During the Triassic, almost all the Earth's land mass was concentrated into a single supercontinent centered more or less on the equator, called Pangaea. From the east a vast gulf entered Pangaea, the Tethys sea. It opened farther westward in the mid-Triassic, at the expense of the shrinking Paleo-Tethys Ocean, an ocean that existed during the Paleozoic. The remaining shores were surrounded by the world-ocean known as Panthalassa. All the deep-ocean sediments laid down during the Triassic have disappeared through subduction of oceanic plates; thus, very little is known of the Triassic open ocean. The supercontinent Pangaea was rifting during the Triassic-especially late in the period-but had not yet separated. The first nonmarine sediments in the rift that marks the initial break-up of Pangaea-which separated New Jersey from Morocco-are of Late Triassic age; in the U.S., these thick sediments comprise the Newark Group. Because of the limited shoreline of one super-continental mass, Triassic marine deposits are globally relatively rare, despite their prominence in Western Europe, where the Triassic was first studied. In North America, for example, marine deposits are limited to a few exposures in the west. Thus Triassic stratigraphy is mostly based on organisms living in lagoons and hypersaline environments, such as Estheria crustaceans.
At the beginning of the Mesozoic Era, Africa was joined with Earth's other continents in Pangaea. Africa shared the supercontinent's relatively uniform fauna which was dominated by theropods, prosauropods and primitive ornithischians by the close of the Triassic period. Late Triassic fossils are found through-out Africa, but are more common in the south than north. The boundary separating the Triassic and Jurassic marks the advent of an extinction event with global impact, although African strata from this time period have not been thoroughly studied.
some what like panagea
i believe roughly 70% (not completely sure though) I'm not really sure, but something like 70% of the earths surface..
Uranus has the surface area of 15.91 Earths. It has the volume of 63.086 Earths. It has the mass of 14.536 Earths. Its diameter is 4.007 times that of Earth. See the related link for more information.
solar energy provides a heat source for all living things on earth. we also transfer solar heat into electricity and other types of energy, using solar panels. however, only a portion of the suns energy makes it to earths surface because the ionosphere reflects some of the rays back into space. only half of the incoming ratiation from the sun makes it to the earths surface.
Well what cools it is the atmosphere and the air that we breathe from. The earth's crust is very rocky and it also could be smooth, so when it rains or snows of course the earths land is cold. It is also just like how the matter rises from the center and goes to the top then the matter packs in and then it drops then rises again then comes back up. These are called convection currents.
rough
flat and even
Type your answer here... it was wet and the surface was covered with a thin layer of warm water.
During the Tertiary Period, the surface of the earth looked much like it does today. It was quite warm with periods of cold much like today.
During the devonian time period most of land was under water.
During the Jurassic period, Earth's climate was generally warmer and more humid than today. Polar regions were ice-free, and forests covered much of the land. Dinosaurs flourished in this lush environment.
The biggest dinosaur in the Jurassic period were the gigantic sauropods like the famous Diplodocus.
Warmer climate
it was the same but there was a groped land
There was a minor extinction event at the end of the Jurassic period. It was probably caused by global climate change. Dinosaurs like Allosaurus, Ceratosaurus, Camarasaurus, and Stegosaurus couldn't adapt to the change in temperature, so they all died out. The Cretaceous period then came after the Jurassic period had ended.
well when i was there ,it was a litt;le bit hot
During the Jurassic period, the atmosphere was warmer and had higher levels of oxygen compared to today. There were lush forests with a diverse range of plant and animal species, including dinosaurs and early mammals. The climate was relatively stable and supported the evolution of many iconic prehistoric creatures.
The Cretaceous period followed the Jurassic period and lasted from about 145 million to 66 million years ago. In the Cretaceous period, flowering plants became more dominant, dinosaurs continued to diversify, and large marine reptiles like mosasaurs thrived. However, the end of the Cretaceous period marked by a mass extinction event where dinosaurs and many other species went extinct.