Answer:
Whichever one is on the bottom in the oldest.
Explanation:
Over time, dust and dirt will cover older fossils.
Answer:
Three conditions are necessary to form a glacier: (1) Cold local climate (polar latitudes or high elevation). (2) snow must be abundant; more snow must fall than melts, and (3) snow must not be removed by avalanches or wind
Explanation:
1. Countries who supply foreign aid to the developing world see domestic benefits.
Ex: Foreign aid to the developing world does create a direct cost paid voluntarily through personal remittance or involuntarily through taxpayer funds. When these payments are made, the diplomatic benefits create new trade opportunities between the two nations. Job opportunities become available through the process of monetary transfers. As the basic needs of the developing country are met, there is even the benefit of doing good for someone else to consider.
2. Countries who supply foreign aid help others solve their domestic issues.
Ex: Examples of foreign aid to counter domestic issues include money and supplies to fight HIV/AIDS, law enforcement resources to fight terrorism, military aid through the provision of training to help local police and Army activities, and food support to help farmers find new ways to increase their yields. By improving these issues or processes abroad, the country providing aid prevents them from becoming negative impacts back at home.
3. Countries who supply foreign aid reduce the impacts of poverty.
Ex: . It begins with the fact that almost 11% of the global population lives on less than $2 per day. Providing foreign aid reduces the impact of this issue, along with these other facts.
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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I believe that this is due to how Japan is near one of the plate boundaries or mid-ocean ridges, where it's easier for a tsunami (from the ridges) to accelerate its speed and for an earthquake (from the plate boundaries) to collide or interact in a myriad of ways. I know that this wasn't so specific, as you have to find the name of the ridge or plates involved in this type of action.
