The Deep Ocean Floor Is Flat And Narly Featureless

The ocean floor has topography as varied as dry land does.

The deep ocean floor is flat and narly featureless.

At depths of over 10 000 feet and covering 70 of the ocean floor abyssal plains are the largest habitat on earth. Core a1 has 2 88 meters m of clay and siliceous ooze covering 4 86 m of pillow basalt. Abyssal plain regions of the sea floor with negative magnetic anomalies were formed during times when earth s magnetic field. This is where the new ocean floor comes from.

The highest mountain in the world in terms of distance from base to peak is in the ocean. The deep ocean floor is flat and nearly featureless. None of the above are correct. Which of these parts of the deep ocean floor is flat and nearly featureless.

Look at figure 14 23. Click card to see definition. A geologist aboard a deep sea research vessel has collected several drill cores of oceanic crust from the bottom of the ocean. 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.

Both a and b are correct. Along constructive divergent plate boundaries. But despite their name these plains are not uniformly flat. The deep ocean floor is flat and nearly featureless.

Rates of sea floor spreading are equal to sea floor consumption. The deep ocean floor is flat and nearly featureless. Abyssal plain question 11 1 out of 1 points correct at transform plate boundaries. Temperature the lithosphere is cooler than the asthenosphere.

The primary difference between lithospheric and asthenospheric mantle is. This is the youngest part of the ocean floor that is. Plates slip past each other. The smooth flat regions that make up 40 of the ocean floor are the abyssal plain.

Sunlight does not penetrate to the sea floor making these deep dark ecosystems less productive than those along the continental shelf.