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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Describe the geologic history of the cross-section shown below. Note any unconformities that may be present and what type they are. Includes faulting and folding events. List from the oldest event to the youngest event on the lines below.

### Geological Cross-Section Diagram

This diagram illustrates a geological cross-section highlighting various rock layers and structures. Here's a detailed description:

- **Surface Layer**:
  - **A**: Diagonal band representing a fault line, illustrated by a series of parallel lines intersecting other layers, indicating past tectonic activity.
  - **B**: Topmost horizontal layer, composed of loosely-packed sediment, possibly soil or alluvium, indicating the current surface.

- **Subsurface Layers**:
  - **C**: Horizontal band below layer B, consisting of fine, consistent striations signifying sedimentary rock, likely sandstone or shale.
  - **Y**: Denotes a vertical cut, marking a potential sampling or exploratory section.

- **Folded Layers**:
  - **D**: Curved layers on either side of the fault line, showing deformation. This layer appears to be composed of more massive, block-like structures, possibly limestone or another carbonate rock.
  - **E, F, and G**: Series of arching strata beneath layer C, indicating previous folding events. These layers depict alternating textures, signifying different rock compositions.
  - **H**: Curved layer similar in texture to C, positioned at the bottom of the visible section, possibly representing an older sedimentary formation.

This cross-section exemplifies geological processes such as sedimentation, faulting, and folding, essential for understanding Earth's geological history.
Transcribed Image Text:### Geological Cross-Section Diagram This diagram illustrates a geological cross-section highlighting various rock layers and structures. Here's a detailed description: - **Surface Layer**: - **A**: Diagonal band representing a fault line, illustrated by a series of parallel lines intersecting other layers, indicating past tectonic activity. - **B**: Topmost horizontal layer, composed of loosely-packed sediment, possibly soil or alluvium, indicating the current surface. - **Subsurface Layers**: - **C**: Horizontal band below layer B, consisting of fine, consistent striations signifying sedimentary rock, likely sandstone or shale. - **Y**: Denotes a vertical cut, marking a potential sampling or exploratory section. - **Folded Layers**: - **D**: Curved layers on either side of the fault line, showing deformation. This layer appears to be composed of more massive, block-like structures, possibly limestone or another carbonate rock. - **E, F, and G**: Series of arching strata beneath layer C, indicating previous folding events. These layers depict alternating textures, signifying different rock compositions. - **H**: Curved layer similar in texture to C, positioned at the bottom of the visible section, possibly representing an older sedimentary formation. This cross-section exemplifies geological processes such as sedimentation, faulting, and folding, essential for understanding Earth's geological history.
Expert Solution
Step 1

In the given geological cross-section, several beds are present. Here, we can see that there are both folding and faulting episodes.

Applying the Law of Superposition, we can conclude that bed H is the oldest followed by bed G, bed F, bed E, and bed D. Then an episode of folding affected beds H, G, F, E, and D. After that Faulting has taken place along Y. The folded beds have been displaced due to the fault. Though from the given image, we cannot confirm whether bed D is affected by the fault. After all these events, an igneous intrusion A has taken place which has been emplaced above beds H, G, F, E. Then there was the deposition of bed C followed by the deposition of bed B. Bed B is the youngest. There lies an unconformity (which is denoted by I).

                                                                      Bed B                                                       Youngest

Bed C

                   -Unconformity (I)-                   

  Igneous intrusion (Bed A)

-Faulting-

                                          -Folding-                                         

Bed D

Bed E

Bed F

Bed G

                                                                   Bed H                                                         Oldest

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