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Exploring Types of Geological Unconformities
Oct 7, 2024
Lecture Notes: Understanding Unconformities in Geology
Introduction
Geologists decipher Earth's history through rock formations.
Missing rock layers affect interpretation, similar to missing pages in a book.
Objective: Identify characteristics and formation of unconformities.
What is an Unconformity?
An unconformity is an erosion surface representing a time gap between rock layers.
Types of unconformities:
Angular Unconformity
Disconformity
Non-Conformity
Angular Unconformities
Formation Process:
Horizontal sediment layers form under marine conditions.
Uplift tilts, faults, or folds layers.
Erosion removes top layers.
New horizontal layers deposit over erosion surface.
Example: Utah
Tan sedimentary rock over tilted red rock.
Disconformities
Formation Process:
Sedimentary layers form under marine conditions.
Uplift and erosion remove some upper layers.
New horizontal layers form parallel to original layers.
Identification:
Old soil horizons or fossil age differences.
Example: Hungary
Parallel layers with color differences.
Non-Conformities
Formation Process:
Igneous/metamorphic rock uplifted and eroded.
Submerged below rising ocean.
Sedimentary rocks deposit on top.
Example: Sandstone on older igneous rock.
Case Study: Grand Canyon
Types of Unconformities present:
Angular Unconformity
Disconformity
Non-Conformity
Examples:
Tapeats Sandstone over igneous/metamorphic rocks (Non-conformity) - Great Unconformity.
Grand Canyon Supergroup under Tapeats Sandstone (Angular Unconformity).
Disconformities between Redwall Limestone and other formations indicating significant time gaps.
Key Takeaways
Unconformities signify significant gaps in geologic time.
Careful examination of fossils helps in identifying unconformities.
The Grand Canyon illustrates all three types of unconformities.
Learning Objectives Recap
Identified types and characteristics of unconformities.
Explained how unconformities form.
Encouragement to reflect on understanding of objectives.
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