Mountain chains in Europe, particularly in the British Isles and Scandinavia, provide evidence for the existence of Pangaea through their geological similarities and alignment. The Caledonian mountain range, which extends from Scotland to Scandinavia, showcases similar rock types and ages, indicating they were once part of a continuous landmass. Additionally, the distribution of fossils and geological features across these regions supports the idea that these areas were connected before the continents drifted apart during the formation of Pangaea. This evidence highlights the historical geological processes that shaped the continents and their current configurations.
Scandinavia covers an area that is approximately 880,000 km2 in size.
In Italy, the Alps. In Scandinavia, the Scandinavian mountains, also known as the Scandes.
Norway with 2469 moh.
There is no scientific evidence to suggest that mountain lions are specifically attracted to menstrual blood. Mountain lions are primarily attracted to the scent of prey animals for hunting purposes.
Evidence supporting the existence of Pangaea includes: Fossil evidence of similar species found on different modern continents. Rock formations and mountain ranges that match up when continents are rearranged. Paleoclimatic evidence, such as glacial deposits in regions that are now warmer. Similarities in geologic structures and ages of rocks across continents.
deep within the mountain ranges of Scandinavia
The Caledonian Mountains were once part of the same mountain range as Scandinavia. This mountain range formed around 400 million years ago and was created by the collision of tectonic plates. As the continents drifted apart, the range eroded, forming the modern-day landscapes of Scandinavia and the British Isles.
The mountain belts along the margins of North America, Africa and Europe line up as well and have similar rock types, indication that the continents at one time were joined as Pangea.
There are mountains in the North Pole. At Longyearbyen, the main gateway to the Norwegian Arctic, there are snow covered mountains.
Galdhøpiggen is Scandinavia's highest mountain. It reigns 2469 meters above sea level (8,100 ft).
The mountain chain is called "Skanderna", and it's from them we get the word Scandinavia.
An example of rock and mountain correlation in the theory of continental drift is the Appalachian Mountains in the eastern United States and the Caledonian Mountains in Scotland and Scandinavia. Both mountain ranges share similar rock formations and structures, providing evidence that these regions were once connected before the continents drifted apart.