Venera Images, VENERA 13 fully calibrated image |
Venera Images, VENERA 13 fully calibrated image |
Sep 14 2005, 09:26 PM
Post
#1
|
|
Senior Member Group: Members Posts: 1091 Joined: 19-February 05 From: Close to Meudon Observatory in France Member No.: 172 |
|
|
|
Jan 10 2006, 06:30 PM
Post
#2
|
|
Member Group: Members Posts: 903 Joined: 30-January 05 Member No.: 162 |
{ I hope I phrase this well enough }
Does any one know the cooling rate for 'earth type' basaltic magma from the time of contact with liquid water to the point it has solidified as compared to the expected cooling rate for the Venusian equivalent of basaltic magma from the time of contact with the Venusian atmosphere to the point of solidification? Is 1300 psi (or whatever it works out to) CO2 more heat absorbing than H2O at 15 psi ? Funny if the magma on Venus solidifies faster than the magma on earth in contact with sea water. Would this effect the forms of the rocks we expect to see? |
|
|
Lo-Fi Version | Time is now: 10th November 2024 - 07:49 PM |
RULES AND GUIDELINES Please read the Forum Rules and Guidelines before posting. IMAGE COPYRIGHT |
OPINIONS AND MODERATION Opinions expressed on UnmannedSpaceflight.com are those of the individual posters and do not necessarily reflect the opinions of UnmannedSpaceflight.com or The Planetary Society. The all-volunteer UnmannedSpaceflight.com moderation team is wholly independent of The Planetary Society. The Planetary Society has no influence over decisions made by the UnmannedSpaceflight.com moderators. |
SUPPORT THE FORUM Unmannedspaceflight.com is funded by the Planetary Society. Please consider supporting our work and many other projects by donating to the Society or becoming a member. |