McNary (Western Apache: Chaabitoʼ) is a census-designated place (CDP) in Apache and Navajo counties in the U.S. state of Arizona. The population was 528 at the 2010 census. It is a 30-minute drive from Show Low and a 10-minute drive from Pinetop-Lakeside.
The Mountains are Calling and You Must Go!
Show Low, Arizona
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Weekends are for the Warriors
Show Low, Arizona
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Mighway, by TH2, allows you to rent your vehicle to discerning travellers when you’re not on the road, earning money and sharing the experience. At Mighway, you choose your level of service and we take good care of the rest. That means comprehensive insurance coverage, customer vetting, security deposits, payment processing and round the clock customer support for renters. It’s a bit like renting out a vacation home, with Mighway beside you all the way.LEARN MORE
If you’re in search of an incredible natural vista, then Horseshoe Bend is definitely worth a visit. The name was inspired by its unusual shape, a horseshoe-shaped meander of the Colorado River located four miles southwest of Page, AZ, within the Glen Canyon National Recreation Area. Just a hop, skip, and a jump from Glen Canyon Dam and the popular Lake Powell, the best view is from the steep cliff above Horseshoe Bend.
This great Navajo Nation valley boasts sandstone masterpieces that tower at heights of 400 to 1,000 feet. framed by scenic clouds casting shadows that graciously roam the desert floor. The angle of the sun accents these graceful formations, providing scenery that is simply spellbinding. "It’s about 16 miles from Bluff to the eastern entrance, on the right, of Valley of the Gods, a highly recommended side trip. Valley of the Gods is like a miniature version of Monument Valley without people. Its mesas and spires are formed of the same Cedar Mesa sandstone as the somewhat larger formations at Monument Valley. The 17-mile loop drive on (mostly good) dirt road is suitable for all but the most low-slung passenger vehicles in good weather. Definitely consider driving this beautiful, lonely loop—though not in a large RV and not dragging a trailer. Stay away after heavy rains. Valley of the Gods is also a very good place to camp if you are entirely self-sufficient. There are no established campgrounds and no facilities, but there are plenty of places to camp in the wild. It is incredibly quiet, and watching the moon rise here is a once-in-a-lifetime experience. The loop finishes on Highway 261 (paved) just south of the descent from the Moki Dugway and north of the turnoff for Goosenecks State Park. Highway 261 will take you south back to U.S. 163, but there are some things to see along Highway 261 so consider taking more side trips. To see the impressive Muley Point overlook’s expansive views, turn right on Highway 261 off the Valley of the Gods scenic drive and immediately climb the 1,000-foot graded gravel road up the Moki Dugway. (If you haven’t taken the Valley of the Gods option, turn right off U.S. 163 and head north on Highway 261 for about 9 miles to get here.) Just at the crest and right before the pavement resumes, look for the turnoff to the left. Trailers and large RVs will find the long climb to Muley Point nerve-racking, but the steep switchbacks and unbeatable scenery make this one of the most thrilling drives in the state." The area is part of the Colorado Plateau. The elevation of the valley floor ranges from 5,000 to 6,000 feet above sea level. The floor is largely siltstone of the Culter Group, or sand derived from it, deposited by the meandering rivers that carved the valley. The valley's vivid red color comes from iron oxide exposed in the weathered siltstone. The darker, blue-gray rocks in the valley get their color from magnesium oxide. The buttes are clearly stratified, with three principal layers. The lowest layer is the Organ Rock Shel, the middle is de Chelly Sandstone, and the top layer is the Moenkopi Formation capped by Shinarump Conglomerate. The valley includes large stone structures including the famed Eye of the Sun.Between 1948 and 1967, the southern extent of the Monument Upwarp was mined for uranium, which occurs in scattered areas of the Shinarump Conglomerate; vanadium and copper are associated with uranium in some deposit The landscape overwhelms, not just by its beauty but also by its size. The fragile pinnacles of rock are surrounded by miles of mesas and buttes, shrubs, trees and windblown sand, all comprising the magnificent colors of the valley. All of this harmoniously combines to make Monument Valley a truly wondrous experience. Enjoy this beautiful land. - Read More at Visit Utah https://www.visitutah.com/places-to-go/most-visited-parks/monument-valley-tribal-park/scenic-drives Monument valley has been used as a filming location for dozens of films and TV shows, from 2001: A Space Odyssey and Transformers: Age of Extinction to the Lone Ranger and Stagecoach, plus more.
Visit the world’s best preserved meteorite impact site just minutes from Interstate 40 in Northern Arizona near Winslow. Meteor Crater is the breath-taking result of a collision between a piece of an asteroid traveling at 26,000 miles per hour and planet Earth approximately 50,000 years ago. Today, Meteor Crater is nearly one mile across, 2.4 miles in circumference and more than 550 feet deep. It is an international tourist venue with outdoor observation trails, air conditioned indoor viewing, wide screen movie theater, interactive discovery center, unique gift and rock shop, and Astronaut Memorial Park at the modern Visitor Center located on the crater rim. Meteor Crater's "IMPACT The Mystery of Meteor Crater" movie, featuring exciting 3D modeling and animation allows viewers to experience the thunderous sound and explosive fury of the meteor's super-heated trip through the Earth's atmosphere. Then, the spectacular result of the collision that rocked the American Southwest with the energy of more than 20 million tons of TNT can be explored first-hand just outside the Visitor Center at Meteor Crater Arizona.
A powerful and inspiring landscape, Grand Canyon overwhelms our senses through its immense size. On December 1, the canyons filled with clouds, providing a rare sight seen by very few in a rare occurrence known as inversion: warm air on the upper parts of the cannon trap cold air and fog on the lower parts. Unique combinations of geologic color and erosional forms decorate a canyon that is 277 river miles (446km) long, up to 18 miles (29km) wide, and a mile (1.6km) deep. Grand Canyon National Park, a World Heritage Site, encompasses 1,218,375 acres and lies on the Colorado Plateau in northwestern Arizona. The land is semi-arid and consists of raised plateaus and structural basins typical of the southwestern United States. Drainage systems have cut deeply through the rock, forming numerous steep-walled canyons. Forests are found at higher elevations while the lower elevations are comprised of a series of desert basins. Well known for its geologic significance, the Grand Canyon is one of the most studied geologic landscapes in the world. It offers an excellent record of three of the four eras of geological time, a rich and diverse fossil record, a vast array of geologic features and rock types, and numerous caves containing extensive and significant geological, paleontological, archeological and biological resources. It is considered one of the finest examples of arid-land erosion in the world. The Canyon, incised by the Colorado River, is immense, averaging 4,000 feet deep for its entire 277 miles. It is 6,000 feet deep at its deepest point and 18 miles at its widest. However, the significance of Grand Canyon is not limited to its geology. The Park contains several major ecosystems. Its great biological diversity can be attributed to the presence of five of the seven life zones and three of the four desert types in North America. The five life zones represented are the Lower Sonoran, Upper Sonoran, Transition, Canadian, and Hudsonian. This is equivalent to traveling from Mexico to Canada. The Park also serves as an ecological refuge, with relatively undisturbed remnants of dwindling ecosystems (such as boreal forest and desert riparian communities). It is home to numerous rare, endemic (found only at Grand Canyon), and specially protected (threatened or endangered) plant and animal species.
Havasu Falls is known throughout the world and has appeared in numerous magazines and television shows, and is often included in calendars that feature incredible waterfalls or beautiful scenery. Visitors from all over the world make the trip to Havasupai primarily for Havasu Falls. The vibrant blue water contrasts against the striking red rocks of the canyon walls as Havasu Falls plunges nearly 100 feet into a wide pool of blue-green waters. This, the most striking waterfall in the Grand Canyon, sports a wide sandy beach and plenty of shady cottonwood trees to relax by. Calcium carbonate and magnesium occur naturally in the waters of Havasu Creek. The pools and natural dams form when the calcium carbonate precipitates out of the water and deposits onto rocks, branches, or man made structures (after a devastating flood) building up over time. Havasu Falls and Havasu Creek get their blue color from the magnesium in the water. As the pools deepen and the calcium carbonate is slowly released from the water, the bluer the water appears as the relative magnesium content increases. Havasu Falls is just a quarter mile from Lower Navajo Falls and about a quarter of a mile before you reach the campground. Easily accessible from several paths leading down to the refreshing waters, of course you must take a swim. Below the major pool, you can explore smaller pools as the stream cascades and winds its way towards the campground. When planning a trip to Havasu Falls, please add the Havasu Trailhead to your trip instead of Havasu Falls. The trailhead must be used to access the falls at the bottom of the canyon, and Havasu Falls cannot be routed properly due to its location far from a road.Visit Havasu Falls
Want to get up close and personal to a dinosaur? At Bedrock City, halfway between the Grand Canyon and Williams, you have the opportunity to do just that. Here you will see Fred and Barney, Wilma and Betty along with Pebbles and Bamm Bamm from the Flintstones cartoons as well as the giant dinosaur that you can slide down the tail, like a slide, just like Fred on the intro to the cartoon. This unique stop is located between the Grand Canyon and Williams on Arizona Hwy 54 at the junction of US 180 in Valle. Created to look like Fred, Barney, Wilma, Betty, Pebbles and Bamm Bamm from the Flintstones cartoons they will bring a smile to your face, regardless of whether you are still a kid or just remembering how the Flintstones made you laugh. The statues are stationary, they are huge and they are fun.Visit Bedrock City
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