Pangaea Supercontinent

Pangea does not exist anymore so it cannot be seen from space.

However when it did exist it might have looked vaguely like the image above.

Rodinia is a supercontinent that existed in the late Proterozoic, from about 1300 million years ago to it's breakup 600 million years ago.

The first continents formed through a process called plate tectonics, where tectonic plates collided and merged over millions of years. These collisions created mountain ranges and landmasses that eventually evolved into the continents we have today. The process is ongoing, with continents continually shifting and changing position.

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The present shape of the continents does not fit perfectly into the shape of a supercontinent because the Earth's tectonic plates are constantly moving. These movements are driven by processes like plate tectonics and convection currents in the mantle, causing the continents to drift apart, collide, and rearrange over millions of years. This results in the continents having different shapes and positions compared to when they were part of a single supercontinent like Pangaea.

Houses 200 years ago varied in size and style, but common features included wood or stone construction, thatched roofs, and multiple floors. They often had small windows with shutters, and were designed to be functional and practical for the needs of the time. Interior layouts typically included small rooms and fireplaces for heating.

The four plates that make up the Mid Atlantic ridge are the North and South American Plates, the Eurasian plate, and the African Plate.

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True. The formation of Pangaea, a supercontinent that existed around 300 million years ago, caused significant climate changes on Earth. The shifting of landmasses and changes in ocean currents resulted in altered patterns of rainfall and temperature distribution, affecting global climate patterns.

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When Pangaea broke apart into two pieces, the northern portion was called Laurasia and the southern portion was called Gondwana. These landmasses eventually formed the continents we have today.

Pangea split in the Triassic period.

The theory is known as plate tectonics. It suggests that the Earth's outer shell is divided into several large, rigid plates that move relative to each other. The movement of these plates explains the positions of continents and ocean basins and supports the concept of continental drift.

Warm interglacial periods occur approximately every 100,000 years, alternating with colder glacial periods. These cycles are driven by variations in Earth's orbital parameters known as Milankovitch cycles. The most recent warm interglacial period we are currently in is called the Holocene epoch.

pangae was a super big land the was about 4.5 million years ago. all seven land masses was pangae back then.

3 cm

because i sead so

No. Pangaea is thought to have broken up about 240 million years ago during the Triassic Period, while early man only evolved during the last few million years.

The last supercontinent.

I know there were Lithosaurus.

once

but in the distant future the continents will thus drift together hence creating another supercontinent.