Like the atmosphere, the ocean transports and distributes heat on Earth, helping to regulate climate.
Answer:
1. Imagine you were an archaeologist working with Sir Leonard Woolley in Iraq. Which of the discoveries do you think was the most exciting? Which discovery helped you most in determining what had happened to the people whose remains you found? Explain your answer.
Answer: I did a little more research about this I think that when I he found 1800 tombs at a Sumer grave and out of all those found 12 royal graves do you know how hard those are to find and he got twelve of them.
2. Suppose you were a historian studying ancient Sumer. How would your work be different from Woolley’s work?
Answer: Woolley was an archeologist if you want to be a historian you have to be kind of on that line but you study it more and figure out what it made of and all that stuff.
3. Sir Leonard Woolley worked on excavating Ur for twelve years. What years were they?
Answer: 1922 to 1934
4. What kinds of changes do you think will occur in the work of archaeologists in the next hundred years?
Answer: I think that archaeologist will find house, rock, and more fossils and maybe even plant that have been console in the soil.
5. Which work would you prefer, the work of the historian or the archaeologist? Why?
Answer: I will like to be an archaeologist is better because I can feel the stuff and be happy that I have found it.
Explanation: I did a lot of research to answer this question. Maybe next time go to Wikipedia it maybe be long to read but it worth It when you get an A RIGHT!
Answer Electric Force: force exerted by two charged objects. Positive/Negative Charges: two unlike charges will exert a force that attracts each other while two like charges will exert repelling forces on each other.
Explanation:
hong kong,japan,china,north korea,south korea
Answer:
Carbonate sedimentary rocks
Explanation:
Carbonate sedimentary rocks are the rocks that are primarily comprised of carbonate minerals such as calcite or aragonite. They are formed chemically. These rocks are formed when Carbon is initially trapped with the accumulation of sediments over it in association with fossil shells. They are also formed due to the dissolution or precipitation by groundwater, depending upon the temperature, pH and dissolved ions present in the solution.
They are often marked by the presence of karst topography and caves.
Some examples of these rocks are limestone and dolomite.
