Search results
Results From The WOW.Com Content Network
Permian–Triassic boundary at Frazer Beach in New South Wales, with the End Permian extinction event located just above the coal layer [2]. Approximately 251.9 million years ago, the Permian–Triassic (P–T, P–Tr) extinction event (PTME; also known as the Late Permian extinction event, [3] the Latest Permian extinction event, [4] the End-Permian extinction event, [5] [6] and colloquially ...
The 2020 East Troublesome Fire was a massive and destructive wildfire, and the second-largest in the history of the U.S. state of Colorado.Named for the East Fork of Troublesome Creek, close to the fire's point of origin in the Arapaho National Forest, the fire burned 193,812 acres (78,433 ha) between its ignition on October 14, 2020, and its containment on November 30.
The Marshall Fire was a destructive wildfire and urban conflagration that started on December 30, 2021, shortly after 11:00 a.m. MST, [3] as a grass fire in Boulder County, Colorado. [4] The fire caused the evacuation of 37,500 people, killed two people, and destroyed more than 991 structures to become the most destructive fire in Colorado ...
For premium support please call: 800-290-4726 more ways to reach us
It was the most severe extinction event of the past 500 million years, wiping out 80% to 90% of species on land and in the sea. Mystery deepens over cause of Earth's worst mass extinction event ...
The eruptions continued for roughly two million years and spanned the Permian–Triassic boundary, or P–T boundary, which occurred around 251.9 million years ago. The Siberian Traps are believed to be the primary cause of the Permian–Triassic extinction event, the most severe extinction event in the geologic record.
The investigation into the cause of the most destructive wildfire in Colorado history, which forced tens of thousands of people to flee their homes ahead of the new year, remains ongoing as a new ...
Permian: Permian–Triassic extinction event: 252 Ma Large igneous province (LIP) eruptions [23] from the Siberian Traps, [24] an impact event (the Wilkes Land Crater), [25] an Anoxic event, [26] an Ice age, [27] or other possible causes End-Capitanian extinction event: 260 Ma: Volcanism from the Emeishan Traps, [28] resulting in global cooling ...