The crust encompasses the brittle and shifting continental plates; it becomes scarred with mountains when the plates grind together or
with deep ocean basins when the plates pull apart.
Not exact matches
The
deep basins under the
oceans are carpeted
with lava that spewed from submarine volcanoes and solidified.
For much of the global
ocean the coarser resolution is okay, but when you are studying a unique location like the Gulf of Maine,
with its complex bathymetry of
deep basins, channels, and shallow banks combined
with its location near the intersection of two major
ocean current systems, the output from the coarser models can be misleading.»
«The main hydrological features of the
deep Mediterranean Sea are (a) high homeothermy from roughly 300 — 500 m to the bottom, and bottom temperatures of about 12.8 °C to 13.5 °C in the western
basin and 13.5 °C to 15.5 °C in the eastern
basin (i.e., there are no thermal boundaries, whereas in the Atlantic
Ocean the temperature decreases
with depth)»
To ascertain
with confidence the extent to which
deep water production impacts the
ocean's meridional circulation and hence the
ocean's contributions to the global poleward heat flux, continuous measures of trans -
basin mass and heat transports are needed.
The Arctic
Ocean sits in an almost enclosed
basin with only one
deep channel in and out called the East Greenland Rift (Figure 4).
All are graced
with relatively pristine waters, and all have significant
deep ocean basin waters.
A quantitative theoretical model of the meridional overturning circulation and associated
deep stratification in an interhemispheric, single -
basin ocean with a circumpolar channel is presented.