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- Strike and dip are used to describe any planar features in geology, including12:
- Sedimentary bedding
- Fractures
- Faults
- Joints
- Cuestas
- Igneous dikes and sills
- Metamorphic foliation and fabric
Learn more:✕This summary was generated using AI based on multiple online sources. To view the original source information, use the "Learn more" links.Any planar feature can be described by strike and dip, including sedimentary bedding, fractures, faults, joints, cuestas, igneous dikes and sills, metamorphic foliation and fabric, etc. Observations about a structure's orientation can lead to inferences about certain parts of an area's history, such as movement, deformation, or tectonic activity.en.wikipedia.org/wiki/Strike_and_dipStrike and dip are used to describe any other planar features, including joints, faults, dykes, sills, and even the foliation planes in metamorphic rocks.openpress.usask.ca/physicalgeology/chapter/13-5-… - People also ask
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In geology, strike and dip is a measurement convention used to describe the plane orientation or attitude of a planar geologic feature. A feature's strike is the azimuth of an imagined horizontal line across the plane, and its dip is the angle of inclination (or depression angle) measured downward from … See more
When measuring or describing the attitude of an inclined feature, two quantities are needed. The angle the slope descends, or dip, and the direction of descent, which can be represented … See more
Conventions
There are a few conventions geologists use when measuring a feature's azimuth. When using the … See moreOn geologic maps, strike and dip can be represented by a T symbol with a number next to it. The longer line represents strike, and is in the same orientation as the strike angle. Dip is … See more
• Compton, Robert R. (1985). Geology in the Field. New York: J. Wiley and Sons. ISBN 978-0-471-82902-7. OCLC 301031779. See more
Wikipedia text under CC-BY-SA license Jan 8, 2020 · In Part I of geological structures, students will learn how to interpret strike and dip information from a geological map, prepare a …
- Author: Joyce McBeth, Karla Panchuk, Tim Prokopiuk, Lyndsay Hauber, Sean Lacey
- Publish Year: 2020
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Jan 8, 2020 · Demonstrate an understanding of the concepts of strike and dip. Use block diagrams to display geologic features. Interpret a geologic map. Create a geologic cross-section from a geologic map.
Figure 12.19 Measurement of strike (left) and dip (right) using a geological compass with a clinometer. [SE] Strike and dip are also used to describe any other planar features, including joints, faults, dykes, sills, and even the …
Strike and dip. A fault is a planar geologic structure. Like any planar structure, it has an orientation that may be characterized by strike and dip. For small faults, it may be possible to walk up to an outcrop and measure the …
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Strike and dip are used to describe any other planar features, including joints, faults, dykes, sills, and even the foliation planes in metamorphic rocks. Figure 13.37 shows an example of how we would depict the beds that make up an …
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