sea-floor spreading - and subduction. Within this model - Earth's lithosphere consists of about 20 distinct pieces - or plates - that move relative to each
Light silicates
Carbonates
Plate tectonics
Hydrolysis