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38 Terms
1
Neptunism
A geological theory proposed by Abraham Werner in 1787, stating all rocks were formed from a primeval ocean.
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2
Catastrophism
A theory by Baron George Cuvier suggesting rocks formed through catastrophic events such as volcanism and earthquakes.
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3
Uniformitarianism
A theory developed by James Hutton that became the backbone of geological thought, asserting that processes observed today have always worked in the same way.
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4
Stratification
The layering of rock sequences, can include igneous, sedimentary, and metamorphic rocks.
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5
Contact
The interface between different lithologies.
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6
Lithology
The physical and chemical characteristics of a rock type.
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7
Formation
A definable stratigraphic unit of rock that has a name and distinctive boundaries.
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8
Stratigraphic sequence
All the vertical changes in rock formations at a specific location.
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9
Hiatus
A significant break in deposition indicating missing geologic time.
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10
Unconformity
Occurs when there is a break in deposition due to the passage of significant geologic time.
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11
Transgression
Geological process involving the rise of sea level and the inundation of land areas.
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12
Regression
The geological process where sea level falls, causing land to be exposed.
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13
Biostratigraphy
Correlation using fossils to determine the age and equivalency of rock layers.
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14
Index fossil
Fossils that were abundant, easily recognizable, and existed for a relatively short geologic timeframe, useful for dating rock layers.
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15
Superposition
The principle that older layers of rock are found below younger layers in a stratigraphic sequence.
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16
Photochemical Dissociation
The breakdown of water vapor by the sun to produce ozone during the Archean eon.
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17
Stromatolites
Layered sedimentary formations created by the activities of cyanobacteria.
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18
Cyanobacteria
Photosynthetic bacteria that play a crucial role in the production of oxygen and the formation of stromatolites.
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19
Polymers
Molecules made up of long chains of monomers; examples include DNA and RNA.
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20
Epeiric sea
Shallow seas that cover continental landmasses.
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21
Paleomagnetism
The study of ancient Earth's magnetic field to determine past plate movements.
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22
Cratonic sequence
A cycle of transgression and regression during the Paleozoic, outlined by Lawrence Sloss.
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23
Sauk Sequence
The first major transgression onto the North American Craton from the late Proterozoic to early Ordovician.
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24
Feedback
The system of solving problems through the ongoing process of assessment and adaptation in scientific research.
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25
Lateral gradation
Changes in lithology that occur horizontally due to varying depositional environments.
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26
Taconic Orogeny
A mountain-building event during the Ordovician caused by the subduction of the Iapetus oceanic plate beneath the Laurentian plate.
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27
Mountain-building episodes
Events related to tectonic forces that result in the uplift of mountain ranges.
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28
Absolute age dating
Techniques used to determine the actual age of a rock or fossil.
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29
Transgressions and regressions
Refers to the rise and fall of sea levels and their impact on sediment deposition.
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30
Glacial melting effects on sea level
The rising of sea levels due to the melting of glaciers during warmer periods.
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31
Fossil correlation
The comparison of two stratigraphic columns using fossils to establish age equivalency.
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32
Range zone
The time span during which a particular index fossil existed in the geological past.
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33
Erosion
The process by which surface materials are worn away and transported elsewhere.
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34
Deposition
The process by which sediments settle out of the transporting medium (water, air, etc.).
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35
Conformable stratigraphic sequences
Sequences of rock layers that show no significant breaks in deposition.
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36
Index fossils
Fossils that are used to define and identify a particular time period in geological history.
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37
Importance of stromatolites
Among the oldest known fossils, important for understanding early life and the Earth's atmosphere.
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38
Origin of life requirements
Presence of appropriate elements and an energy source to promote the synthesis of organic molecules.