Exploring the Geology of Blacktail Canyon

Sep 17, 2024

Notes on Blacktail Canyon Lecture

Introduction

  • Location: Blacktail Canyon, Grand Canyon, Northern Arizona
  • Presenter: Geology Professor Sean Bilsey
  • Focus: Geologic features, specifically the Great Unconformity

Overview of Blacktail Canyon

  • Narrow canyon carved by flash floods
  • Contains impressive scenery and geology
  • Access to hallmark geologic features

Tapeats Sandstone

  • Main Unit: Tapeats Sandstone
    • Color: Beige to buff
    • Age: Cambrian (about 530 million years old)
    • Composition: Grains of sand, some pebbles
    • Depositional Environment: Coastal setting where rivers fed into the ocean
    • Features: Possible small crossbeds indicating river channel deposits

Vishnu Schist and Zoroaster Granite

  • Underlying Unit: Vishnu Schist
    • Age: About 1.8 billion years old
    • High-grade metamorphic rock
  • Intrusions: Zoroaster Granite
    • Intrudes into Vishnu Schist

The Great Unconformity

  • Definition: Contact between Tapeats Sandstone and Vishnu Schist
    • Represents a significant period of erosion or missing rock layers
    • Known as the Great Unconformity (1.3 billion years of geological history)
  • Implications:
    • Metamorphic rocks indicate formation at great depths beneath mountains
    • Erosion smoothed the landscape to allow for deposition of Tapeats Sandstone
    • Represents a drastic change in geological settings

Geological Processes

  • Formation of Vishnu Schist: Created through heat and pressure deep within the Earth
  • Erosion: Period needed to planar off mountains to allow for sedimentary deposits
  • Importance of understanding how these processes shaped the Grand Canyon

Visual Observations

  • Foliation in Schist: Vertical layering cut by quartz veins or dikes
  • Contact View: Tapeats Sandstone directly on Vishnu Schist
  • Sand Lens: Observed within the base of the Tapeats Sandstone
  • Additional Remarks: Folded or bent foliation observed in some metamorphic rocks

Rafting and River Dynamics

  • Flash floods push rock and debris into the Colorado River, creating rapids
  • Water constriction increases flow speed, contributing to river channel irregularities

Conclusion

  • Blacktail Canyon offers an exceptional view of the Great Unconformity
  • Importance of preservation for geological education
  • Encouragement for further support and engagement with geology education through donations and social media engagement.