Search results
Results from the WOW.Com Content Network
The Chicxulub crater (IPA: [t͡ʃikʃuˈluɓ] ⓘ cheek-shoo-LOOB) is an impact crater buried underneath the Yucatán Peninsula in Mexico. Its center is offshore, but the crater is named after the onshore community of Chicxulub Pueblo (not the larger coastal town of Chicxulub Puerto ). [ 3 ]
Chicxulub Puerto (IPA: [tʃikʃuˈlub] ⓘ) is a small coastal town in Progreso Municipality in the Mexican state of Yucatán. It is located on the Gulf of Mexico , in the northwestern region of the state about 8 km (5 mi) east of the city port of Progreso , the municipality seat, and 42 km (26 mi) north of the city of Mérida , the state capital.
Chicxulub crater: 182 km (113 mi) 1.4% Cause or contributor of the Cretaceous–Paleogene extinction event: Sudbury Basin: 130 km (80 mi) 1% Moon (moon of Earth) Procellarum: 3,000 km (2,000 mi) 3,470 km 86% Not confirmed as an impact basin. South Pole–Aitken basin: 2,500 km (1,600 mi) 70% Imbrium: 1,145 km (711 mi) 33% Mars: North Polar Basin
Chicxulub Pueblo (Mayan pronunciation: [tʃʼikʃuluɓ] Ch’ik Xulub) is a town, and surrounding municipality of the same name, in the Mexican state of Yucatán. At the census of 2010, the town had a population of 4,080 people. The center of the Chicxulub Impact Crater (approx 21°20'N 89°30'W) is off the Yucatan coast, near Chicxulub Puerto
Main page; Contents; Current events; Random article; About Wikipedia; Contact us; Donate; Pages for logged out editors learn more
Chicxulub Pueblo Municipality is a municipality in the Mexican state of Yucatán containing (196.72 km 2) of land and located roughly 25 km north of the city of Mérida. [2] The area is directly onshore of the epicenter of the Chicxulub crater .
"The size and damage that would have been wrought by the Chicxulub impact is in agreement with the theory postulated by the late physicist Luis Alvarez and his son, geologist Walter Alvarez, for the extinction of the dinosaurs." I feel this sentence needs a re-write; the proposed damage caused by the impact cannot be in "agreement" with the ...
The top of the melt sheet, which is the, "crater floor" and base of the post-impact sedimentary fill, ranges from 1.2 to 1.6 km below sea level as confirmed by drilling (Gulick et al. 2013:44). Interpretation of geophysical data indicates that the sedimentary fill on top of the melt sheet is as deep as 1.9 km (Gulick et al. 2013:44).