Skip to primary content

Sierra Geology

where rocks meet the human environment (or vice versa)

Sierra Geology

Main menu

  • Home
  • Documents
    • 2013 GSA Cordilleran Conference Presentations
      • Early Tertiary Climate Change and its Impact on the Matrix Mineralogy of “auriferous gravels” in the Sierra Nevada Foothills
      • The Nature of Early Tertiary Soils and Sediments — Mineralogy and Petrology
      • Geologic Hazards in the Early Tertiary Sediments of the Sierra Nevada Foothills of California
      • Landslide Hazards Along the Interstate 80 Corridor Associated with the Early Oligocene Sedimentary and Volcanic Deposits in the Sierra Nevada
    • References
      • The Upper Reaches of the Sierra Nevada Auriferous Gold Channels
      • Geology of the Ione Formation in the Ione Area
      • A Historical Review Of The Age Assignments Applied To The Chalk Bluff Fossil Plant Assemblage, Central Sierra Nevada
      • Gold Bearing Gravels of the Ancestral Yuba River, Sierra Nevada
      • Re-evaluation of the origin of kaolinite in the Ione Formation
      • Geology and Ceramic Properties of the Ione Formation, Buena Vista Area
      • A Middle Eocene Flora From The Central Sierra Nevada
      • Origin of gold in placer deposits of the Sierra Nevada Foothills, California
      • The Ione Formation of California
    • Geologic hazards associated with Eocene and Oligocene Sedimentary Units in the Sierra Nevada Foothills
      • CGS Geologic Hazard Notice — Smectitic Sediments
  • Contact
  • About
  • Images
    • UC Davis Petrified Log Installation
    • Pritchard Marble Quarry and Kiln

Post navigation

← Previous Next →

Re-evaluation of the origin of kaolinite in the Ione Formation

Posted on October 10, 2013 by James Wood

This research document is posted in the References collection.

This entry was posted in Early Tertiary References, Oxisols and tagged anauxite, detrital clay clasts, Eocene kaolinite, Eocene Oxisol, Ione Formation kaolinite, Late Eocene smectite, pedarenite, pedogenic silica cement by James Wood. Bookmark the permalink.
Proudly powered by WordPress