a stratification is a term generally used for layering of sediments. Thus a "stratified" ocean is one in which a layer of sediments accumulate at the bottom of the ocean and over time, sediment infill from the continents fill up small local areas around the points where fresh water meets saline ocean water. These areas fill with so much sediments, eventually they become stratified with sediment layers and dry up.
The Earth's temperature, density, and chemical composition form layers within the planet, leading to stratification. The Earth is stratified based on its internal structure, such as the core, mantle, and crust. Each layer has distinct physical and chemical properties that contribute to the Earth's overall composition and behavior.
The thermohaline circulation is a term for the global density-driven circulation of the oceans. Derivation is from thermo- for heat and -haline for salt, which together determine the density of sea water
The atmosphere sits above Earth's oceans due to gravity, which pulls all matter towards the center of the planet. The density of air is lower than that of water, so it occupies the space above the oceans. Temperature and pressure also play a role in determining the vertical distribution of the atmosphere.
Density plays a part in the layers of the Earth because it determines the distribution of materials based on their mass. The inner core is the densest layer due to the high pressure and temperature, while the less dense materials are found in the outer layers such as the crust and mantle. This stratified structure is a result of the gravitational sorting of materials during the Earth's formation.
Glacial till is unsorted and unstratified sediment deposited directly by a glacier, while stratified drift is sorted and stratified sediment deposited by glacial meltwater. An example of glacial till is a moraine, which is a ridge of mixed debris left behind by a moving glacier. An example of stratified drift is an outwash plain, which is a flat, gently sloping area formed by the deposition of sorted sediments carried by glacial meltwater.
The ocean is stratified with denser layers below less dense layers.
it satisfies :)
Torbjorn Spurkland has written: 'The effect of boundary geometry on internal density currents in a density stratified reservoir' -- subject(s): Reservoirs
oceans stuff
Layered.
Stratified rocks have a defined horizontal layering.
Simple columnar epithelium cells will heal faster than stratified squamous cells. The stratified squamous cells rarely have contact with blood.
It's due to the chemical reaction of the co2 on the ocean water, since there is no salt the density increases
A couple of synonyms for stratified are flaky, laminated, or stratiform.
The Earth's temperature, density, and chemical composition form layers within the planet, leading to stratification. The Earth is stratified based on its internal structure, such as the core, mantle, and crust. Each layer has distinct physical and chemical properties that contribute to the Earth's overall composition and behavior.
Stratified squamous epithelium lines the mouth and serves to protect the underlying tissues from mechanical stress and abrasion. This type of epithelium has multiple layers of flat cells that help resist wear and tear.
Stratified: I disagree with stratified, the answer is "simple" arrangement.