Sexual coment
narrower than those of the Atlantic and are not covered with thick layers of sediment
Large flat areas of the ocean floor are called abyssal plains. These regions are typically covered in thick layers of fine sediment and are among the flattest, most featureless parts of the ocean floor. Abyssal plains are found at depths between 3,000 and 6,000 meters.
the crust will cool to form metamorphic rock
The mantle
Large areas of sea floor are covered with thick layers of sediment containing calcium due to the accumulation of calcium carbonate shells and skeletons from marine organisms over time. This process, known as biomineralization, contributes to the formation of limestone and other calcium-rich sediments.
Antartica has no agriculture, the ground is covered with thick layers of ice.
Adjacent seas were covered by shallow oceans. Over a period of millions of years the remains of marine animals and plants fell to the sea floor, they accumulated into thick layers and eventually were covered by layers of sand and silt. Over time, the immense weight of all of these layers compressed the lower layers into sedimentary rock. Bacterial actions, heat, and pressure converted the remains of the animals and plants into oil. The middle east was one covered in ocean, hence why they have so much sand, there are even places in the desert where you can go shark tooth hunting.
The forest floor was covered with thick vegetation.
the thickest accumulation of sediment on the ocean floor is at the CONTINENTAL SLOPES AND RISES. :)
Since the following options are not stated a person will not know which would most likely be covered with thick turbidite layers. Including this information would allow a person to know the right answer.
The thick slime on the ocean floor is commonly referred to as marine mucilage. Marine mucilage is a gelatinous substance formed by the aggregation of organic matter in seawater, and it can harm marine life by depleting oxygen levels as it decomposes.
In a restricted ocean as opposed to a closed ocean, as the restricted ocean evaporates, more salty water enters from outside. This continuously replenishes the salt that is being deposited allowing for thick evaporate layers to form. Many examples actually show that the new water episodically enters the evaporating ocean.