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TWA Flight 260

1955 in New MexicoAccidents and incidents involving the Martin 4-0-4Airliner accidents and incidents caused by instrument failureAirliner accidents and incidents in New MexicoAviation accidents and incidents in 1955
Aviation accidents and incidents in the United States in 1955Aviation accidents and incidents involving controlled flight into terrainFebruary 1955 events in the United StatesHistory of Bernalillo County, New MexicoTrans World Airlines accidents and incidents
MillsField 4martin (4395667839)
MillsField 4martin (4395667839)

TWA Flight 260 was the Trans World Airlines (TWA) designation for a flight from Albuquerque, New Mexico to Santa Fe, New Mexico. On February 19, 1955, the 40-passenger Martin 4-0-4 prop plane used by TWA for that route crashed into the Sandia Mountains. Its deviation from the normal flight path, initially believed to be the result of pilot error, was revised to "unknown" given that the contribution of other factors could not be definitively ruled out.

Excerpt from the Wikipedia article TWA Flight 260 (License: CC BY-SA 3.0, Authors, Images).

TWA Flight 260
Domingo Baca/TWA Route,

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Wikipedia: TWA Flight 260Continue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N 35.194 ° E -106.442 °
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Domingo Baca/TWA Route

Domingo Baca/TWA Route

New Mexico, United States
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MillsField 4martin (4395667839)
MillsField 4martin (4395667839)
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Sandia–Manzano Mountains
Sandia–Manzano Mountains

The Sandia–Manzano Mountains are a substantial mountain area that defines the eastern edge of the middle Rio Grande valley of central New Mexico. They are not only an attractive backdrop to greater Albuquerque, the largest metropolitan area in New Mexico, but their elevation changes provide recreational opportunities including winter skiing and cool summer hiking or picnicing, as compared to the desert grasslands, foothills, and Rio Grande Valley below. The entire mountain chain comprises three parts, arranged north to south: the Sandia Mountains, the Manzanita Mountains, and the Manzano Mountains. The Manzanita Mountains are a series of low-lying foothills that separate the Sandias from the Manzanos. The Sandia–Manzano Mountains are often considered to be the easternmost major range in the Basin and Range Province. A substantial distance gap of much lower elevation grasslands and savanna exists between the Sangre de Cristo Mountains and the Sandia Mountains, and climate conditions shift between both ranges. This distinction is further made by plant, animal, and insect species that are common in both the Sandia–Manzano Mountains and in other mountainous areas to the south, but diminish quickly in the mountains to the north. These include Quercus turbinella, Opuntia engelmannii, Aloysia wrightii, and the western diamondback rattlesnake. However, at higher elevations in the Sandia–Manzano Mountains, a strong climatically driven Rocky Mountain biotic element exists.