Category: Geology

Goblin Valley Utah

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A Goblin formed from a soft limestone, water and time offer a unique hiking experience. Photograph by James L Rathbun

Goblin Valley is located in Utah is a state park and campground which is adjacent to eroded flood plain. Formed by water, time and a soft sandstone, erosion sculpted the limestone into unique rock formations which some have stated appears to be goblins.  The Goblin Valley itself is a day use hiking area which allows one to get lost in the maze of spires and rock formations.

Valley Queen, Goblin Valley, Utah Photography by James L Rathbun
Valley Queen, Goblin Valley Utah. Photograph by James L Rathbun

Each rock spire ranges in height from 3 feet to about 20 feet tall.  The fragile structures litter the landscape and sadly on occasion have been felled by people who do not have respect for nature.  There are three established self, however the Valley of the Goblins is a open trail flat mud plane after a easy and short trail down from the parking area.

Goblin Valley State Park does offer an established campground of 22 campsites just over a hill from the Valley of the Goblins.  The campground features, paved sites, bathrooms, showers, water and dump stations. The campground is very popular destination due to location next to Goblin Valley and is also a wonderful centralized base camp location for exploring the San Rafael Swell.

A solitary Pronghorn ( Antilocapra americana ) found near Golbin Valley, Utah
A solitary Pronghorn ( Antilocapra americana ) found near Golbin Valley, Utah

We stated in Goblin Valley in the off season several years ago. We were greeted with lots of camp sites available, privacy and a minor wind and rain storm. Despite the less then desirable conditions, we enjoyed our stay and will try to make it back again in the future.

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Racetrack Valley

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TeaKettle Junction lets you know you are starting to get close to the Racetrack.
TeaKettle Junction lets you know you are starting to get close to the Racetrack.

Racetrack valley is a rough graded road which departs the Ubehebe Crater site and heads south into the desert. The road is rough, but easily passable in a regular car. However, when entering back country areas such as this it is always a good idea to have the insurance of a reliable vehicle, high clearance, four wheel drive, etc…  Do yourself a huge favor and air down your tires if you are properly equipped to air up when the trip is over.

Looking north from the Lippincott Mine towards the Racetrack off in the distance.
Looking north from the Lippincott Mine towards the Racetrack off in the distance.

The racetrack valley road is a 25 miles one way trip to the playa. The road is grated, but can be heavily wash-boarded depending on the time of year, rain fall, etc…

Along the way, there are many side trips and alternate trails to help expand your visit.

As you leave Ubehebe Crater, you will be driving south and gradually gaining elevation. Take your time and enjoy the drive, if you are lucky you may see a big horn sheep herd. The road gradually gains in elevation and climbs through a Joshua Tree Forest.

Once you reach the pass, the road continues to drop in elevation all the way down to the playa. Continue straight through tea kettle junction, and bear left down the valley past the side road to the Lippincott mine, which is a great side trail.

The Racetrack Playa of Death Valley.
The Racetrack Playa of Death Valley.

As you continue past the road to the Lippincott mine the road drops down to the Racetrack Playa itself. The first stop is ‘The Grandstand’ which is an outcropping of rock located in the north west corner of the racetrack. The second stop is the parking area to hike towards the stones. Don’t try to hike to the stones from the first Grandstand parking lot, or you will be hiking significantly further.

The highlight of the trip, is a short hike to the sailing or racing stones. The start of the hike is the parking area at the southern end of the racetrack playa.

Jeeps and Labradors are not allowed on the playa!

To reach the stones hike east from the parking lot across the playa towards the dark stone hillside. It is short FLAT, meaning really FLAT hike towards the stones. Be sure the check the temperatures before you leave, and bring lots of water. This is true with anything you might want to do in Death Valley. Don’t walk on the playa if it is wet or muddy.

The Racing stones.
The Racing stones.

At the end of the 30 miles road there is a small primitive campground for overnight visits. Be sure to check with the National Park Service for regulations of back country camping within the park.

Every racetrack needs a grandstand.
Every racetrack needs a grandstand.

Notoriety

On September 19th, 1969 a Michigan front end loading is found burning along the road near the playa. Apparently, Manson order the machine burned. Park Rangers were deployed to the Racetrack. The rangers followed a set of tire tracked which belonged to a Toyota Land Cruiser which was stolen by Manson. The follow up investigate lead to the arrest of Charles Manson at Barker Ranch on October 12th, 1969.

Racetrack Valley Trail Map

References

Devil’s Gate – Nevada State Historic Marker 223

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Devil’s Gate, located in Lyon County, Nevada, is a striking natural landmark renowned for its rugged and otherworldly beauty. The geologic landmark is recognized as Nevada State Historic Marker number 223. Devil’s Gate is an impressive rock formation located along Nevada State Route 342 outside of Silver City, Nevada. The gate to Gold Canyon was carved by the forces of nature over thousands of years.

Devil's Gate near Silver City. This was a toll road on the way to Virginia City.
Devil’s Gate near Silver City. This was a toll road on the way to Virginia City.

Nevada State Historic Marker 223

Nevada State Historical Markers identify significant places of interest in Nevada’s history. The Nevada State Legislature started the program in 1967 to bring the state’s heritage to the public’s attention with on-site markers. These roadside markers bring attention to the places, people, and events that make up Nevada’s heritage. They are as diverse as the counties they are located within and range from the typical mining boom and bust town to the largest and most accessible petroglyph sites in Northern Nevada Budget cuts to the program caused the program to become dormant in 2009. Many of the markers are lost or damaged.

It gives … “a forcible impression of the unhallowed character of the place.” J. Ross Browne . 1860

This rugged reef of metamorphic rock was once one of the famous landmarks of the Nevada Territory.  In June of 1850, John Orr and Nicholas Kelly unearthed a gold nugget nearby, the first ever found in Gold Canyon.  For the next ten years, the can was the scene of placer mining and one of the first stamp mills in the Territory was erected just to the south of Devil’s Gate during the summer of 1860.

During the brief Paiute War of May, 1860, the people of Silver City built a stone battlement atop the eastern summit and constructed a wooden cannon for protection.

Devil’s Gate marks the boundary line between Storey and Lyon Counties.  Through this narrow gorge paraded thousands of the most adventurous souls of the mining West as they made their way to the gold and silver mines of the Comstock Lode.

STATE HISTORICAL MARKER No. 223

DIVISION OFHISTORIC PRESERVATION AND ARCHAEOLOGY

SPONSORED BY:

RENO CHAPTER OF THE NATIONAL SOCIETY

DAUGHTERS OF THE AMERICAN COLONISTS

Devil’s Gate Historic Marker Map

Nevada State Historic Marker number two hundred twenty three is location on the western side of Nevada State Route near the geologic feature. The marker is just north of Silver City, Nevada.

Devil's Gate as seen from the townsite of Silver City. State Route 342 goes through the "gate" on its way to Virginia City. Original view is circa 1866
Devil’s Gate as seen from the townsite of Silver City. State Route 342 goes through the “gate” on its way to Virginia City. Original view is circa 1866

Nevada State Historic Marker Summary

NameDevil’s Gate
LocationLyon County, Nevada
Latitude, Longitude39.2667, -119.6419
GNIS222304
Nevada State Historic Marker 223

References

Subway Canyon – Left Fork of North Creek

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Subway Slot Canyon is a unique geological formation located in the Zion National Park in southwestern Utah, USA. It is considered one of the most popular hiking trails in the park, known for its challenging terrain and breathtaking views. The canyon gets its name from its tubular shape, which resembles the underground trains or subway tunnels.

The Subway Slot Canyon located in Zion National Park, Utah. Photograph by James L Rathbun
The Subway Slot Canyon located in Zion National Park, Utah. Photograph by James L Rathbun

History

The Subway Slot Canyon was formed millions of years ago by the erosion of Navajo Sandstone, a red-colored rock formation that is found in the southwestern United States. The slot canyon was created by the flow of water, which gradually wore away the sandstone, forming a narrow, winding passage through the rock. The canyon was first discovered by explorers in the 1930s, but it was not until the 1970s that it became a popular destination for hikers.

Geology

The Subway Slot Canyon is a part of the Zion Wilderness, which covers an area of approximately 124,406 acres. The canyon is about 9 miles long and ranges in width from 5 to 15 feet. The canyon walls are made up of Navajo Sandstone, which is known for its unique patterns and colors. The sandstone is layered, with different colors and textures, giving the canyon walls a unique and stunning appearance. The canyon also features a series of pools and waterfalls, which add to its beauty.

Flora and Fauna

The Subway Slot Canyon is home to a variety of flora and fauna. The area around the canyon is covered with sagebrush, juniper, and pinyon trees. The canyon itself is home to a variety of ferns, mosses, and other plant species. The canyon is also home to a variety of animals, including bighorn sheep, mule deer, and mountain lions. Hikers may also see a variety of birds, including hawks, eagles, and owls.

Hiking Experience

The Subway Slot Canyon is considered one of the most challenging hiking trails in the Zion National Park. The trail is rated as moderate to strenuous and requires a permit to hike. Hikers must be prepared for a difficult and sometimes dangerous hike, as the trail includes steep drops, narrow passageways, and deep pools of water. Hikers must also be prepared for changing weather conditions, as the canyon can be very hot in the summer and very cold in the winter.

The Subway Slot Canyon is a unique geological formation that offers hikers a challenging and rewarding experience. The canyon’s unique colors, textures, and shapes make it a must-see destination for anyone visiting the Zion National Park. However, hikers must be prepared for the challenges that come with hiking in the canyon, including difficult terrain and changing weather conditions. With proper preparation and precautions, hikers can safely explore the beauty of the Subway Slot Canyon and experience one of the most stunning geological formations in the world.

Temple of Sinawava

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Located in Zion National Park in southwestern Utah, the Temple of Sinawava is a stunning geological formation that attracts visitors from all around the world. This natural temple is the result of millions of years of geological processes, and it has been a sacred site for the indigenous people of the area for centuries. In this travel and geological report, we will explore the history, geology, and attractions of the Temple of Sinawava, as well as provide practical information for visitors.

Temple of Sinawava, Zion National Park, Utah, Medium Format Photograph: James L Rathbun
Temple of Sinawava, Zion National Park, Utah, Medium Format Photograph: James L Rathbun

History

The Temple of Sinawava is named after the Paiute Indian god, Sinawava, who is believed to have lived in the area. For centuries, the Paiute and other indigenous peoples have considered the area to be sacred, and they have performed various rituals and ceremonies there. The Paiute called the area “Mukuntuweap,” which means “straight canyon,” and it was later renamed Zion National Park by the Mormons who settled in the area.

Geology

The Temple of Sinawava is located at the end of the Zion Canyon Scenic Drive, and it is one of the most popular destinations in the park. The temple is a natural amphitheater that was formed by the Virgin River, which has been carving through the sandstone for millions of years. The river has eroded the sandstone in such a way that it has created a stunning array of geological features, including towering cliffs, deep canyons, and narrow slot canyons.

The Temple of Sinawava is a particularly unique geological formation because it is located at the end of Zion Canyon, where the canyon narrows dramatically. The canyon walls rise up to over 2,000 feet in height, and they are composed of various layers of sandstone that were deposited over millions of years. The layers of sandstone are different colors, ranging from red to white, and they provide a stunning contrast against the blue sky.

Attractions

The Temple of Sinawava offers visitors a variety of attractions, including hiking, wildlife viewing, and photography. The most popular activity at the temple is hiking the Riverside Walk, which is a 2.2-mile round-trip hike that follows the Virgin River to the entrance of the temple. Along the way, hikers will be treated to stunning views of the canyon walls, as well as a variety of wildlife, including bighorn sheep, mule deer, and numerous bird species.

Once visitors reach the entrance of the temple, they can continue hiking up the river, which leads to the beginning of the Narrows. The Narrows is a narrow slot canyon that is formed by the Virgin River, and it is one of the most popular hikes in Zion National Park. The Narrows can be hiked in two ways, either by hiking up the river or by hiking down the river. Hiking up the river requires a permit and special equipment, while hiking down the river is open to all visitors.

Another popular attraction at the Temple of Sinawava is photography. The temple is a popular destination for photographers, both amateur and professional, who come to capture the stunning beauty of the canyon walls and the river. The best time to photograph the temple is during the early morning or late afternoon, when the sun is low in the sky and the light is soft and warm.

Practical Information

The Temple of Sinawava is located in Zion National Park, which is open year-round. The park is located in southwestern Utah, and it can be accessed via State Route 9, which runs through the park. There are a variety of lodging options in the park, including campgrounds, lodges, and hotels, as well as numerous restaurants and gift shops.

Visitors to the Temple of Sinawava should come prepared with appropriate clothing and gear, as the weather can be unpredictable.