Continents

The biggest is Asia, and the smallest is Australia.

Alfred Wagner find the sea were move 255 million years ago the earth continents were one and it was call pangea. as years pass the earth continents separate and thats why different fossil are found on different continents.

Yes, scientists support the theory of plate tectonics, which explains how the continents have drifted and continue to do so. The movement of the Earth's plates is driven by processes such as seafloor spreading and subduction, which are part of a cycle that has occurred over millions of years. The movement of continents is not exactly repetitive but rather a continuous process that shapes the Earth's surface.

Comparing the shapes of continents with the shapes of Earth's plates can provide insights into past plate movements. The jigsaw-like fit of continents, such as South America and Africa, indicates that they were once connected and have since drifted apart due to plate tectonics. Similar shapes of continental margins or continental shelves can suggest that they were once part of the same landmass before separating.

Detroit is located in North America, specifically in the state of Michigan, United States.

Antarctica is the flattest and driest continent on Earth. It has the highest average elevation of all the continents and receives very little precipitation, with some parts being classified as polar deserts.

The single landmass that once contained all of Earth's continents is called Pangaea. It existed during the late Paleozoic and early Mesozoic eras, before breaking apart into the continents we recognize today.

Continents collide when tectonic plates collide. For example, let's look at Europe and Africa. Europe is located on the Eurasian Plate while Africa is located on the African Plate. The African Plate is currently colliding with the Eurasian Plate. In the future, this will cause the Mediterranean Sea to disappear and the Mediterranean Mountains will form. When continents collide, mountains are usually formed. In addition, they form a new connected landmass.

Tectonic plates can also scrape against each other, which causes an earthquake.

The eastern part of the Australian continent, particularly in Queensland and New South Wales, has spent the most time underwater over the last 600 million years. This region has experienced several marine transgressions and regressions, resulting in the deposition of marine sediments and the formation of marine fossils.

It is subjective to label a continent as the "dirtiest," as pollution levels vary across regions within continents. However, continents with high population density and industrial activity such as Asia and Africa often face significant pollution challenges.

Alfred Wegener (a meteorologist - someone who studies the weather) was the man who saw that there were both fossils in brazil and africa. He also noticed that the coast fitted together, like a jigsaw. His theory was that there has been one big continent, which he named Pangaea. In 1912, there was no way of measuring the up to 10cm per year moving if the continents. Geologists believed that there has been a giant land-bridge between brazil and africa. In 1960, he was proved correct, because there were ways of measuring continental drift.

TH

A continent that extends underwater is called a submerged continent. An example of a submerged continent is Zealandia in the South Pacific Ocean.

North America: Varied climates from arctic in the north to tropical in the south. South America: Also varied, from tropical in the north to temperate in the south. Europe: Mostly temperate climate with some areas experiencing arctic or Mediterranean conditions. Asia: Diverse, with arctic conditions in the north and tropical in the south. Africa: Mostly tropical, with desert regions in the north. Australia: Mostly arid or semi-arid, with some temperate regions. Antarctica: Extremely cold and dry, with icy conditions prevailing.

The name of Earth's single landmass before it split into separate continents was Pangaea. It existed during the late Paleozoic and early Mesozoic eras, approximately 335-175 million years ago.

The first original land mass is called Pangaea. It was a supercontinent that existed about 335 million years ago, before breaking apart into the separate continents we have today.

There are traditionally seven continents: Africa, Antarctica, Asia, Europe, North America, Australia, and South America.

Europe is often nicknamed the "continent of science" due to its rich history of scientific advancement and groundbreaking discoveries made by European scientists throughout history. This reputation for scientific innovation is further solidified by the presence of prestigious institutions, research centers, and scientific collaborations in Europe.

The continents used to all be connected, which means animals were free to roam. If they were free to roam, then they obviously spread out throughout the continent. So when this continent separated, the same species ended up on new continents because they had originally spread out.

The process in which Earth's continents slowly move over time is called plate tectonics. This movement is driven by the motion of the Earth's tectonic plates, which float on the semi-fluid asthenosphere below them. Over millions of years, this movement can result in the formation of mountains, earthquakes, and volcanic activity.

The theory of plate tectonics explains that the continents have moved and shifted over millions of years due to the movement of tectonic plates. Initially all the continents were part of a supercontinent called Pangaea, which began breaking apart around 200 million years ago. The movement of these plates continues to this day, causing the continents to drift and form the shapes and positions we see today.

The cohesion of the supercontinent was primarily caused by the movements of tectonic plates. Plate tectonics brought the various landmasses together through processes like continental drift and convergent boundaries, ultimately leading to the formation of the supercontinent.

If you are referring to Pangea, the theorized land mass that all continents were once part of, they know this because of the continents' puzzle like features, because things most likely exploded apart, causing the seemingly random shapes of the shores of the continents.

The coordinates 30 S and 20 E point to the continent of Africa.

A continent-continent collision can produce large mountain ranges, such as the Himalayas formed by the collision between the Indian Plate and the Eurasian Plate. This collision typically results in intense folding and faulting of the Earth's crust, leading to the uplift of rocks and the creation of deep mountain roots.

The theory that explains how continents moved apart is called plate tectonics. It proposes that the Earth's lithosphere is divided into several large plates that move and interact with each other, causing phenomena like continental drift, earthquakes, and volcanic activity.