Search this site
Embedded Files

The Crisis in US Science 2025-2026

Get downloads & resources
Steven B Shirey
  • Home
    • Background
    • Scientific Interests
    • EPL Geochemistry
  • Information
    • Crisis in US Science
      • The crisis in science
      • NSF Talking Points
      • What Can I Do?
      • Distict Office Visits
      • Supporting Information about NSF
    • Fellows & Visitors
    • Local Geology
    • About Diamonds
  • Resume, CV
    • Resume + Pubs
    • List of Mentees
    • Complete CV
  • Publications
    • All Publications
    • Nature, Science, Geology
    • Method Development
    • Superdeep Diamonds
    • Lithospheric Diamond/Continental Mantle
    • Arc Volcanism
    • Archean Crust/Mantle
    • Continental Volcanism
    • Oceanic Volcanism
    • Impacts & Meteorites
    • Mantle Heterogeneity
  • Resources
    • Journals & Useful Links
    • DC Area Lectures
    • EPL-CIW History
  • Outreach
    • DC Area Geology
    • Las Campanas Geology
    • Sudbury Area Field Trip
    • Postdoc Workshops
    • Diamond Columns
    • Diamond Schools
    • Teacher Education
    • Science Festival
Steven B Shirey
  • Home
    • Background
    • Scientific Interests
    • EPL Geochemistry
  • Information
    • Crisis in US Science
      • The crisis in science
      • NSF Talking Points
      • What Can I Do?
      • Distict Office Visits
      • Supporting Information about NSF
    • Fellows & Visitors
    • Local Geology
    • About Diamonds
  • Resume, CV
    • Resume + Pubs
    • List of Mentees
    • Complete CV
  • Publications
    • All Publications
    • Nature, Science, Geology
    • Method Development
    • Superdeep Diamonds
    • Lithospheric Diamond/Continental Mantle
    • Arc Volcanism
    • Archean Crust/Mantle
    • Continental Volcanism
    • Oceanic Volcanism
    • Impacts & Meteorites
    • Mantle Heterogeneity
  • Resources
    • Journals & Useful Links
    • DC Area Lectures
    • EPL-CIW History
  • Outreach
    • DC Area Geology
    • Las Campanas Geology
    • Sudbury Area Field Trip
    • Postdoc Workshops
    • Diamond Columns
    • Diamond Schools
    • Teacher Education
    • Science Festival
  • More
    • Home
      • Background
      • Scientific Interests
      • EPL Geochemistry
    • Information
      • Crisis in US Science
        • The crisis in science
        • NSF Talking Points
        • What Can I Do?
        • Distict Office Visits
        • Supporting Information about NSF
      • Fellows & Visitors
      • Local Geology
      • About Diamonds
    • Resume, CV
      • Resume + Pubs
      • List of Mentees
      • Complete CV
    • Publications
      • All Publications
      • Nature, Science, Geology
      • Method Development
      • Superdeep Diamonds
      • Lithospheric Diamond/Continental Mantle
      • Arc Volcanism
      • Archean Crust/Mantle
      • Continental Volcanism
      • Oceanic Volcanism
      • Impacts & Meteorites
      • Mantle Heterogeneity
    • Resources
      • Journals & Useful Links
      • DC Area Lectures
      • EPL-CIW History
    • Outreach
      • DC Area Geology
      • Las Campanas Geology
      • Sudbury Area Field Trip
      • Postdoc Workshops
      • Diamond Columns
      • Diamond Schools
      • Teacher Education
      • Science Festival

Project Areas

Diamonds and the Mantle Geodynamics of Carbon

Old Continental Crust

Ore Deposit Distribution

✦ Graham Pearson (foreground) and Jesse Reimink (background) unloading the float plane in order to construct a new basecamp for fieldwork in the Northwest Territories. (Photo: Steve Shirey)

Large Scale Research Initiatives


Diamonds and the Mantle Geodynamics of Carbon


Central Slave Basement Complex


Metal Earth 


Off-Axis Seamount Investigation at Siqueiros (OASIS), Cruise AT-05

Contact information

Updated August 26, 2026  —  Content © 2005-2026 Steven B. Shirey 

This website is the personal website of the author. It contains information used, created, copyrighted, and provided by the author for the express use of the reader.  This website does not represent an official viewpoint of the Carnegie Institution for Science, nor is it intended to be used for any official business of the Carnegie Institution for Science.

Report abuse
Page details
Page updated
Report abuse