The Cretaceous is the 3rd and final period of the Mesozoic Era geological period that continued from about 145 to 66 million years ago. It was a geologic period with a comparatively warm climate, resulting in high eustatic sea levels that shaped many shallow inland water bodies.In the Late Cretaceous, the many contemporary U.S. states were beneath the waves of the Western Interior Seaway.
Read more: North America 77 million years ago
Discover the future of Africa as tectonic movements create new oceans, alter climates, and redefine economic landscapes.
Read more: Africa 10 Million Years Later
The Central Pangean Mountains were a great mountain chain in the middle part of the supercontinent Pangaea that stretches across the continent from northeast to southwest during the Carboniferous, Permian Triassic periods.
Read more: The Scottish Highlands, the Appalachians, and the Atlas are the same mountain range, once connected as the Central Pangean Mountains
Mars is home to dizzyingly tall mountains and deep canyons. Olympus Mount is the tallest mountain in the Solar system. It’s about two and a half times taller than Mount Everest.
Read more: Mapping Mars: The Topography and Geology of the Red Planet
Looking at a rock means looking at time itself. Every stone formation around us formed through billions of years of pressure, heat, and transformation. Three remarkable global geological maps let you explore this planetary memory, from the depths of ocean trenches to the highest mountain ranges.
Read more: Three Global Geological Maps That Show 4 Billion Years of Earth’s History
The breakup of Pangaea, a supercontinent that existed around 335 million years ago, is a significant event in Earth’s geological history. Pangaea began to break apart during the Mesozoic Era, forming the continents as we recognize them today. The process of breakup and continental drift occurred due to the movement of tectonic plates beneath the Earth’s surface.
Read more: The breakup of PangaeaAccording to the tectonic theory, the cycles of splitting apart and coming together occur because of subduction, which happens when tectonic plates meet with one another.
Read more: The movement of tectonic platesRelated posts: – How to say ‘Yes’ in Europe
Read more: How to say ‘yes’ in Southeast AsiaThe map was published under the direction of Sir Archibald Geikie.
Read more: Geological Map of England and Wales (1896)