Four days ago
Pteranodon lived on the coast of the Western Interior Seaway. The Western Interior Seaway was a subtropical, shallow sea that stretched from what is now the Gulf of Mexico to Hudson Bay, splitting North America in half. Pteranodon were piscivorous, or fish eating, and would have depended on the abundant waters of the shallow sea for food.
During the Triassic and Jurassic, Wisconsin was an inland area and above water. During the Cretaceous, the Western Interior Seaway submerged the center of North America from Hudson Bay to the Gulf of Mexico, dividing the continent. Wisconsin was on the eastern shore of the Western Interior Seaway, but it was above water.
During the Mesozoic era, significant tectonic activity included the breakup of the supercontinent Pangaea, which led to the formation of the Atlantic Ocean through the process of seafloor spreading. This era also experienced the opening of the Tethys Sea and the formation of the Western Interior Seaway in North America.
Torosaurus lived along the western shore of the Western Interior Seaway at the end of the Mesozoic. The habitat was a floodplain crisscrossed by rivers. Common plants were conifers, cycads, ferns, gingkoes, and even some flowering plants.
strait of malacca
The seaway on the map is named the St. Lawrence Seaway, which is named after the St. Lawrence River. The seaway connects the Great Lakes to the Atlantic Ocean, allowing for maritime transportation between the interior of North America and the rest of the world. The St. Lawrence River and Seaway have played a significant role in the economic development of the region by providing a vital transportation route for goods.
Inland Seas were shallow seas that cover the central portion of a continent during high sea levels. In North America the Western Interior Seaway extended from the Gulf of Mexico deep into present day Canada in the Cretaceous Period.
interior plains
The western part of the interior plains in North America is called the Great Plains.
st. Lawrence seaway st. Lawrence seaway
Oceans covered western Canada during the Late Cretaceous period, approximately 100 to 66 million years ago. During this time, a large inland sea known as the Western Interior Seaway split the North American continent, allowing marine environments to extend into present-day western Canada. This geological period is significant for the preservation of rich fossil beds found in the region.
probably during the early part of the Cretaceous Period