|Lat/Lon:||37.17470°N / 109.9269°W|
|Season:||Spring, Summer, Fall, Winter|
|Elevation:||5160 ft / 1573 m|
Goosenecks State Park is one of the least developed properties in the Utah State Park system. It is located in southeastern Utah.
The Park has just one extended viewpoint of several huge river bends, flowing in a deep canyon with a series of stepped cliffs and terraces. Beyond the visible meanders, the river continues to twist and turn as the canyon deepens, before joining Lake Powel after about 35 miles.
Visitors can park just a few feet away from the cliff edge and gaze down onto the river far below. Until the moment you step out of the car you really can’t see anything but then suddenly the ground just opens up and you get the most magnificient views of the canyons below! It is one of the places I keep coming back to - a geological wonder.
Goosenecks State Park offers spectacular views of winding San Juan River 1,000 feet below. Over a distance of one and half miles, the San Juan river flows for more than 6 miles through the twists of the entrenched meander. The goosenecks are series of tight loops made by the river. (The photo above is hard to catch - expect to get only one of the twists into a regular camera).
The park offers great picnic areas, primitive free camping, incredible views and expansive star gazing. There is no river access in the park, but there is an unmarked trail leading down to the river - Honaker trail a couple of miles west from the park.
You can also drive east (left) along the cliff on an initially good dirt road for about 1 mile, after that the road becomes rough (high clearance vehicle needed), and after about 1/2 miles you reach the end of the rock peninsula and have views of the river below. This area provides more solitude and you can camp here. There are several points you can scramble part down, but no established trails, and cliffs prevent you from reaching the river.
Area: 10 acres (4 ha)
Visitation: roughly 65,000 per year
Climate: Goosenecks State Park lies at an elevation of 5,100 feet. The climate is arid with less than 15 inches of precipitation per year. Summer days are usually hot with temperatures reaching 90 degrees F or more and night cool to 65 degrees F. Winter can be very cold and snowfall does occur. Expect daytime temperatures to reach 55 degrees F and nighttime temperatures to drop to below freezing.
How Were the Goosenecks formed?
The San Juan river originates in the San Juan Mountains of Colorado, and many millions of years ago flowed gently across a flat landscape, forming large meanders that frequently changed position. Uplift associated with creation of the Colorado Plateau caused the river gradually become entrenched, preserving its most recent course in the deep canyon seen today. The rocks forming the sides of the gorge are shale and limestone from the Paradox Formation and the Honaker Trail Formation, up to 300 million years old.
Geologists Love the Goosenecks - The Goosenecks of the San Juan river often appear in geology textbooks as a classic location for observing entrenched or incised meanders. The canyon walls reveal the 300 million year old rocks. Near the Goosenecks Park is the Honaker Trail, which leads down to the river. It was along this historic trail that early detailed studies were done on the Pennsylvanian period limestone, and is known as the Honaker Trail Formation, a rock layer laid down in the Pennsylvanian period. Under the Honaker Trail Formation lies the Paradox Formation. Geologists are interested in Paradox layer because rich amounts of oil have been found in this layer of rock in other areas.
Bluff. Drive west from Bluff on US 163 for 20 miles, then turn north on UT-261. Turn left at the sign for Goosenecks State Park UT-316. The access road is paved. The side roads and the access road to Honaker Trail are dirt roads.
The small town of Mexican Hat has a population of roughly 70 people, don't expect much in the term of services. Bluff is not that much bigger.
There is no public transportation. The closest large airports would be Salt Lake City, approximately 350 miles away.
Albuquerque, New Mexico is about 310 miles away, and Denver, Colorado 460 miles away. Flagstaff, Arizona is about 240 miles away.
There are no official/established trails at Goosenecks State Park and it is not easy to climb down to the river (I always got cliffed out). You encounter cryptobiotic soil on your explorations, so mind your step, and watch for rattlesnakes.Honaker Trail - this is a historic hiking trail located near Goosenecks State Park. It was built in the late 1890s as a supply route for gold prospectors. However, the route proved too rugged even for pack animals. Besides, the gold rush was short lived in this territory. The trail is a mixture of steep switchbacks and traverses along the cliffs. It is 2.5 miles (4.0 km) one way and connects the river with the canyon rim over 1,200 feet (370 meters) above. It is very popular with geologists, the trail serves as the type locality for the Pennsylvanian Honaker Trail Formation.
The Goosenecks offers picnic areas, primitive camping, vault toilets, and an observation shelter.
Camping: limit 14 days, no fees
Goosenecks State Park is very primitive. Camping is allowed, but there are no developed campsites. The area can be intensely hot during the summer (no shade, no trees), and very windy since there is no protection.
No drinking water available.It is popular with large RV, many are parked along the rim, and use the picnic tables.