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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. Successive turbidity currents deposit successive graded beds - creating this sequence of strata.
Rock layering
Turbidite
Assimilation
Crystalline
2. 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
3. A linear belt in which continental lithosphere pulls apart - the lithosphere stretches horizontally.
Source rock composition
Continental rift
Melts
Facets
4. Clast size - clast composition - angularity and sphericity - sorting - and character of cement.
Biochemical sedimentary rocks
Factors classifying clastic sedimentary rocks
Glass
Laterite
5. The distance that the world's deepest mine-shaft penetrates into the Earth beneath South Africa.
Geothermal gradient
3.5km (2 miles)
Limestone
Streak
6. Actively slipping segment of a fracture zone between two ocean ridge segments - these faults make a third type of plate boundary - transforms.
Crystalline
Transform fault
Specific gravity
Sill
7. A single layer of sediment or sedimentary rock with a recognizable top and bottom.
Dipole
Bed
Rock layering
Continental rift
8. Rock made by the freezing of magma underground - after it has pushed its way (intruded) into preexisting rock of the crust.
Cementation
Root wedging
Intrusive igneous rock
Fragmental igneous rocks
9. 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.
Specific gravity
Biochemical sedimentary rocks
Cinder cone
Sandstone
10. Distinguishing feature of magma; the process where different magmas formed in different locations from different sources may come in contact within a magma chamber prior to freezing. Thus the originally distinct magmas mix to create a new - different
Gabbro
Effusive eruptions
Magma mixing
Magnetic reversals
11. A sedimentary bed that has developed a reddish color. The red comes from a film of iron oxide (hematite) that forms on grain surfaces.
Plate tectonics
Turbidity current
Redbeds
Granite
12. 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
Factors classifying clastic sedimentary rocks
collision
Halides
Sulfates
13. Physical property of a mineral; refers to the shape (morphology) of a single crystal with well-formed crystal faces - or to the character of an aggregate of many well-formed crystals that grew together as a group. Depends on the internal arrangement
Rocks
Crystal habit
Deep-ocean trenches
Hydrolysis
14. 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.
Sedimentary structure
Continental drift evidence
Batholiths
Siliceous rocks
15. 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.
Large Igneous Provinces (LIPs)
Assimilation
Relative plate velocity
Abyssal plains
16. Mineral group; feldspars - quartz - muscovite - clay minerals.
Metamorphic foliation
Root wedging
Convergent plate boundary
Light silicates
17. Chemical weathering during Which minerals dissolve into water.
Dissolution
Composite cone (stratovolcano)
Shield volcano
Glassy igneous rocks
18. The force that subducting plates apply to oceanic lithosphere at a convergent boundary - arises simply because lithosphere formed 10 million years ago is denser than asthenosphere - so it can sink into the asthenosphere. Thus once an oceanic plate st
Slab-pull force
Igneous rocks
Dolostone
Polymorphs
19. 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.
20. Refers to the chemical reactions that alter or destroy minerals when rock comes in contact with water solutions or air.
Fracture zones
Fracture and cleavage
Chemical weathering
Conchoidal fractures
21. A reference to the sinking of the lithosphere; allows for sediment to accumulate in regions where this occurs.
Conchoidal fractures
Zone of leaching
Subsidence
Granitic composition
22. Mineral group; olivine group - pyroxene group - amphibole group.
Dark Silicates
Crystal structure
The effect of the environment on eruptive style
Transform fault
23. Mineral crystal formation type; form from a solidification of a melt - meaning the freezing of a liquid.
Melting
Dike
Crust
Sulfates
24. Built up deposit of volcanic bombs and lapilli - known as volcanic agglomerate.
Flood basalts
Tuff
Quartz sandstone
Large Igneous Provinces (LIPs)
25. Type of sedimentary rock; rocks whose grains are stuck together by cement.
Bedding
Soil erosion
Topography
Clastic
26. 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
Effusive eruptions
Divergent plate boundary
Ultramafic
Granite
27. Physical property of a mineral; refers to the way a mineral surface scatters light. Metallic versus non-metallic in nature.
Luster
Magnetic reversals
Viscosity
Batholiths
28. 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.
Basaltic lava flows
Composite cone (stratovolcano)
Limestone
Deep-ocean trenches
29. Forms from a chemical reaction between solid calcite and magnesium-bearing groundwater.
Dolostone
Crust
Mineral crystal destruction
Effusive eruptions
30. 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.
Magnetic inclination
Transported soil
Light silicates
Euhedral crystal
31. Rock formations still attached to the Earth's crust.
Magnetic inclination
Bedrock
Viscosity
Sedimentary structure
32. The transformation of loose sediment into solid rock.
Magnetic reversals
Rock-forming silicate minerals
Light silicates
Lithification
33. A layer of sediment in which grain size varies from coarse at the bottom to fine at the top.
Graded bed
Lithification
Carbonates
Rock-forming silicate minerals
34. 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 -
Caliche
Mid-ocean ridges
Volcanic pipes/necks
Weathering
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.
Heat transfer
3.5km (2 miles)
Hydration
Cement
36. The process by which sediment settles out of the transporting medium.
Luster
Columnar jointing
Deposition
Soil
37. Heat from an intense surface fire bakes and expands the outer layer of the rock. On cooling - the layer contracts - causing the outer part of the rock spall - or break off in sheet-like pieces.
Topography
Xenolith
Bed
Thermal expansion
38. A felsic rock with large grains. Intrusive - phaneritic igneous rock.
Conchoidal fractures
Glass
Granite
Subduction
39. Mineral crystal formation type; form by type of diffusion - the movement of atoms or ions through a solid to arrange into a new crystal structure; process takes place very slowly.
Soil Horizons
Metamorphic foliation
Solid-state diffusion
Salt wedging
40. Molten rock that has flowed out onto Earth's surface.
Lava
Rock texture
Rocks
Plates
41. Solids composed of metal atoms (such as iron - aluminum - copper - and tin). Within this type of solid - outer electrons are able to flow freely.
Plates
Rocks
Metals
Volcanic pipes/necks
42. A sediment-filled depression; in an area where the lithosphere has subsided.
Crystalline
Sedimentary Basins
Regolith
Lithification
43. 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.
Inner core
Transition zone
Compaction
Basaltic magma
44. When different rocks in an outcrop undergo weathering at different rates.
a'a'
Oxides
Differential weathering
Hardness
45. Volcanic landform; bulbous mass of congealed lava - associated with explosive eruptions of gas-rich magma.
Oxides
Magma's speed of flow
Coal
Lava domes
46. Type of igneous rock composition; composed of light-colored silicates - very rich in felsic (feldspar and silica). Major constituent of continental crust.
Gem
Dissolution
Cinder cone
Granitic composition
47. The distance of the deepest well ever drilled - hole in northern Russia. Penetrates only about 0.03% of the Earth.
Root wedging
Felsic
C-horizon
12km
48. A cut and finished stone ready to be used in jewelry. Examples - diamond - ruby - sapphire - emerald.
Gem
Rhyolitic lava flows
Convergent plate boundary
Limestone
49. Irregular or blob-shaped intrusions that range in size from tens of meters across to tens of kilometers across.
Evaporites
Plutons
Paleopole
Laccolith
50. Weathering - erosion - transportation - deposition - and lithification.
The effect of the environment on eruptive style
Lava tube
Diagenesis
Five steps of clastic sedimentary rock formation