Mesa Verde National Park in February

Mesa Verde National Park has the largest ancient cliff dwelling ruins in the Southwest, most notably Cliff Palace, though there are many other impressive ones as well.

Cortez, Colorado and snowy cliffs of Mesa Verde.

Cortez, Colorado along the east end of Main Street, with the snowy cliffs of Mesa Verde.

The park is located in southwest Colorado, about ten miles east of  Cortez, or about 35 miles west of Durango, the two largest towns in the area.

Cortez, Colorado at dusk in winter.

Cortez, Colorado at dusk.

Cortez makes for a nice “base camp” if you’re staying in a motel while you explore the area. In fact, the cliffs that form the North Rim of Mesa Verde also provide a dramatic backdrop to the town. If you’re camping in winter, you’re limited to what few commercial campgrounds are open.

Although the splendid Visitor Center and Research Center is just off of Highway 160, to get all the way to the south end of the park on Chapin Mesa, where the park headquarters, the museum, and the main cliff dwelling ruins are located, is 21 miles, a drive of 45 minutes.  Thus even a quick look at the highlights of the park takes at least a couple hours. And that’s just from the side of the road. In winter, the Wetherill Mesa road is closed, as is the Far View Lodge, and the campground. Also, there are no ranger-led hikes to the main cliff dwellings.

Mancos Valley and La Plata Mountains, from Mesa Verde.

The Mancos Valley and the La Plata Mountains, from Mesa Verde.

After passing the entrance station, some sharp switchbacks take you up onto Mesa Verde’s north end. The first pull-out is the Mancos Valley Overlook. Here you can view not only the valley, with Highway 160 following it east toward Durango, but the high peaks of the distant La Plata mountain range to the northeast.

North Rim of Mesa Verde.

Cortez, Colorado along the east end of Main Street, with the snowy cliffs of Mesa Verde.

The next stop is to look the other direction: northwest, at the Montezuma Valley Overlook. Montezuma Valley is where Cortez is located, and being on the North Rim of Mesa Verde you can also look all the way to the Abajo Mountains across the state line at Monticello, Utah.

City of Cortez, Colorado, and Abajo Mountains in Utah.

Telephoto shot of the Abajo Mountains in Utah, looking across Cortez and the Montezuma Valley in Colorado.

“Mesa Verde” means “green table” in Spanish. But it’s not like a typical mesa, which is typically quite flat. Mesa Verde is more like a table with two of the legs cut short, making it tilt to the south, toward the sunlight. That makes for more frost free days than you would otherwise experience if you were living up there at 8,000-8,500 feet in elevation. Meaning the Ancestral Puebloan people that grew their crops in the fertile soil got enough precipitation (usually) from being up that high, but warm enough for corn to mature before the first frosts of autumn.

Mesa Verde canyons and ridges, in winter.

Some of the canyons and ridges that form the interior of Mesa Verde.

So overall Mesa Verde, the landform, is more like several smaller mesas along with a lot of parallel canyons that drain from north to south.

Winter is a great time to take in the many variations in this complex of mesas and canyons. When there is snow on the ground, as soon as the latest storm has passed and the sun comes out again, the hillsides that are facing south start melting off almost right away. The slopes that are facing north, however, hold their snow much later, because in winter the sun is at too low of an angle to touch them. And the ground is too cold to melt snow that’s in the shade. Until spring comes.

Different aspects of a slope show where the winter sun shines, or not.

Even slight changes in direction affect whether the winter sun can warm a slope, or not.

Finally, to the south end of the park where the famous cliff dwellings are located. The trail down to Spruce Tree House, near the Archeological Museum, was closed due to a recent rockfall. So it was on to the Mesa Top Loop drive.

Oak Tree House cliff dwelling ruin, Mesa Verde National Park, Colorado.

The ruins of Oak Tree House in its sheltering alcove in the canyon wall.

The Cliff Palace Loop is closed in winter, but you can get views of Cliff Palace from across Cliff Canyon on the Mesa Top Loop. From there, overlooks let you get scenic shots of the best ruins.

Fire House Ruin panorama, Mesa Verde National Park, Colorado.

The two-level alcoves of Fire House Ruin. Where was the elevator?

The cliff dwelling era was when the Ancestral Puebloans built their adobe, often multi story dwellings and other structures. There are 600 cliff dwellings in the park. Cliff dwellings were built in alcoves: natural recesses in the sandstone cliffs. Alcoves that face south were preferred. Why? Because in winter they get the most sunlight, while in summer, when the sun is at a much higher angle, the alcoves are in the shade of the overhanging cliff in the heat of the day. They also built pueblos and pit houses on the mesa tops. In fact, there are many more of those than their are cliff dwellings. But the overhanging alcoves provide a lot of protection from the weather to the cliff dwellings, so they are much better preserved over the approximately 750 years since the last of the ancient ones migrated on from here.

Cliff Palace cliff dwelling ruins, Mesa Verde National Park, Colorado.

Cliff Palace, from Camera Point at Sun View.

Photo location: Mesa Verde National Park, Colorado.

Copyright 2016 Stephen J. Krieg

One comment on “Mesa Verde National Park in February

  1. The cliff dwellers were certainly industrious people. Building a home high above where it’s cool, giving them adequate shelter and full view of their surroundings is what only the elite can afford today. Always enjoy your photography!


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