South America is South of North America.
The Indian Ocean is east of Africa.
They touch the Gulf<span> of Guinea.</span>
<u>Answer:</u>
Induced climate change and its effects will proceed for a long time, and at times for a long time. Separately and by and large, and in blend with the impacts of other human exercises, these progressions posture dangers for a broad scope of social and ecological frameworks, including freshwater resources, the seaside condition, environments, farming, fisheries, social wellbeing, and national security, among others.
Earth’s physical climate framework, which incorporates the environment, seas, cry sphere, and land surface, is mind-boggling and always advancing.
It is expected that seafloor samples taken farther from land usually contain a greater proportion of biogenous sediments because sediments are thinnest on the seabed closest to spreading centres (young seafloor) and thicker distant from the ridge (older seafloor with more time for accumulation). Additionally, sediments are substantially thicker close to continents.
More about seafloor sediments:
Terrigenous, pelagic, and hydrogenous sediment are the three different types of sea floor sediment. Terrigenous sediment is deposited on the continental shelf, continental rise, and abyssal plain and is derived from the land.
Clay particles and tiny marine animal skeletons that progressively sink to the ocean floor make up pelagic sediment. Minerals that precipitate from seawater on the ocean floor, such as manganese nodules, are abundant in hydrogenous sediments.
Learn more about sediments here:
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