Subway Canyon – Left Fork of North Creek

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

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.

Balanced Rock

Balanced Rock is an iconic natural feature located in Arches National Park, Utah, USA. This geological formation consists of a large boulder balanced precariously on top of a much smaller pedestal rock. The rock formation is an example of a natural geological process known as erosion and has become a popular destination for tourists from around the world. In this report, we will explore the geological history of Balanced Rock, its significance, and how it has become an important part of the natural landscape of Arches National Park.

Early Evening At Balanced Rock in Arches National Park, Medium Format Photograph bu James L Rathbun
Early Evening At Balanced Rock in Arches National Park, Medium Format Photograph bu James L Rathbun

Geological History

Balanced Rock is situated in an area known as the Entrada Sandstone Formation. This formation was created around 180 million years ago, during the Jurassic Period, when the region was a vast desert. Over time, layers of sediment accumulated on the desert floor, which eventually became compressed and turned into rock. The Entrada Sandstone Formation is composed of a soft, red sandstone, which is prone to erosion.

Erosion is a natural geological process that occurs when wind, water, and other natural forces wear away at the surface of the Earth. In the case of Balanced Rock, the pedestal rock is made of a harder, more erosion-resistant sandstone than the boulder on top. As the softer sandstone eroded away, the harder rock was left behind, forming a pedestal. Over time, the boulder on top was also eroded, creating the balanced formation that we see today.

Significance

Balanced Rock has become an iconic symbol of Arches National Park and a popular destination for tourists from around the world. The formation is an excellent example of the natural geological processes that shape our planet and provides a unique window into the history of the Earth.

Balanced Rock is also significant from a cultural perspective. For centuries, the land that is now Arches National Park was home to indigenous people, including the Ute and Paiute tribes. These tribes believed that the rock formations in the park held spiritual significance and would often conduct ceremonies and rituals in the area.

In addition to its cultural significance, Balanced Rock is also an important habitat for a variety of plants and animals. The area around the formation is home to a variety of desert plants, including cacti and sagebrush, as well as a variety of small mammals and birds.

Conservation Efforts

Arches National Park was established in 1971 to protect the unique geological and cultural features of the area, including Balanced Rock. The park is managed by the National Park Service and is dedicated to preserving the natural beauty of the region for future generations.

Conservation efforts in the park are focused on maintaining the delicate balance between human use and environmental preservation. Visitors to the park are encouraged to stay on designated trails and follow the “Leave No Trace” principles to minimize their impact on the natural environment.

In addition to visitor education, the National Park Service also conducts ongoing research to monitor the health of the park’s ecosystems. This research helps to identify potential threats to the park’s natural resources and develop strategies to mitigate those threats.

Conclusion

Balanced Rock is a natural wonder that has captured the imagination of people from around the world. This iconic formation is a testament to the power of natural geological processes and provides a unique window into the history of the Earth. Its cultural and ecological significance make it an important part of Arches National Park, and conservation efforts are underway to ensure that this unique feature remains protected for future generations to enjoy.

Christopher Houston Carson

Christopher Houston Carson (December 24, 1809 â€“ May 23, 1868), also known as “Kit” Carson, was a nineteenth century American Frontiersman, Army Officer and Politician and the namesake of Carson City, Nevada. During his lifetime, he achieved notoriety for his exploits as an Indian Fighter, Fur Tapper, Mountain man

Christopher 'Kit' Carson (1809-1868), American explorer - Photograph byMathew Brady or Levin C. Handy - This image is available from the United States Library of Congress's Prints and Photographs division under the digital ID cwpbh.00514.
Christopher ‘Kit’ Carson (1809-1868), American explorer – Photograph by Mathew Brady or Levin C. Handy – This image is available from the United States Library of Congress’s Prints and Photographs division.

Carson was born on December 24, 1809 in Madison County, Kentucky to Lindsey Carson and Rebecca Robinson Carson. He is a cousin to Danial Boone on his mothers’ side. The family moved to Missouri two years later. Survival being the priority, Carson never learned to read or write. At the age of 16, he signed up with a large caravan of merchants headed west towards Santa Fe.

Exploration

In 1854, a change encounter with the explorer John C. Frémont, made Carson an active participant in the clash of empires that eventually extended the boundaries of the continental United States to its present. The two men met aboard a steamboat on the Missouri River. He served as a guide to for Fremont on three expeditions for a sum of $100 per month. These expeditions found the Oregon Trail and opened to west for the settlers who followed.

First expedition, 1842

In 1842, during the first expedition, Carson guided Frémont across the Oregon Trail to South Pass, Wyoming. The purpose of this expedition was to map and describe the Oregon Trail as far as South Pass. It is during this trip, that the two men produced a guidebook, maps, and other paraphernalia would be printed for westward-bound migrants and settlers. After the completion of the five-month expedition, Frémont wrote his government reports, which made Carson’s name known across the United States, and spurred a migration of settlers westward to Oregon via the Oregon Trail.

Second expedition, 1843

In 1843, Carson agreed to join Frémont’s again during his second expedition into the west. Carson guided Frémont across part of the Oregon Trail to the Columbia River in Oregon. The purpose of the expedition was to map and describe the Oregon Trail from South Pass, Wyoming, to the Columbia River. They also ventrured towards the Great Salt Lake in Utah, using a rubber raft to navigate the waters.

On the way to California, the party is held up during bad weather in the Sierra Nevada Mountains. Fortunately, Carson’s good judgement and his skills as a guide and they found some American settlers who fed them. The expedition turned towards California. This ventures is illegal, at the time, and dangerous because California was Mexican territory.

During the expedition, the expedition arrive in the Mojave Desert. His party met a Mexican man and boy, who informed Carson that Native Americans had ambushed their party. The Native Americans killed the men, and the women are staked to the ground, sexually mutilated, and killed. The murderers then stole the Mexicans’ 30 horses. Carson and a mountain man friend, Alexis Godey, went after the murderers. It took the two men, two days to find the culprits. The pair rushed into their camp and killed and scalped two of the murderers. The horses were recovered and returned to the Mexican man and boy. This act brought Carson even greater reputation and confirmed his status as a western hero in the eyes of the American people.

The Mexican government ordered Frémont to leave. Frémont returned to Washington, DC and filed his reports. He but did not mention the California trip. The government liked his reports but ignored his illegal trip into Mexico. Frémont was made a captain. The newspapers nicknamed Fremont, “The Pathfinder.”

Third expedition, 1845

In 1845, Carson lead Frémont on a third expedition. Leaving Westport Landing, Missouri, they crossed the Rockies, passed the Great Salt Lake, and down the Humboldt River to the Sierra Nevada of California and Oregon. The third expedition is more political in nature. Frémont may have been working under secret government orders. US President Polk wanted Alta California, which includes parts of California, Arizona, Nevada, Utah and parts of Wyoming.

Once in California, Frémont set out to rouse American settlers into a patriotic fervor. The Mexican General Jose Castro at Monterey ordered him to leave. On Gavilan Mountain, Frémont erected a makeshift fort and raised the American Flag in defiance to these orders. While in Oregon, while camped near Klamath Lake, a messenger from Washington, DC, caught up with Fremont and made it clear that Polk wanted California.

On 30 March 1846, while traveling north along the Sacramento Valley, Fremont’s expedition met a group of Americans Settlers. The settlers claimed that a band of Native Americans was planning to attack them. Frémont’s party set about searching for Native Americans. On April 5 1846, Frémont’s party spotted a Wintu village and launched a vicious attack, which resulted in the deaths of approximately 120 to 300 men, women, and children and the displacement of many more. This act of savagery became known as the Sacramento River massacre. Carson, later stated that “It was a perfect butchery.

Army

Kit Carson accepted a commission as a colonel in the U.S. Army in 1861, Carson fought against Native American and Confederate forces in several actions.

His fame was then at its height,… and I was very anxious to see a man who had achieved such feats of daring among the wild animals of the Rocky Mountains, and still wilder Indians of the plains…. I cannot express my surprise at beholding such a small, stoop-shouldered man, with reddish hair, freckled face, soft blue eyes, and nothing to indicate extraordinary courage or daring. He spoke but little and answered questions in monosyllables.

Northern Civil War General William Tecumseh Sherman

References

Old Spanish Trail

The Old Spanish Trail was a historic trade route that linked Santa Fe, New Mexico to Los Angeles, California. The trail was established in the early 19th century and was primarily used for the transportation of goods, such as furs, horses, and mules.

The Told Spanish Trail BLM Sign
The Told Spanish Trail BLM Sign

The trail began as a network of routes used by Native American tribes, who traded goods such as salt, obsidian, and turquoise. In the late 18th century, Spanish traders began to use these routes to transport goods between Santa Fe and California. These traders were known as the “Comancheros” and were primarily focused on trading with the Ute and Navajo tribes in the area.

The route became known as the Old Spanish Trail in the early 19th century, when American traders began using the trail to transport furs and other goods to California. The trail was difficult to traverse, with harsh deserts, steep mountains, and treacherous canyons, but it was a vital link between the Southwest and the West Coast.

The trail was not a single route, but rather a network of different paths that crossed the desert and mountains of the Southwest. The most popular route followed the Virgin River in Utah, crossed the Colorado River at the mouth of the Virgin River, and then passed through the Mojave Desert to Los Angeles. Another route followed the Gila River in Arizona and crossed the Sonoran Desert to California.

The Old Spanish Trail played an important role in the development of the American West, as it provided a direct link between the remote and isolated communities of the Southwest and the growing cities of California. The trail was also a source of conflict, as American traders often clashed with Native American tribes over access to resources and trading rights.

In the mid-19th century, the discovery of gold in California brought thousands of settlers to the West Coast, and the Old Spanish Trail became a major thoroughfare for travelers and goods. The trail was also used by the Mormon pioneers, who traveled to California in the late 1840s and early 1850s.

In the late 19th century, the construction of railroads and highways made the Old Spanish Trail less important as a trade route. However, the trail remained an important part of the cultural history of the American Southwest, and efforts were made to preserve the trail and its landmarks.

Today, several sections of the Old Spanish Trail have been designated as National Historic Trails by the National Park Service, including sections in Utah, Colorado, New Mexico, and California. These trails allow visitors to experience the beauty and history of the Old Spanish Trail and to appreciate the legacy of the traders, Native Americans, and settlers who traveled its rugged terrain.

Old Spanish Trail Routes

All routes came together at Fork of Roads, east of present-day Barstow in the Mojave desert, and then crossed Cajon Pass between the San Gabriel and San Bernadino Mountains to Coastal California. After negotiating the pass, traders had an easy two to three days travel to the San Gabriel Mission and beyond to Los Angeles.

Armijo Route

Exterior, south facade of Mission San Gabriel Arcangel - 1878
Exterior, south facade of Mission San Gabriel Arcangel – 1878

The first complete trip across the trail began in Abiquiú, northwest of Santa Fe. The Armijo party followed well-known trails northwest to the San Juan River, then nearly due west to the Virgin River. They used the Crossing of the Fathers, cut into rock canyon wall some 75 years earlier by the Domínguez-Escalante party. Armijo’s caravan went down the Muddy River and across
the Mojave Desert to the Amargosa and Mojave Rivers, through Cajon Pass and down to Mission San Gabriel.

The Armijo and Northern Route diverge from each other on the east bound trail near the town of Tecopa, California.

Main Northern Route

First blazed by William Wolfskill and George C. Yount in 1831, this route veered northwest from Abiquiú through Southern Colorado and central Utah. It avoided the rugged canyons of the Colorado River that the Armijo party had encountered and took advantage of the better water and pasture resources across central Utah before returning to the Colorado River and Armijo’s route not far from Las Vegas.

Northern Branch

This route followed well-known trapper and trade routes north through the Rio Grande gorge to Taos and into southern Colorado. It then went west through Cochetopa Pass, largely open during the winter when other passes were snowed in and up the Gunnison River valley, rejoining the Northern Route near present-day Green River, Utah.

Mojave Road

Afton Canyon in the Mojave National Preserve.
Afton Canyon in the Mojave National Preserve.

The Mojave Road is a 188-mile crossing of the Mojave Desert long used by area Indians and by Spanish explorers and missionaries, it was first traveled by Jedediah Smith, an American trapper, in 1826.

Old Spanish Trail Locations

Government Holes in the central section of the Old Mojave Road.

Old Mojave Road

The Old Mojave Road (Government Road) is an east-west route that enters the Mojave National Preserve off the highway 95 in Nevada, and Afton Canyon…
The Old Spanish Trail BLM Sign

Old Spanish Trail

The Old Spanish Trail was a historic trade route that linked Santa Fe, New Mexico to Los Angeles, California. The trail was established in the…
Francisco Hermenegildo Tomás Garcés O.F.M. (April 12, 1738 – July 18, 1781)

Old Spanish Trail (Garces Expedition)

Old Spanish Trail (Garces Expedition) is a Nevada State Historic Marker Number 140 located in Clark County, Nevada. This marker is one of several which…
Captain John C. Frémont, explorer first mapped Diamond Valley Nevada

Old Spanish Trail (Journey of the Dead Man)

Old Spanish Trail (Journey of the Dead Man) is a Nevada State Historic Marker Number 139 located in Clark County, Nevada. This marker is one…

Old Spanish Trail Mountain Springs Pass – Nevada State Historic Marker

Old Spanish Trail Mountain Springs Pass is located along highway 160 and Nevada State Historic Marker No. 142 in Clark County, Nevada. The Old Spanish…
Old Tecopa house at smelter on Willow Creek, Amargosa Valley. Dr. Noble, Mrs. Noble. Inyo County, CA. 1922 - Photo from Herbert E. Gregory Book 8: 1915 - 1924.

Tecopa Inyo County

Tecopa is a small town located in the southeastern part of California, United States and its named for Chief Tecopa. The town is situated in…
The Old Spanish Trail 1829-1850 - Nevada State Historic Marker 33

The Old Spanish Trail 1829-1850 – Nevada State Historic Marker 33

Old Spanish Trail 1829-1850 is Nevada State Historic Marker Number 33, located in the town of Blue Diamond, in Clark County, Nevada. The Old Spanish…
Old Spanish Trail 1829-1850 - Nevada State Historic Marker #34 located in Mountain Springs, Nevada

The Old Spanish Trail 1829-1850 – Nevada State Historic Marker 34

Old Spanish Trail 1829-1850 is Nevada State Historic Marker Number 33, located in the town of Mountain Springs, in Clark County, Nevada. Old Spanish Trail…

References