template below. Use measurements along the vertical dashed line for the thickness of each part of the turbidite and include the mudstone below and above the turbidite in your column. Include the scale, lithology, and grain size (as best you can tell). Label the sedimentary structures (LO5) and Bouma facies (LO9) that are present at the location(s) they are present in the column. Scale Lithology Mud Sand Gravel vf m vc Texture (Sorting, color, sedimentary structures, fossils, etc.) Bouma Facies

Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
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As a hint, everything crumbled in the photo is mudstone and the solid block is all sandstone.

You also need to label the layers of sandstone w/ which section of bouma facies they represent. 

This educational resource provides a template for creating a stratigraphic column of a turbidite sequence. The template includes several key sections for data recording and analysis.

### Template Components:

1. **Scale:**
   - A vertical line is provided for marking the scale of the stratigraphic column, essential for indicating the thickness of each sediment layer in the turbidite sequence.

2. **Lithology:**
   - A column labeled "Lithology" is used to specify the type of rock or sediment present in each layer of the stratigraphic sequence.

3. **Grain Size:**
   - A table for grain size includes categories for different sediment types:
      - **Clay**
      - **Silt**
      - **Sand**: divided into very fine (vf), fine (f), medium (m), coarse (c), and very coarse (vc)
      - **Gravel**: divisions include granules (gra), pebbles (peb), cobbles (cob), and boulders (boul)

4. **Texture:**
   - This section captures additional sediment characteristics, such as sorting, color, sedimentary structures, and the presence of fossils.

5. **Bouma Facies:**
   - The column allows for labeling of Bouma facies, which are specific sequences of sedimentary structures commonly found in turbidites, following the Bouma Sequence classification.

### Instructions:

- Use the vertical dashed line to measure and input the thickness of each part of the turbidite sequence.
- Include the surrounding mudstone layers, both above and below the turbidite.
- Indicate the scale, lithology, grain size, sedimentary structures (LO5), and Bouma facies (LO9) at specific locations on the column where they are observed.

This template is a guide for geologists and students to systematically document and analyze the characteristics of turbidite deposits in the field.
Transcribed Image Text:This educational resource provides a template for creating a stratigraphic column of a turbidite sequence. The template includes several key sections for data recording and analysis. ### Template Components: 1. **Scale:** - A vertical line is provided for marking the scale of the stratigraphic column, essential for indicating the thickness of each sediment layer in the turbidite sequence. 2. **Lithology:** - A column labeled "Lithology" is used to specify the type of rock or sediment present in each layer of the stratigraphic sequence. 3. **Grain Size:** - A table for grain size includes categories for different sediment types: - **Clay** - **Silt** - **Sand**: divided into very fine (vf), fine (f), medium (m), coarse (c), and very coarse (vc) - **Gravel**: divisions include granules (gra), pebbles (peb), cobbles (cob), and boulders (boul) 4. **Texture:** - This section captures additional sediment characteristics, such as sorting, color, sedimentary structures, and the presence of fossils. 5. **Bouma Facies:** - The column allows for labeling of Bouma facies, which are specific sequences of sedimentary structures commonly found in turbidites, following the Bouma Sequence classification. ### Instructions: - Use the vertical dashed line to measure and input the thickness of each part of the turbidite sequence. - Include the surrounding mudstone layers, both above and below the turbidite. - Indicate the scale, lithology, grain size, sedimentary structures (LO5), and Bouma facies (LO9) at specific locations on the column where they are observed. This template is a guide for geologists and students to systematically document and analyze the characteristics of turbidite deposits in the field.
The image displays a sedimentary rock formation with a focus on its texture and layers. A black vertical scale is visible on the left side, marking intervals of 1 cm and extending to 5 cm, providing a reference for the size of the rock layers. A dashed black line runs vertically across the image, indicating a clear division or boundary within the formation.

At the bottom, a scale bar featuring alternating black and white segments measures geological formations, each segment representing a standard length for precise measurement. The text on the scale bar reads "Society for Sedimentary Geology," indicating the source or affiliation.

The rock shows stratifications, indicating different layers of sediment deposition over time. The texture and color variations across the rock suggest historical geological processes and changes in environmental conditions during formation. The surrounding area consists of smaller, fragmented rock pieces, likely resulting from natural weathering or erosion processes.
Transcribed Image Text:The image displays a sedimentary rock formation with a focus on its texture and layers. A black vertical scale is visible on the left side, marking intervals of 1 cm and extending to 5 cm, providing a reference for the size of the rock layers. A dashed black line runs vertically across the image, indicating a clear division or boundary within the formation. At the bottom, a scale bar featuring alternating black and white segments measures geological formations, each segment representing a standard length for precise measurement. The text on the scale bar reads "Society for Sedimentary Geology," indicating the source or affiliation. The rock shows stratifications, indicating different layers of sediment deposition over time. The texture and color variations across the rock suggest historical geological processes and changes in environmental conditions during formation. The surrounding area consists of smaller, fragmented rock pieces, likely resulting from natural weathering or erosion processes.
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