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Elden Pueblo (Hopi: Pasiwvi) was a prehistoric Native American village at the foot of Mount Elden near Flagstaff, Arizona. The pueblo is considered part of a major trading system. [1] Various trade items, such as macaw skeletons from Mexico and shell jewelry from the coast of California, have been found throughout the site. The area is now ...
The entrance to the cave is around 14 miles (23 km) west of Flagstaff, Arizona. Being in Coconino National Forest, the cave is managed by the United States Forest Service. While the cave is open year-round, the dirt roads which lead there may be impassable to cars in winter months or during wet weather conditions.
The Arizona Lumber and Timber Company Office – built in 1900 and is located on 1 Riordan Road. The Bank Hotel, originally called "The Arizona Central Bank and Hotel" – built in 1887 and located on Route 66 and Leroux Street. The Weatherford Hotel – built in 1887 by John W. Weatherford. The hotel is located at 23 N. Leroux Street.
Location of Coconino County in Arizona. This is a list of the National Register of Historic Places listings in Coconino County, Arizona. It is intended to be a complete list of the properties and districts on the National Register of Historic Places in Coconino County, Arizona, United States. The locations of National Register properties and ...
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Pinedale, Arizona: Ruins of a multistoried pueblo of 200–250 rooms, AD 1275–1325 (late Pueblo III Era and/or early Pueblo IV Era). Betatakin: Ancestral Pueblo Kayenta: Navajo Reservation: Grand house Ruins located at the Navajo National Monument. Box Canyon Ruins: Flagstaff Ruins located in the Wupatki National Monument. Canyon Creek Ruins ...
This is a partial list of ghost towns in Arizona in the United States. Most ghost towns in Arizona are former mining boomtowns that were abandoned when the mines closed. Those not set up as mining camps often became mills or supply points supporting nearby mining operations. [1]
They are found in two forms. Some are hollow cylindrically shaped soda straws, formed by escaping gases. The others are cone shaped drip pendants formed when re-melted lava dripped from the ceiling. At the end of Low Bridge area, the tube begins to narrow and the cave is divided into two tunnels with intermittent connecting passages.