Who_obtained_new_information_about_the_continents_and_their_coastlines_400_years_ago
Who_obtained_new_information_about_the_continents_and_their_coastlines_400_years_ago
i think it was Alfred wegener or explorers
I believe Alfred Wegner
Unless you are over 400 years old, or psychic, or a liar, you will say that you know nothing at all about it. The part of Shakespeare's life during which he left for London is called the "Lost Years" because we have absolutely no information on it.
July 18 & 19, 2009 See site for Massassauga's of Scugog Island site for futher information.
I have a table made by the Chicago Table bed Company & am trying to find info as well. Please advise if information becomes avaiable. Thanks
Let Ashley's current age be ( x ). Then, Alfonso's age is ( x + 8 ). Five years ago, Ashley was ( x - 5 ) and Alfonso was ( x + 3 ). Setting up the equation based on the information given: ( x + 3 = 3(x - 5) ). Solving this gives ( x = 11 ), so Ashley is currently 11 years old.
I believe Alfred Wegner
The continents fit together like puzzle pieces because they were once part of a supercontinent called Pangaea, which broke apart over millions of years due to the movement of tectonic plates. This phenomenon, known as continental drift, explains the similarities in the coastlines of different continents.
Mostly. Although some positions will shift and Coastlines will change. However, it is not enough to be considered a difference.
Pangaea was a supercontinent that existed about 335 million years ago and began to break apart around 175 million years ago, eventually forming the continents we recognize today. Evidence for Pangaea's existence includes the fit of the coastlines of continents, similar rock formations and mountain ranges across continents, and the distribution of fossils of the same species on different continents.
Continental drift is the theory that the Earth's continents have drifted apart from a single landmass known as Pangea over millions of years. This movement is due to the shifting of tectonic plates on the Earth's surface. This theory is supported by evidence such as the matching coastlines of continents, similar rock formations, and fossils found on different continents.
As the continents moved further apart, natural erosion of the coastlines removed and added to the basic shape over billions of years. Much of the evidence relates to the similarities of plants and animals found on now separate continents. Geological evidence points to Antarctica was once further north and had a tropical climate!
The shapes of the continents provide evidence of past tectonic activity, such as the splitting of continents through plate tectonics. For example, the fit of the continents' coastlines, like the matching shapes of South America and Africa, suggests they were once joined. This helps us understand the movement of Earth's plates over millions of years.
As the continents moved further apart, natural erosion of the Coastlines removed and added to the basic shape over billions of years. Much of the evidence relates to the similarities of plants and animals found on now separate continents. Geological evidence points to Antarctica was once further north and had a tropical climate!
The continents look the way they do today due to the movement of tectonic plates over millions of years. Plate tectonics have caused the continents to drift apart, collide, or slide past each other, leading to the current configuration. This process also influences the shapes of coastlines and mountain ranges.
Pangaea was a supercontinent that existed about 335 million years ago, supported by evidence such as the matching coastlines of continents, similar fossils found on different continents, and the distribution of certain rock formations. Plate tectonics theory explains how Earth's continents have drifted over time, eventually breaking apart Pangaea into the continents we have today.
As the continents moved further apart, natural erosion of the Coastlines removed and added to the basic shape over billions of years. Much of the evidence relates to the similarities of plants and animals found on now separate continents. Geological evidence points to Antarctica was once further north and had a tropical climate!
Africa and South America are two continents that are similar in physical shape, due to the resemblance of their coastlines. This similarity is explained by the theory of continental drift and the separation of the landmass Pangaea millions of years ago.