A cooperative program of seismic refraction profiling was completed in the vicinity of the Puerto Rico Trench by Hudson Laboratories, Woods Hole, Lamont, and Texas A. & M. Profiles completed near the western end of the Trench were analyzed at Hudson Laboratories. Five seismic layers are indicated below the water layer. The thickness/velocity relationships are as follows: 5.1 km of 1.5 km/sec. (water); 1 km of 1.7 km/sec. (sediment); 1.5 km of 3 km/sec. (metamorphics?); 2 km of 5.5 km/sec. (basement); and 2 km of 7.1 km/sec. (high speed basement). Below these, typical Moho velocities of 8.1 km/sec. were measured. Total depth to Moho ranges from 9 to 12 km below sea level, the greatest variation occurring in the basement layers. The least depth was measured 65 miles north of the Puerto Rico Trench.
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March 01 1962
Some Seismic Profiles near the Western End of the Puerto Rico Trench
John Northrop,
John Northrop
From The Hudson Laboratories, Columbia University, Dobbs Ferry, New York.
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Morris Ransone
Morris Ransone
From The Hudson Laboratories, Columbia University, Dobbs Ferry, New York.
Search for other works by this author on:
John Northrop
From The Hudson Laboratories, Columbia University, Dobbs Ferry, New York.
Morris Ransone
From The Hudson Laboratories, Columbia University, Dobbs Ferry, New York.
Mr. Northrop's present address is the Marine Physical Laboratory of the Scripps Institution of Oceanography, University of California, San Diego
Online ISSN: 1540-7748
Print ISSN: 0022-1295
Copyright, 1962, by The Rockefeller Institute Press.
1962
J Gen Physiol (1962) 45 (4): 243–251.
Citation
John Northrop, Morris Ransone; Some Seismic Profiles near the Western End of the Puerto Rico Trench . J Gen Physiol 1 March 1962; 45 (4): 243–251. doi: https://doi.org/10.1085/jgp.45.4.243
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