The deep ocean floor is flat and nearly featureless.
The deep ocean floor is flat and narly featureless.
Abyssal plain regions of the sea floor with negative magnetic anomalies were formed during times when earth s magnetic field.
The sea floor then drops off steeply along the continental slope the true edge of the continent.
At depths of over 10 000 feet and covering 70 of the ocean floor abyssal plains are the largest habitat on earth.
The highest mountain in the world in terms of distance from base to peak is in the ocean.
Look at figure 14 23.
The deep ocean floor is flat and nearly featureless.
None of the above are correct.
Core a1 has 2 88 meters m of clay and siliceous ooze covering 4 86 m of pillow basalt.
This is the youngest part of the ocean floor that is.
Temperature the lithosphere is cooler than the asthenosphere.
The cores are collected in order from east to west along the bottom of the basin and are labeled a1 b1 c1 and d1 respectively.
The deep ocean floor is flat and nearly featureless.
Click card to see definition.
Both a and b are correct.
A geologist aboard a deep sea research vessel has collected several drill cores of oceanic crust from the bottom of the ocean.
Sunlight does not penetrate to the sea floor making these deep dark ecosystems less productive than those along the continental shelf.
The primary difference between lithospheric and asthenospheric mantle is.
If you follow the ocean floor out from the beach at the top left the seafloor gently slopes along the continental shelf.
Which of these parts of the deep ocean floor is flat and nearly featureless.
Plates slip past each other.
Along constructive divergent plate boundaries.
But despite their name these plains are not uniformly flat.
Rates of sea floor spreading are equal to sea floor consumption.
Correct which of these parts of the deep ocean floor is flat and nearly featureless.
This is where the new ocean floor comes from.
