It supports the theory because it can be found on all of the continents.
Since all of the continents once were formed as one big land mass, the temperature could have been warmer when Antarctica was closer to the equator.
The shapes of continents appearing on the map clearly show similar shapes and how the continents might fit together.
Coal can be found underneath the cold and dry Antarctic ice cap, though coal can only form in warm and wet conditions. This could mean that Antarctica was once together with the other continents as part of the Pangaea, and was once in a warm and humid region
Deep-sea mountain ranges had caught his attention. Alfred Wegener's fully developed theory of continental drift attempted to point out evidences that the continents were once joined into a single continent he called Pangaea. Wegener's theory hypothesized that the continents were able to push through the rock of the seafloor to their present positions. As evidence, he noted (as had others before him), of the geographic correlation in coastline perimeters of South America and Africa. This was the feature that led Wegener to investigate other clues. His investigations revealed that mountain ranges in South America and Africa, and strata and composition of coal fields in Europe and North America matched or lined up. Additionally, matching reptilian fossils were found on either side of the ocean, indicating that the continents were once joined together. Although he was unable to find a mechanism for his proposed continental drift theory, he also observed that the more shallow an ocean, the younger its geologic age. It wasn't until the 1950's and 1960's, with the discovery of the Mid-Atlantic Ridge (and other sea floor mapping discoveries) that Wegener's hypothesis started to become more accepted. The newer science of plate tectonics owes much to Wegener's scientific groundwork. sdhtshehdtubt6yhsx ryjut7iyldrtysvefgb 6u fyu6uerjthe5tjkj jgyuftyk
Alfred Wegener's fully developed theory of continental drift attempted to point out evidences that the continents were once joined into a single continent he called Pangea. Wegener's theory hypothesized that the continents were able to push through the rock of the seafloor to their present positions. As evidence, he noted, as had others before him, of the geographic correlation in coastline perimeters of South America and Africa. This was the feature that led Wegener to investigate for other evidences. His investigations revealed that mountain ranges in South America and Africa, and strata and composition of coal fields in Europe and North America matched or lined up. Additionally, matching reptilian fossils were found on either side of the ocean, indicating that the continents were once joined together. Although he was unable to find a mechanism for his proposed continental drift theory, he also observed that the more shallow an ocean, the younger its geologic age. It wasn't until the 1950's and 1960's, with the discovery of the Mid-Atlantic Ridge, and other sea floor mapping discoveries that Wegener's hypothesis started to become more accepted. The newer science of plate tectonics owes much to Wegener's scientific groundwork.
Wagner has a theory on continental drift and the evidence that did not support it is where we see the continental drift in examining species of animal and human life drifting from continent to continent without the aid of mechanical devices or some form of trasportation except for by their own feet and them being the drifters of the continents.
Continental Drift. The land mass wasn't always at the poles so could support forests that then got covered to become coal. Climate Change's another. Earth maybe WAS warm enough at the pole but the climate as a whole warm enough to support foorests there.
Since all of the continents once were formed as one big land mass, the temperature could have been warmer when Antarctica was closer to the equator.
Because coal is usually found in tropical areas, but Pennsylvania is not a tropical area.
The shapes of continents appearing on the map clearly show similar shapes and how the continents might fit together.
Proof of Continential drift is that they found fossils of the same animals and plants on different continents.They also found the same rock patterns on different continents.Also some continents fit together likea jigsaw puzzle.
This question is simply too general, but i'll give you the definition and an example of the geological evidence of Pangaea.Definition: evidence that geologically prove the existant of such theory inrelation to being of the past (on most occaisions)A geological example of evidence of the existant of Pangaea is how there are coal mines in Antarctica. Coal mines only form near the equator, therefore proving that continental shift was involved and that there was once a "Pangaea".
Coal can be found underneath the cold and dry Antarctic ice cap, though coal can only form in warm and wet conditions. This could mean that Antarctica was once together with the other continents as part of the Pangaea, and was once in a warm and humid region
No
Yes, both can be mined from the continental shelf.
Deep-sea mountain ranges had caught his attention. Alfred Wegener's fully developed theory of continental drift attempted to point out evidences that the continents were once joined into a single continent he called Pangaea. Wegener's theory hypothesized that the continents were able to push through the rock of the seafloor to their present positions. As evidence, he noted (as had others before him), of the geographic correlation in coastline perimeters of South America and Africa. This was the feature that led Wegener to investigate other clues. His investigations revealed that mountain ranges in South America and Africa, and strata and composition of coal fields in Europe and North America matched or lined up. Additionally, matching reptilian fossils were found on either side of the ocean, indicating that the continents were once joined together. Although he was unable to find a mechanism for his proposed continental drift theory, he also observed that the more shallow an ocean, the younger its geologic age. It wasn't until the 1950's and 1960's, with the discovery of the Mid-Atlantic Ridge (and other sea floor mapping discoveries) that Wegener's hypothesis started to become more accepted. The newer science of plate tectonics owes much to Wegener's scientific groundwork. sdhtshehdtubt6yhsx ryjut7iyldrtysvefgb 6u fyu6uerjthe5tjkj jgyuftyk
Deep-sea mountain ranges had caught his attention. Alfred Wegener's fully developed theory of continental drift attempted to point out evidences that the continents were once joined into a single continent he called Pangaea. Wegener's theory hypothesized that the continents were able to push through the rock of the seafloor to their present positions. As evidence, he noted (as had others before him), of the geographic correlation in coastline perimeters of South America and Africa. This was the feature that led Wegener to investigate other clues. His investigations revealed that mountain ranges in South America and Africa, and strata and composition of coal fields in Europe and North America matched or lined up. Additionally, matching reptilian fossils were found on either side of the ocean, indicating that the continents were once joined together. Although he was unable to find a mechanism for his proposed continental drift theory, he also observed that the more shallow an ocean, the younger its geologic age. It wasn't until the 1950's and 1960's, with the discovery of the Mid-Atlantic Ridge (and other sea floor mapping discoveries) that Wegener's hypothesis started to become more accepted. The newer science of plate tectonics owes much to Wegener's scientific groundwork. sdhtshehdtubt6yhsx ryjut7iyldrtysvefgb 6u fyu6uerjthe5tjkj jgyuftyk