Kimberlite explosion in New York

  • Thread starter Thread starter Count Iblis
  • Start date Start date
  • Tags Tags
    Explosion
Click For Summary
SUMMARY

The discussion centers on the geological phenomenon of kimberlite eruptions, specifically their rapid ascent from depths of 250 km to the surface at speeds of approximately 70 km/hr. Unlike typical volcanic eruptions, kimberlites are characterized by their abrupt and focused nature, lacking a known mechanism for gradual movement through the mantle. The presence of ancient carbon, or diamonds, at such depths raises questions about their stability and the geological processes involved in their transport. Kimberlite eruptions have been documented across all continents, primarily in ancient shield regions, with ages ranging from the early Precambrian to recent times.

PREREQUISITES
  • Understanding of kimberlite geology
  • Familiarity with diamond stability conditions
  • Knowledge of mantle dynamics and geological processes
  • Awareness of mineral chemistry related to kimberlite
NEXT STEPS
  • Research the geological mechanisms behind kimberlite eruptions
  • Study the stability of diamonds under varying pressure and temperature conditions
  • Explore the mineral chemistry of kimberlite to understand its origins
  • Investigate the historical distribution of kimberlite eruptions globally
USEFUL FOR

Geologists, mineralogists, and anyone interested in the dynamics of kimberlite eruptions and diamond formation will benefit from this discussion.

Count Iblis
Messages
1,859
Reaction score
8
http://www.users.muohio.edu/rakovajf/WTTW%20Kimberlite.pdf"
 
Last edited by a moderator:
Earth sciences news on Phys.org
I think you might mean kimberlite extrusion !
Unfortunately diamonds->kimberlite but kimberlite->diamonds
 
Kimberlites are interesting as there is no known geological mechanism to push or pull the kimberlite suddenly from a depth of 250 km to 150 km to the surface at 70 km/hr. Kimberlites are very focused abrupt events. Would not a force generated at great depths gradually push the kimberlite up through the mantel. What stops kimberlite from moving gradually to the surface as magma? (i.e. Think of forces balanced. Strength of the mantel that stops movement vs whatever force moves the kimberlite.)

Kimberlite eruptions are quite different than volcanos.

Why is the ancient carbon (diamond) found at great depths in the planet?

Kimberlites (The Oxford Companion to The Earth, page 577/578)

(kimberlite) … provides the deepest samples of the planet, because it has been erupted at high speed (roughly 70 km/hr as diamond is not stable above 150 km and will in the high heat revert in form back to carbon, if it does not move at 70 km/hr cooled by the entrapped expanding gas.) from depths in excess of 150 km (a region in which diamond is stable)

Diamondiferous kimberlite is known on all the continents, where is confined to the oldest shield segments, …

The eruptions range in age from early Precambrian to recent with a notable display in Cretaceous times in Africa and South America. No kimberlites have been recorded in the ocean basin.

From the detailed mineral chemistry it is possible to estimate the samples (Saul: Kimberlite) come from depths to about 250 km…

The ages of the diamonds are also interesting, because they are commonly much older than the host kimberlite, some, indeed, are as old as the oldest rocks on the Earth, showing that many, if not all were picked up by the kimberlite during its passage to the surface.
 

Similar threads

  • · Replies 6 ·
Replies
6
Views
2K
  • · Replies 5 ·
Replies
5
Views
4K
Replies
3
Views
4K
  • · Replies 2 ·
Replies
2
Views
3K
  • · Replies 2 ·
Replies
2
Views
1K
  • · Replies 17 ·
Replies
17
Views
2K
  • · Replies 5 ·
Replies
5
Views
3K
  • · Replies 3 ·
Replies
3
Views
1K
  • · Replies 17 ·
Replies
17
Views
3K
  • · Replies 4 ·
Replies
4
Views
1K