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Newsletter of the Utah Geological Association P.O. Box 520100 Salt Lake City, Utah 841520100 http://utahgeology.org VOLUME 42, NUMBER 7July 2010July UGA Luncheon Meeting July 12, 2010Stratigraphy
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Step 1: Begin by collecting geological data and rock samples from the area of interest.
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Step 2: Analyze the rock samples to identify different layers and their characteristics.
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Step 3: Create a stratigraphic column, a diagram that represents the sequence of rock layers from oldest to youngest.
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Step 4: Use various stratigraphic principles, such as superposition and cross-cutting relationships, to determine the relative ages of the rock layers.
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Step 5: Apply correlation techniques to establish connections between different stratigraphic columns in different locations.
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Step 6: Use fossil dating and absolute dating methods to assign numerical ages to the rock layers.
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Step 7: Document the findings and interpretations in a comprehensive stratigraphy and correlation report.

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Stratigraphy and correlation is the study of rock layers and their relationships to each other.
Geologists and other professionals working in the field of earth sciences are typically required to file stratigraphy and correlation reports.
Stratigraphy and correlation reports are typically filled out by documenting the different rock layers present in a specific area and determining their chronological order.
The purpose of stratigraphy and correlation is to understand the geological history and structure of a particular area.
Information such as the types of rock layers present, their thickness, and their relative ages must be reported in a stratigraphy and correlation report.
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