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Creep
Rock and debris avalanches
Debris flows
Lahars
Slump
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Creep
Rock and Debris Avalanches
Debris flows
Lahars
Slump
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Creep
Rock and Debris Avalanches
Debris flows
Lahars
Slump
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Creep
Rock and Debris Avalanches
Debris flows
Lahars
Slump
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The transportation of earth materials from slopes to river systems.
The reduction of steep topographic features to more gravitationally stable slopes.
The widening of canyons and valleys
All of the above
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Increasing the downslope force.
An increase in water saturation
An increase in the resistance or friction force
Increasing the angle of a slope
A reduction in the resistance or friction force.
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A) Saturation of sediments with water adds weight to slopes.
B) The addition of water along a plane of weakness between layers reduces friction.
Water forces grains of sediment apart allowing them to slide past one another
Only a and b
All of the above
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Slump
Earth Flow
Debris flow
Rockslide
Rok fall
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Earth flow
Slump
Debris flow
Creep
Rockslide
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Protons and electrons
Protons and neutrons
Protons, neutrons, and electrons
Only electrons
Only neutrons
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The number of protons in an atom
The number of electrons in an atom
The number of neutrons in an atom
The number of protons and neutrons in an atom
The number of electrons and neutrons in an atom
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Atoms with different numbers of protons.
Atoms of the same element with different numbers of electrons.
Atoms the are radioactive due to unstable nuclei.
Atoms of the same element with different chemical properties.
Atoms of the same element with different numbers of neutrons.
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An imbalance of electrical charge that results from the from the presence of excess electrons in the electron cloud of an atom.
The strong nuclear force being overcome by the repulsive electrical force between protons - usually caused by an imbalance of protons and neutrons.
The breaking of chemical bonds in which a large quantity of thermal energy is released into the surrounding environment.
The strong nuclear force exceeding the repulsive electrical force between the nuclenons of an atom
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High speed electrons emitted by an unstable atomic nucleus.
Particles consisting of 2 protons and 2 neutrons emitted by and unstable atomic nucleus.
A single neutron emitted by an unstable atomic nucleus.
A high ferquency form of electromagnetic radiation emitted by an unstable atomic nucleus
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Alpha particles.
Beta Particles
Gamma Rays
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Remains unchanged
Increases by 2
Decreases by 2
Increases by 4
Decreases by 4
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A measure of the rate of decay for a radioactive isotope.
Is the time required for half of an original quantity of an isotope to decay.
Is not constant and may vary significantly due to environmental conditions.
Can be calculated at any given moment by measuring the rate of decay of a known quantity using a radiation detector.
The length of a half-life is different for different isotopes.
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Determining the ages of organic materials in the very recent geological past (within the last 1000,000 years).
Determining the ages of deposition for sedimentary rocks.
Determining the ages of fossilized remains of plant life that are millions of years old.
Determining the ages of igneous and metamorphic rocks that are millions of years old.
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0 g
20 g
5 g
10 g
13.3 g
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17,280 years
5,760 years
720 years
1,920 years
11,520 years
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100 million years
3.8 billion years
4.5 million years
4.5 billion years
462 million years
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All of the Earth's surface was formed by cataclysmic events in a brief period of time.
The Earth's surface was shaped by processes that have operated over vast spans of time and these same processes can still be observed at the present.
The natural processes operating today were occurring at much more rapid rates in the geological past and are now becoming very gradual.
The present landscape was formed by processes that operated only in the geologic past and the Earth's surface is no longer changing
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All layers of sedimentary rock are generally deposited in a horizontal position.
All layers of sedimentary rock are deposited uniformly over a large area and at a constant rate over geological time
In an undeformed sequence of sedimentary rocks, each bed is younger than the one above it and older than the one below.
In an undeformed sequence of sedimentary rocks, each bed is older than the one above it and younger than the one below.
An igneous intrusion or fault that cuts through preexisting rock is younger than the rock through which it cuts.
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Horizontal Layers of sedimentary rock are deposited on tilted or folded layers.
An igneous intrusion has invaded horizontal layers of sedimentary rock and contains inclusion of those units.
There is and erosion surface between horizontal layers of rock representing a gap in the geological record.
Younger sedimentary rock layers are deposited directly on ancient igneous and metamorphic rocks.
Cenozoic
Mesozoic
Paleozoic
Precambrian
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Cenozoic
Mesozoic
Paleozoic
Precambrian
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Cenozoic
Mesozoic
Paleozoic
Precambrian
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Cenozoic
Mesozoic
Paleozoic
Precambrian
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Cenozoic
Mesozoic
Paleozoic
Precambrian
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Cenozoic
Mesozoic
Paleozoic
Precambrian
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True
Fals
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Very slow sedimentation rates and abundant oxygen.
The presence of high temperatures and high pressures.
Rapid burial and the possession of hard parts such as bones or shells.
Very warm temperatures and abundant moisture.
Oreganisms must be large in size and must be rapidly buried.
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Fossils can tell us what the climate of a region was like in the past.
Fossils can tell us whether or not a region was covered by and ocean in the past.
Fossils document how life has evolved from simpler forms in the oldest fossil-bearing rocks to more complex forms of life found in more recent rock formations.
Fossil organisms reveal that some species become extinct and new ones appear.
Fossils have documented that the complex forms of animal life that we see today are also found in the oldest rocks indicating that life has changed very little over geologic time.
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A substance made of molecules that are composed of only one type of atom.
A substance formed only from covalent bonds.
A substance in which atoms of two or more different elements are chemically bonded.
A substance formed only form ionic bonds.
A substance that is organic in compostion.
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Chemical change
Physical change
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The nuclei of two separate atoms are combined or split, forming new atoms.
An unstable atomic uncleus emits radiation.
The state of matter of a substance is changed from a solid to liquid.
Protons are shared or transferred between the nuclei of separate atoms.
Valence electrons in the outermost shells are transferred or shared between atoms.
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Exothermic
Endothermic
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True
Fals
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Increasing the temperature.
Increasing the concentrations of reactants.
Using a catalyst.
Reducing the temperature.
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The nucleii of the atoms (mass) of gasoline are converted into pure energy during nuclear reactions according to E=mc 2.
During combustion reactions, mass can actually be destroyed and will no longer exist.
The atoms (mass) of gasoline are rearranged and converted into exhaust fumes.
Internal combustion engines have not yet been designed to conserve mass and therefore gasoline will disappear over time.
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The temperature or average thermal energy of material.
The amount of energy released or absorbed during a chemical or physical change.
The rate of a chemical reaction
The conservation of mass.
The degree to which energy has become dispersed.
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Exothermic reactions, because they increase entropy.
Endothermic reactions, because they increase entropy.
Exothermic reactions, because they decrease entropy.
Endothermic reactions, because they decrease entropy.
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Gabbro Dike
Tyee formation
Siletz River Formation
River Terrace sediments
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Gabbro Dike
Tyee Formation
Siletz River Formation
River Terrace Sediments
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Angular Unconformity
Disconformity
Nonconformity
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The same age as the Siletz River Formation and older than the River Terrace Sediments.
Older than the River Terrace Sediments and younger than Tyee Formation.
Older than the tyee formation and younger than the Siletz River formation
Younger than all of the geologic unicts in the diagram.
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High speed electrons emitted by an unstable atomic nucleus.
Particles consisting of 2 protons and 2 neutrons emitted by and unstable atomic nucleus.
A single neutron emitted by an unstable atomic nucleus.
A high ferquency form of electromagnetic radiation emitted by an unstable atomic nucleus
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Horizontal Layers of sedimentary rock are deposited on tilted or folded layers.
An igneous intrusion has invaded horizontal layers of sedimentary rock and contains inclusion of those units.
There is and erosion surface between horizontal layers of rock representing a gap in the geological record.
Younger sedimentary rock layers are deposited directly on ancient igneous and metamorphic rocks.
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