Goodyear
Arizona, United States β 99 km
πΊπΈ Utah Β· United States β Altitude 1586 m
This live stream looks out over the Oljato area of Monument Valley, on the Navajo lands straddling the Utah and Arizona border. It is a good way to check the sky and light over one of the American Southwest's most photographed landscapes before planning a trip or simply enjoying the view.
Monument Valley is known for its sandstone buttes and mesas rising abruptly from the desert floor, shaped over millions of years by erosion. Oljato sits on the Navajo Nation and is closely tied to the tribe's history and daily life. The landscape is open and dry, with wide horizons, and the red and orange rock changes colour noticeably as the sun moves across the sky.
Since the camera is a live stream from a fixed position, the most interesting moments tend to be near sunrise and sunset, when low light sharpens the rock formations. Cloud shadows moving across the valley and seasonal changes in haze and snow are also worth watching. Conditions depend on the view and weather at the time of your visit.
The region has a high desert climate with hot summers, cold winters and little rain, so spring and autumn are the most comfortable times to visit. Monument Valley is roughly a few hours' drive from the other cameras in this area, including Goodyear, Moab and the Grand Canyon Village. Check the live weather on this page before setting out.
Source: Utah State University
Arizona, United States β 99 km
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The current conditions and a 3-day forecast are shown in the live weather block on this page, updated automatically for the location.
The local time for this camera is displayed on the page, so you can see whether it is day or night there before you watch.
The camera is in the Oljato area of Monument Valley, in the Navajo Nation near the Utah and Arizona border. The map on this page shows its exact position.
Early morning and late afternoon usually give the richest colours on the rock formations, though the best moment depends on the weather and the season.
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