Continents

Armeria is a genus of flowering plants in the family Plumbaginaceae. It is not located on a continent because it is a genus of plants, not a physical location.

Wegener's background as a climatologist helped him notice similarities in rock formations, fossils, and geological structures between continents separated by vast oceans. He realized that these similarities could not be explained by existing theories about seafloor spreading or continental drift. This led him to propose the groundbreaking theory of continental drift, suggesting that the continents were once connected and have since moved apart.

Alfred Wegner thought that all the continents used to be one giant landmass called Pangea. He said that the continents would move a little each year. The scientists didnt believe him though, but later found out that it could be true because of the plates in the earth

It is estimated that Earth's continents have come together to form a super-continent around three times in the last 600 million years. This cycle of continents coming together and then breaking apart is known as the supercontinent cycle. Examples of supercontinents include Pangea, Rodinia, and Columbia.

Yes, the 7 continents on Earth were once joined/fitted together about 250 million years ago, forming a supercontinent named Pangaea. It then splitted into 2 smaller supercontinents, Laurasia, consisting of North America, Asia & Europe and Gondwanaland, consisting of South America, Oceania, Antarctica & Africa, which then drifted apart to where they are now.

The Gulf of Thailand lies within the coastline of Thailand, Cambodia, and Vietnam. It is an extension of the South China Sea and is known for its stunning beaches and diverse marine life.

Asia is Earth's biggest continent, covering around 30% of the planet's land area and hosting a diverse range of cultures and landscapes.

its hard to say it but i know it.it is Africa,Asia,south and north America and also these Antarctica the same as artic it is a synonym

The hypothesis that proposed that Earth's continents were once joined in a single land mass is called continental drift. This theory, formulated by Alfred Wegener in the early 20th century, suggested that the continents were once part of a supercontinent called Pangaea that later broke apart and drifted to their current positions.

In 20 million years, the continents will continue to slowly shift due to plate tectonics. Some predictions suggest that the continents will move closer together, potentially creating a new supercontinent similar to Pangea, although this process occurs over hundreds of millions of years. Geologic time scales are vast, and while we can make educated guesses based on current plate movements, predicting exact positions is challenging.

Australia is located near major air and sea routes, making it a common transit point for international travel and trade. Additionally, Australia is a popular destination for migratory birds flying to and from Southeast Asia and other regions. The Great Barrier Reef off the coast of Australia is a prominent marine highway for a diverse range of marine life.

Antarctica is the most southerly continent on Earth. It is located at the South Pole and is mostly covered in ice.

Antarctica is geologically stable, as it sits on a tectonic plate away from major plate boundaries. Australia, the interiors of South America, and Africa are also relatively stable, with fewer tectonic activities compared to regions along the Pacific Ring of Fire.

The hypothesis that Earth's continents were once joined in a single landmass and then gradually moved apart is known as the theory of continental drift, proposed by Alfred Wegener in 1912. This theory laid the foundation for the development of the theory of plate tectonics.

The theory is called "plate tectonics," which explains how Earth's outer shell is divided into several large plates that move and interact with each other. This movement is responsible for the shifting of continents, earthquakes, volcanic activity, and the formation of mountain ranges.

Antarctica is the continent with no permanent residents except for researchers. The harsh climate and remote location make it inhospitable for permanent human settlement.

Yes, the upper layer of Earth is broken into more than a dozen large tectonic plates that move very slowly in various directions. These movements can cause earthquakes, volcanic activity, and the formation of mountains.

Australia is often referred to as the "land of superlatives" due to its unique and diverse natural features, such as the Great Barrier Reef, Uluru (Ayers Rock), and the Outback. These landmarks are among the world's largest, oldest, and most distinctive geological formations.

Alfred Wegener called the large supercontinent that once existed Pangaea.

Alfred Wegener hypothesized that the continents were once connected in a single supercontinent called Pangaea. He suggested that the continents drifted apart over millions of years due to the process of continental drift.

200 million years ago the continent of Pangaea was beginning to break up. At this time there were only two continents; Laurasia in the north and Gondwanaland in the south separated by the Tethys Sea.

Chinese surely. They make up 1/5 of the World's population and nearly 30% of Eurasia's population.

The term "Pangaea" was coined by German scientist Alfred Wegener in the early 20th century. It is derived from the Greek words "pan" meaning all, and "gaea" meaning earth, to represent the idea of a supercontinent where all land masses were once connected before breaking apart into separate continents.

The theory that explains how continents move apart is called plate tectonics. This theory suggests that the Earth's lithosphere is divided into several rigid plates that float on the semi-fluid asthenosphere below. These plates can move relative to each other, causing continents to separate due to processes such as seafloor spreading at divergent plate boundaries.

Continents formed through the process of plate tectonics, where the Earth's lithosphere is divided into several large and small plates that move slowly over the semi-fluid asthenosphere beneath them. The movement of these plates causes them to collide, separate, or slide past each other, leading to the formation and shifting of continents over millions of years. The process is ongoing and continues to shape the Earth's surface.