120 Degree Celsius

 

30 DEGREE CELSIUS

60 DEGREE CELSIUS

90 DEGREE CELSIUS

120 DEGREE CELSIUS

BACK TO SEDIMENT ISOTHERMS

The map below shows the estimated depth below seafloor of the 120°C isotherm.  White shading indicates areas where the isotherm does not occur within the sediments, but within the basement rock. This map is based on the data and limitations discussed in Sediment Isotherms .

 

 

 

 

 

   

PROGRAM OVERVIEW
RESEARCH ACTIVITIES
STUDENT OPPORTUNITIES
CONTACT US
GRADUATE SCHOOL OF OCEANOGRAPHY
UNIVERSITY OF RHODE ISLAND

Copyright © 2002 University of Rhode Island. All rights reserved. Disclaimer. Contact webmaster@gso.uri.edu
for more information about this page. Last revised June 2003.