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Total questions: 41
Worksheet time: 24mins
The largest intervals of geologic time and are hundreds of millions of years in duration.
Era
Eon
Epoch
Period
Estimate whether an object is younger or older than other things found at the site.
The geologic time scale
Radiocarbon dating methods
Absolute dating methods
Relative dating methods
Is the acquisition and transportation of rock debris by geomorphic agents like running water, the wind, waves etc.
Erosion
Deposition
Aborasion
Frost wedging
Is the laying down of sediment carried by wind, water or ice, Sediments can be transported as pebbles, sand & mud, or as salts dissolved in water.
Deposition
Erosion
Oxidation
Dissolution
The breaking down or dissolving of rocks and minerals on the surface of the Earth. Water, ice, acids, salts, plants, animals, and changes in temperature are all agents of weathering.
Gradation
Wedging
Weathering
Hydrolysis
Also called mass wasting, includes all processes by which soil and rock materials are dislodged and transported downslope under the direct application of gravitational stresses.
Fast Movements
Sudden Movements
Mass Movements
Slow Movements
The movement of solid materials in the crust could take up to hundreds and millions of years in duration and could affect relatively large areas.
Fast Movements
Mass Movements
Slow Movements
Sudden Movements
Plants and animals as agents of mechanical weathering.
Dissolution
Industrial waste
Biological Activity
Abrasion
Built through forces of tension.
Fault Mountains
Monocline
Syncline
Fold Mountains
The most abundant among the groups of minerals contains chemical elements such as silicon and some aluminum.
Non-Metallic Minerals
Metallic Minerals
Siliceous Minerals
Substances that contain carbonates and other compounds or native elements of sulfur.
Non-mettalic Minerals
Metallic Minerals
Siliceous Minerals
Substances that usually have shiny appearance.
Non-mettalic Minerals
Siliceous Minerals
Metallic Minerals
Another type of fossil fuel formed from organic matter from dead marine plants and animals
(a)
Energy generation through wastes produced by living or once-living organism.
(a)
This layer is consist mostly organic material upper portion is plant litter and other organic debris that are still recognized
Q Horizon
A Horizon
B Horizon
C Horizon
E Horizon
Has large mineral matter where biological activity is high and humus is present.
Q Horizon
A Horizon
B Horizon
C Horizon
E Horizon
light - colored layer that contains the little organic matter.
Q Horizon
A Horizon
B Horizon
C Horizon
E Horizon
When minerals removed from E horizon by eluvation is deposited in horizon called zone of accumulation
Q Horizon
A Horizon
B Horizon
C Horizon
E Horizon
Most tress produce a ring of new wood annually; archeologist use the variations in cross-sections of wood to produce timelines.
Archaeomagnetic dating
Dendrochronolgy
Fission-track dating
Radiocarbon dating
A technique that analyzes how much of the chemical fluorine has been absorbed by bones from the surrounding soils to determine how long the specimen has been underground
Stratigraphy
Fluorine dating
Seriation
A combustible black or brownish-black sedimentary rock usually occurs in rock strata.
(a)
When water gets inside the joints, alternate freezing and thawing episode pry the rock apart.
Salt crystal growth
Frosting
Frost wedging
Abrasion
Waste generated from the exploitation of mineral resources
Biomedic waste
Industrial waste
Mining waste
Agricultural waste
Waste released from manufacturing plants, such as chemical plants, cement production, textile industries, power plants, etc
Industrial waste
Agricultural waste
Mining waste
Biomedic waste
Measure the decay of the radioactive isotope Carbon-14 (C-14).
Dendrochronolgy
Radiocarbon Dating
Fission-track dating
Archaeomagnetic dating
Magnetic particles in most materials of geological origin. such as rocks and clay. are analyzed to track shifts in the Earth's magnetic field over time.
Fission-track dating
Archaeomagnetic dating
Radiocarbon dating
Dendrochronology
The subdivisions of eon.
(a)
Subdivision of eras. the events that bound the periods are widespread in their extent but are not as significant as those which bound the eras.
(a)
The periods of the Cenozoic are frequently subdivide into epochs.
(a)
Distribution of mid-ocean ridges and depth of the seafloor.
Distribution of submarine earthquakes
Distribution seafloor topographic
Sediment thickness
Composition of oceanic crust
Consists primarily of basalt.
Composition of oceanic crust
Distribution of seafloor topographic features
High heat flow along mid-ocean ridges axes
Distribution of submarine earhquakes
Occur along spreading centers where plates are moving apart and new crust is created by magma pushing up from the mantle.
Divergent Boundaries
Convergent Boundaries
Transform Boundaries
Zone between two plates sliding horizontally past one another.
Divergent Boundaries
Convergent Boundaries
Transform Boundaries
A technique that was common in the mid-20th century.
Stratigraphy
Seriation
Fluorine dating
Allows archeologists to construct a relative chronological sequence from the oldest to youngest layer
Stratigraphy
Seriation
Fluorine dating
Determine the age of pottery or ceramics, it can be used to date specific heating event in the past.
Radiocarbon Dating
Thermoluminescence
Fission- track dating
Archeomagnetic dating
Fuels formed by natural processes such as the anaerobic decomposition of buried dead organisms.
(a)
Change in the composition of minerals when they react with water.
Hydrolysis
Oxidation
Dissolution
Reaction between minerals and oxygen dissolved in water.
Hydrolysis
Oxidation
Dissolution
Dissociation of molecules into ions; common includes dissolution of calcite and salt.
Hydrolysis
Oxidation
Dissolution
The weathering away of rocks by constant collision of loose particles.
Salt crystal growth
Abrasion
Biological activity
Frost - wedging
