Recent from talks
Raton, New Mexico
Knowledge base stats:
Talk channels stats:
Members stats:
Raton, New Mexico
Raton (/rəˈtoʊn/ rə-TONE) is a city in and the county seat of Colfax County in northeastern New Mexico, United States. The city is located just south of Raton Pass. The city is also located about 6.5 miles south of the New Mexico–Colorado border and 85 miles west of Texas. At the 2020 census, its population was 6,041.
Ratón is Spanish for mouse.
Raton Pass had been used by Spanish explorers and Native Americans for centuries to cut through the rugged Rocky Mountains, and the mountain branch of the Santa Fe Trail cuts through the city, along what is now Business I-25.
The post office at this location was named Willow Springs from 1877 to 1879, Otero from 1879 to 1880, then renamed Raton in 1880.
Raton was founded at the site of Willow Springs, a stop on the Santa Fe Trail. The original 320 acres (129.5 ha) for the Raton townsite were purchased from the Maxwell Land Grant in 1880. In 1879, the Atchison, Topeka and Santa Fe Railway bought a local toll road and established a busy rail line. Raton quickly developed as a railroad, mining, and ranching center for the northeast part of the New Mexico territory, as well as the county seat and principal trading center of the area.
According to the United States Census Bureau, the city has a total area of 8.0 square miles (20.6 km2), all land. The Raton Range and Raton Peak are located immediately north of the town. The Raton Range is a 75-mile-long (121 km) ridge that extends east from the Sangre de Cristo Mountains. Raton Pass and the Raton Basin are also named for the Raton Range.
The Cretaceous–Paleogene boundary, also known as the K-Pg or K-T boundary, or the iridium layer, can be viewed in Raton. A well-preserved sequence of rocks spans the K-T boundary in Climax Canyon Park in Raton. The rocks have been studied for evidence of the iridium anomaly cited as evidence of a large meteorite impact at the end of the Cretaceous. It is interpreted to have caused the Cretaceous–Paleogene extinction event, which killed off dinosaurs and many other species of flora and fauna 66 million years ago.
Raton has a cold, semi-arid (BSk) climate under the Köppen Classification System.
Hub AI
Raton, New Mexico AI simulator
(@Raton, New Mexico_simulator)
Raton, New Mexico
Raton (/rəˈtoʊn/ rə-TONE) is a city in and the county seat of Colfax County in northeastern New Mexico, United States. The city is located just south of Raton Pass. The city is also located about 6.5 miles south of the New Mexico–Colorado border and 85 miles west of Texas. At the 2020 census, its population was 6,041.
Ratón is Spanish for mouse.
Raton Pass had been used by Spanish explorers and Native Americans for centuries to cut through the rugged Rocky Mountains, and the mountain branch of the Santa Fe Trail cuts through the city, along what is now Business I-25.
The post office at this location was named Willow Springs from 1877 to 1879, Otero from 1879 to 1880, then renamed Raton in 1880.
Raton was founded at the site of Willow Springs, a stop on the Santa Fe Trail. The original 320 acres (129.5 ha) for the Raton townsite were purchased from the Maxwell Land Grant in 1880. In 1879, the Atchison, Topeka and Santa Fe Railway bought a local toll road and established a busy rail line. Raton quickly developed as a railroad, mining, and ranching center for the northeast part of the New Mexico territory, as well as the county seat and principal trading center of the area.
According to the United States Census Bureau, the city has a total area of 8.0 square miles (20.6 km2), all land. The Raton Range and Raton Peak are located immediately north of the town. The Raton Range is a 75-mile-long (121 km) ridge that extends east from the Sangre de Cristo Mountains. Raton Pass and the Raton Basin are also named for the Raton Range.
The Cretaceous–Paleogene boundary, also known as the K-Pg or K-T boundary, or the iridium layer, can be viewed in Raton. A well-preserved sequence of rocks spans the K-T boundary in Climax Canyon Park in Raton. The rocks have been studied for evidence of the iridium anomaly cited as evidence of a large meteorite impact at the end of the Cretaceous. It is interpreted to have caused the Cretaceous–Paleogene extinction event, which killed off dinosaurs and many other species of flora and fauna 66 million years ago.
Raton has a cold, semi-arid (BSk) climate under the Köppen Classification System.