On the western side
one of the seven seas
The western side of continents tends to have cooler ocean temperatures because of cold ocean currents flowing towards the equator from the poles. These currents bring colder water to the western coasts, influencing the climate of the adjacent land areas.
The temperature of ocean currents is generally influenced by their geographic location relative to the equator. Warm currents, typically found on the western sides of ocean basins, flow from tropical regions towards the poles, while cold currents are usually located on the eastern sides, flowing from polar regions towards the equator. This pattern is influenced by the Coriolis effect and the prevailing wind patterns. As a result, currents can significantly affect the climate of coastal regions, with warm currents contributing to milder temperatures and cold currents leading to cooler conditions.
Deep ocean currents are in the depths of the oceans. Surface current are at the surface, not deep down. Deep ocean currents bring vitamins and nutrients to the shore, surface currents do not. Deep ocean currents are caused by salinity and temperature differences. Surface currents are cause by the force and impact of the wind.
No, in general the Atlantic basin is very young and the ocean is still getting wider each year. This means that the continents either side are moving in the same direction as the ocean floor so oceanic crust is not yet being forced down into the mantle at the basin margins.
when there is two potential , due to potential difference ,electron from -ve side(cathode) flow towards +ve side(anode)(this is nature that electrons from cathod attract by anode) , so the electron moves in the path - ---> +, so current flow opp to that flow + ---> -in
Submarine Canyons
Mountains can block the flow of air masses, causing them to cool and release moisture as precipitation on one side (windward) and create a rain shadow effect on the other side (leeward). Ocean currents can transport heat around the globe, influencing the temperature and humidity of nearby land areas. Cold currents can cool nearby coastal regions, while warm currents can warm them, affecting local climate patterns.
The Pacific Ocean is located on the western side, while the Atlantic Ocean is found on the eastern side of the United States. This geographical positioning places the Pacific Ocean to the west of the continental U.S. and the Atlantic Ocean to the east.
Eastern boundary currents are relatively shallow, broad, and slow-flowing. Western boundary currents are warm, deep, narrow, and fast-flowing currents that form on the west side of ocean basins due to western intensification.
Eastern boundary currents are relatively shallow, broad, and slow-flowing. Western boundary currents are warm, deep, narrow, and fast-flowing currents that form on the west side of ocean basins due to western intensification.
The polarities were mirror images on either side of the mid-ocean ridge.