Geology and the Environment - Unit 1 Flashcards
4.6 Billion Years Ago
Planet formed from cloud of gases
3 Billion Years Ago
Earliest life forms preserved in rocks
570 million Years Ago
First abundant organisms with hard skeletal parts appeared in rock record
430 million Years Ago
First land plants appeared
190 million Years Ago
First Mammals Appeared
63 million Years Ago
First primates
2 million Years Ago
First human species
35 Thousand to 50 thousand years ago
Apperance of Homo Sapiens
18th Century
Begining of industrial revolution
20th Century
Advent of the Automobile
1950s
Thermonuclear Weapons were tested frequently
Pesticides became widely used
1960s to present
Increased usage of aerosol sprays
1970s to present
Increased amounts of radioactive wastes
-Require 1/4 million years before they decay to safe levels (More than the lifespan of Humans)
Core
The innermost zone of the earth; composed largely of iron
Crust
The outermost compositional zone of the earth; composed predominantly of relatively low-density silicate materials
Doubling Time
The length of time required for a population to double in size
Environmental Geology
The study of the interactions between humans and their geologic environment
Hypothesis
A conceptual model or explanation for a set of data, mneasurments or observations
Mantle
The zone of the earth’s interior between crust and core; rich in ferromagnesian silicates
Exponential Growth
Growth Characterized by a constant percentage increase per unit time
Scientific Method
Means of discovering scientific principles by formulating hypotheses, making predictions from them and testing the predictions
Theory
A generally accepted explanation for a set of data or observations; its validity has usually been tested by the scientific method
Renewable Resources
Agiculture
Forestry
Horticulture
Non-Renewable Resources
Mineral Resources
(Subject to depletion)
Water
Cyclic resource
Can undergo degredation
Anion
An ion with a net negative charge
Atom
The smallest particle into which a chemical element can be subdivided
Atomic Mass Number
The sume of the number of protons and neutrons in an atomic nucleus
Atomic Number
Number of protons in an atomic nucleus; characteristic of a particular element
Carbonate
Nonsilicate mineral containing carbonate groups (CO3), carbon, and oxygen in the proportions of one atoms of carbon to three atoms of oxygen
Cation
An ion with a net positive charge
Chemical Sedimentary Rock
A rock formed from sediments at low temperature
Clastic Sedimentary Rock
Broken or fragmented; describes sediments or sedimentary rocks that are formed from fragments of pre-existing rocks or minerals
Cleavage
The tendancy of a mineral to break preferentially along planes in certain directions in the crystal structure
Compound
A chemical combination of two or more elements, in specific proportions, having a distinctive set of resultant physical properties
Contact Metamorphism
Local metamorphism adjacent to a cooling magma body
Covalent Bonding
Bonding involving sharing of electrons between atoms
Crystalline
Describes materials possessing a regular, repeating internal arrangement of atoms
Electron
A subatomic particle with an electrical cahrge or -1; generally found orbiting the nucleus
Ferromagnesian
A termdescribing silicates containing significant amounts of iron and/or magnesium; these minerals are usually dark-colored
Foliation
Parallel alignment of linear or platy minerals in a rock
Glass
Solid (especially silicate)lacking a regular internal crystal structure
Igneous
A rock formed or crystallized from a magma
Ion
Atom that has gained or lost electrons, so it has a net electrical charge
Ionic Bonding
Bonding due to attraction between oppositely charged ions
Isotope
Atoms ofa given chemical elements having the same atomic number but different atomic mass numbers
Lava
Magma that flows out at the earth’s surface
Lithification
Conversion of unconsolidated sediment into cohesive rock
Magma
A naturally occuring silicate melt, which may also contain mineral crystals, dissolved water,or gases
Metamorphic
Rock that is changed in form (deformed and/or recrystalized) through the effects of heat and/or pressure
Mineral
A naturally occuring, inorganic, solid element or compound with a definite composition or range in composition, usually havign a regular crystal structure
3000 minerals known
Native Element
Nonsilicate mineral consisting of a single chemical element
Neutron
An electrically neutral subatomic particle with a mass approximately equal to one atomic mass unit; generally found within an atomic nucleus
Nucleus
The center of an atom, containing protons and neutrons
Organic Sediments
Carbon rich sediments derived from the remains of living organisms
Oxide
Nonsilicate mineral containing oxygen combined with one or more metals
Periodic table
The regular arrangement of chemcial elements in a chart that reflects patterns of chemical behavior related to the electronicstructure of atoms
Plutonic
Describes an igneous rock crystallized well below the earth’s surface; typically coarse-grained
Proton
Subatomic particle with a charge of +1 and a mass of approximately one atomic mass unit; generally found within an atomic nucleus
Regional Metamorphism
Metamorphism on a large scale, involving increased heat and pressure; often associated with mouontain building
Rock
A solid, cohesive aggregate of one or more minerals
Rock Cycles
Teh concept thatrocks are continually subject to change and that any rock may be transformed into another type of rock through an appropriate geologic process
Sediment
Surface accumulation of loose, unconsolidated mineral or rock particles
Sedimentary
A rock formed from sediments at low temperature
Silicate
Mineral contianing silicon and oxygen and usually one or more additional elements
Sulfate
Nonsilicate mineral contianing sulfate (SO4) groups, each made up of one atom of sulfur and four atoms of oxygen
Sulfide
Nonsilicate mineral continingsulfur but no oxygen
Volcanic
describes any igneous rock formed at or near the earth’s surface
Asthenosphere
Partially molten, weak xone within the upper mantle immediately below the lithosphere
Brittle
Describes materials that tend to rupture before appreciable plastic deformation has occured
Compressive Stress
Stress tending to compress an object
Continental Drift
The concept that the continents have moved about over teh earth’s surface
Convection Cell
Circulating masses of material driven by temperature differences (hot material rises, then moves laterally,cools, sinks, and is reheated to rise again)
Convergent Plate Boundary
Plate boundary at whcih lithospheric plates are movingtoward each otehr; for example, a subduction zone or continental collision zone
Curie Temperature
Temperature above which a magnetic material loses its magnetism; different for each such material
Divergent Plate Boundary
A boundary along which lithospheric plates are moving apart; for example, seafloor spreading ridfges and continental rift zone
Ductile
Describes material that undergoes extensive plastic deformation without rupturing
Elastic Deformation
Deformation proportional to applied stress, from whcih the affected material will return toits original size and shape when the stress is removed
Elastic Limit
The stress above which a material will cease to deform elastically
Hot Spot
An isolated center of volcanic activity; often assocaited with a plate boundary
Island Arc
Chain of volcanic islands formed parallel to a subduction zone, on the overriding plate
Lithosphere
The solid, outermost zone of the earth, including the crust and a portion of the upper mantle; approximately 50 km thick under the oceans and commonly more than 100 km thick beneath the continents
Paleomagnetism
The fossil magnetism preserved inrocks formed in the past
Plastic Deformation
Permanent strain in material stressed beyond the elastic limit; the material will not return to its original dimensions when the stress is removed
Plate Tectonics
The theory that holds that the rigid lithosphere is broken up itnoa series of movable plates
Polar-Wander Curve
A plot of apparent magnetic pole positions atvarious times in teh past relative toa continent, assuming the continent’s position to have been fixed on the earth
Rupture
Breakage or failure of material under stress
Seafloor Spreading
The process by which new lithosphere is created at spreadingridges as plates of oceanic lithosphere move apart
Shearing Stress
Stress that tends to cause different parts of an object to slide past each other across a plane; with respect to mass movements, stress tending to pull material downslope
Strain
Deformation resulting from the application of stress
Stress
A force applied to an object
Subduction Zone
A convergent plate boundary at whcih oceanic lithosphere is being pushed beneath another plate (continental or oceanic) into the asthenosphere
Tectonics
The study of large scale movement and deformation of the earth’s crust
Tensile Stress
Stress tending to pull an object apart
Transform Fault
A fault between offset segments of a spreading ridge, along which two plates move horizontally inopposite directions
Chemical Elements
104 Elements
, 88 Naturally Occuring