What is gondwana land?

Answer 1

Gondwana land no longer exists. It has to do with the theory of tectonic plates. At one time the continents of Africa, South America, Australia, Antarctica, the sub continent of India, and the Island of New Zealand one body of land. That piece of land split apart and became the pieces of land they are today.

The animals and plants on that piece of land explain the close connection between many of the creatures that exist on those separated pieces and why those pieces of land can fit together like a jigsaw puzzle. For example, the flightless Ostrich of Africa is closely related to the Rhea of South America. Both are closely related to the Kiwi of New Zealand.

Answer 2

For hundreds of millions of years, all the land of Earth was joined together in one large mass or super continent. Scientists call it Pangaea (meaning "all lands" in Greek)

Then about 200 million years ago the land began to drift apart. It broke into two pieces, and scientists have called the continent in the north Laurasia and the continent in the south Gondwanaland. Gondwanaland included what we know as Antarctica, which was joined to South America, Africa, India, and Australia.

The two large continents continued to break apart into the smaller continents that exist today. Scientists call this movement 'continental drift'

Gondwanaland was named by Eduard Suess, an Austrian geologist. The name he chose was after a district in India where the fossil plant Glossopteris was found. Suess said that because this fossil plant could be found in India, South America, southern Africa, Australia, and Antarctica, then all the lands must once have been joined together.

Gondwanaland was a hot and dry place with rainy seasons. The first tree ferns and coniferous trees appeared there. Dinosaurs lived there at one time too.

The top layer of the Earth's crust is made up of large sections called tectonic plates. Some are oceanic plates, located in the oceans, and some are continental plates carrying continents on top of them. The plates all move very very slowly and in different directions. Where they meet is called a boundary. At some boundaries the plates move apart and liquid rock seeps into the valley that results. It hardens and becomes new crust. At some boundaries two plates collide, and one is forced up, forming mountains. The other is forced down and part of it goes into the Earth's core and melts. At other boundaries, the two plates grind together as they pass in different directions, but neither is changed. Earthquakes occur along the boundary as the plates grind each other.

　

In geologic terms, a plate is a large, rigid slab of solid rock. The word tectonics comes from the Greek root "to build." Putting these two words together, we get the term plate tectonics, which refers to how the Earth's surface is built of plates. The theory of plate tectonics states that the Earth's outermost layer is fragmented into a dozen or more large and small plates that are moving relative to one another as they ride atop hotter, more mobile material. Before the advent of plate tectonics, however, some people already believed that the present-day continents were the fragmented pieces of preexisting larger landmasses ("supercontinents").

Answer 3

Gondwanaland (also Gondwana) was a super-continent that existed during a long period ending about 200 million years ago, which broke up into India, Arabia, Africa, Australia, South America, and Antarctica. It formed the Southern Hemisphere portion of Pangaea, the single continental landmass of the Earth at the time. The northern half is referred to as Laurasia, which formed Eurasia, North America, and Greenland.

Answer 4

Gondwana Land was a supercontinent that existed from the Late Paleozoic era until the Mesozoic era. It consisted of present-day South America, Africa, Antarctica, Australia, the Indian subcontinent, and the Arabian Peninsula. Gondwana Land eventually broke apart, leading to the continents we have today.

Answer 5

Gondwana included parts of all the modern day continents except North America.