The continents are currently in their present shapes due to the movement of tectonic plates over millions of years. The Earth's surface is divided into several major plates that are constantly shifting, causing the continents to move and change position. This movement, known as plate tectonics, is responsible for the current shapes and positions of the continents.

The two supercontinents that Pangaea split up into were Laurasia and Gondwana. Laurasia eventually formed North America, Europe, and Asia, while Gondwana formed South America, Africa, Antarctica, Australia, and the Indian subcontinent.

Alfred Wegener named his supercontinent "Pangaea," which means "all lands" in Greek. He proposed the concept of Pangaea in his theory of continental drift, suggesting that all continents were once connected as one large landmass before drifting apart to their current positions.

Gondwana was a supercontinent that existed during the Paleozoic and Mesozoic eras, before breaking apart into the continents we have today. It included landmasses that now make up South America, Africa, Antarctica, Australia, the Indian subcontinent, and Arabian Peninsula. Its breakup played a crucial role in the geographical evolution of Earth.

The area of Pangaea is estimated to have been around 213 million square kilometers. It was a supercontinent that existed between 335 and 175 million years ago before breaking apart into the continents we know today.

A. Pangaea: Supercontinent
B. Panthalassa: Super ocean
C. Himalayas: Caused by continents colliding
D. Magma: Generated in subduction zones

The splitting of Pangaea led to a global rise in biodiversity. As the single supercontinent broke apart, different species were isolated on separate landmasses, leading to the evolution of new species and diverse ecosystems. This increase in biodiversity laid the foundation for the variety of life forms we see on Earth today.

Some of the land masses that were part of Pangaea include Laurasia, Gondwana, Angaraland, and Siberia. These land masses eventually broke apart and drifted to form the continents we have today.

The Atlantic Ocean is the name of the large sea that formed as Pangaea broke apart around 175 million years ago.

The supercontinent is called Pangaea. It existed during the late Paleozoic and early Mesozoic eras before breaking apart into Laurasia and Gondwana, which eventually formed the continents we have today.

Pangaea was a supercontinent that existed about 300 million years ago, consisting of almost all of Earth's landmasses fused together. It began breaking apart about 175 million years ago, leading to the formation of the continents we have today. Pangaea created a single large ocean, called Panthalassa, surrounding it.

Present-day land areas that were part of the supercontinent Pangaea include South America, Africa, Antarctica, Australia, India, and parts of Europe and North America. These landmasses were all connected together before the breakup of Pangaea.

There is no specific information provided about Mr. Freeman, so it is unclear what you are referring to. Can you provide more context or details?

Pangaea began to break apart around 175 million years ago during the Jurassic period. This breakup eventually led to the formation of two separate landmasses known as Laurasia (in the north) and Gondwana (in the south).

• Antarctica
• South America
• Africa
• Madagascar
• Australian
• Arabian Peninsula
• India

Gondwana included present-day South America, Africa, Antarctica, Australia, and the Indian subcontinent. Laurasia included present-day North America, Europe, and Asia. Pangaea was the supercontinent that existed before the breakup to form Gondwana and Laurasia.

Australia has moved the most since Pangaea, shifting over 4000 kilometers from its original position.

Antarctica was connected to the supercontinent Gondwana, located near the South Pole, around 250 million years ago during the late Paleozoic and early Mesozoic eras. Over millions of years, tectonic plate movements caused Antarctica to drift to its current location in the southern hemisphere.

Yes, millions of years ago, Antarctica was located closer to the equator within a warmer climate. This was due to the shifting of tectonic plates and changes in Earth's orbit and axial tilt.

Pangaea was a supercontinent that existed around 335-175 million years ago. It was made up of all of Earth's continents joined together as a single landmass. Pangaea began to break apart due to the movement of tectonic plates, leading to the formation of the continents we have today.

Wegener named the supercontinent he proposed "Pangaea," which he believed existed before breaking apart into the continents we have today. The name "Pangaea" is derived from Greek, meaning "all lands."

Some advantages of Pangaea include increased connectivity of the landmasses which facilitated species migration between continents, creating wider ranges of biodiversity. It also enabled the exchange of flora and fauna, contributing to a richer ecosystem. Additionally, the formation of Pangaea influenced the distribution of resources which could have led to the development of different species with unique adaptations.

The countries that were once connected by the supercontinent Pangaea include the landmasses that now form North America, South America, Africa, Europe, Asia, and Antarctica. These modern continents were all part of Pangaea before they broke apart due to tectonic plate movement.

Pangaea separated into Laurasia (North America, Europe, and Asia) and Gondwana (South America, Africa, Antarctica, Australia, and the Indian subcontinent) during the Mesozoic Era.

The two landmasses that split from Pangaea are Laurasia and Gondwana. Laurasia eventually formed North America, Europe, and Asia, while Gondwana formed South America, Africa, Antarctica, Australia, and the Indian subcontinent.