Answer:
D) Jovian planets are mostly gas and liquid and terrestrial planets are solid and rocky
Explanation:
Answer and Explanation:
- The Columbian exchange basically alludes to the European pilgrim Christopher Columbus who was engaged with boundless trade or move of different plants , crops, societies, creatures, and human populace and technological thoughts between the Americas and rest of the portion of the world or the past world in the fifteenth and sixteenth century.
- Christopher Columbus was attempting to leave Europe and head west to discover Asia that was his real arrangement however he accidentally found the America.
- Over the Americas he established a lot of things that he never observed in Africa, Asia or Europe and a few things which were found in the accidentally found district of Americas were items like potatoes, corn, tomatoes and couple of creatures they had never observed that were significant, for example, Llama and furthermore diseases.
- Discussing the Columbian exchange the individuals which were dwelling in the America, the local Americans never came across things which Columbus brought to them from the ancient world, for example, Bananas, carrots, apples and animals which was significant throughout the entire existence of man, steeds.
- Columbian exchange the nourishment, plants, crops, organic products, animals, thoughts between the old world and the America were traded.
- Things traded were similarly new and amazing to the two sides of the world( Americas and the ancient world).
This is a case of how worldwide connection changed the human progress in various parts of the world.
Climate changes, loss of biodiversity, acidification and forest degradation I think.
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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