The third layer of the ocean is the Bathypelagic Zone. This is also called the dark zone. There is no sunlight in this zone, and it extends from 1,000 meters to about 4,000 meters in depth. The pressure is extremely high in this zone.
The water table is located at the top of the zone of saturation, where soil and rock are completely saturated with water. It is not generally found under the zone of saturation. The water table is typically above the layer of bedrock. It is usually located above the layer of bedrock, not below it.
The layer surrounding the core of the sun is the radiative zone. This zone is responsible for transferring energy produced in the core to the outer layers of the sun through the process of radiation.
The upper layer of an aquifer is called the unsaturated zone or vadose zone. This zone is located above the water table where the pore spaces are filled with both air and water. It acts as a buffer between the surface and the saturated zone below.
The second innermost layer of the sun is the radiative zone. This layer is where energy generated in the sun's core is conveyed through radiation as the photons bounce between atoms until they reach the convective zone.
The radiation zone is the sun's thickest layer.
The ceiling to the weather zone is the Tropopause.
There is an ozone layer. It protects us from the UV rays.
1.surface layer 2.zone of aeration 3.zone of saturation
The third layer of the ocean is the Bathypelagic Zone. This is also called the dark zone. There is no sunlight in this zone, and it extends from 1,000 meters to about 4,000 meters in depth. The pressure is extremely high in this zone.
No, the nortical zone and the middle layer of the ocean are not the same. The nortical zone refers to the region of the ocean near the surface where there is abundant sunlight. The middle layer, also known as the mesopelagic zone, is the twilight zone where sunlight is limited and deeper-sea creatures reside.
The second layer from the center of the sun is Convection Zone.
The second cooler layer of ocean water is called the thermocline. It is the region of rapidly decreasing temperature with depth, typically found between the warmer surface layer (epipelagic zone) and the colder deep layer (abyssal zone) in the ocean.
radiative zone
atmosphere
photic zone.
From the Sun's core, energy moves through the radiative zone, across the tachocline (transition layer) to the convective zone, and then to the outer convective zone with its visible granulation.