1.
Science
; 151(3717): 1525-6, 1966 Mar 25.
Artigo
em Inglês
| MEDLINE
| ID: mdl-17730083
RESUMO
A thermograd record obtained over the Ayes Ridge indicated existence, at the time of observation, of a cold layer of water in the lowest 13 meters, undergoing high-frequency internal oscillations. The great discontinuity in temperature across the sedimnent-water interface and the lack of agreement with the normal temperature structure indicate that the layer was a transient feature. This abnormal condition may be related to the passage of a hurricane 3 days earlier.
2.
Science
; 163(3865): 383-6, 1969 Jan 24.
Artigo
em Inglês
| MEDLINE
| ID: mdl-17730184
RESUMO
The discovery of a leveed deep-sea channel whose axial gradient reverses near the Aleutian trench supports the hypothesis that the downbowing of the trench interrupted the turbidity current processes that constructed the Aleutian abyssal plain.