Big Bear, CA
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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.
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.
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.
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.
Jarbidge Community Hall – Nevada State Historic Marker 153
The Jarbidge Community Hall is a central gathering place for the residents of Jarbidge, Nevada. Built in 1939, the hall has served as a venue for community events, meetings, and social gatherings for more than 80 years. The hall is located on the main street of Jarbidge, and its distinctive Art Deco design makes it a landmark in the town.
The history of the Jarbidge Community Hall is intertwined with the history of the town itself. Jarbidge was founded in the late 19th century, during Nevada’s mining boom. The town was named after a nearby creek, and its population grew rapidly as miners flocked to the area in search of gold and silver.
By the early 20th century, Jarbidge had become an important mining town, with several mines operating in the area. The town’s population peaked in the 1920s, with around 1,500 residents. During this time, the town was home to several businesses, including hotels, saloons, and general stores.
However, the Great Depression hit Jarbidge hard, and the town’s mining industry began to decline. By the late 1930s, many of the mines had closed, and the town’s population had dwindled to just a few hundred people.
Despite the difficult times, the residents of Jarbidge remained committed to their community. In 1939, they came together to build a place to gather within the town. The building was designed by local architect Paul Revere Williams, who was one of the few African American architects working in the United States at the time. Williams was known for his Art Deco designs, and the Jarbidge Community Hall is one of his few surviving buildings in Nevada.
The Jarbidge Community Hall was built using local materials, including stone from a nearby quarry and wood from the surrounding forests. The hall’s Art Deco style is evident in its streamlined design, geometric shapes, and use of decorative elements such as the zigzag patterns on the building’s façade.
Over the years, the building has served as a venue for a wide range of events. In the early days, it was used for dances, social gatherings, and community meetings. During World War II, it was used as a venue for USO shows and other events to support the war effort. In the decades that followed, it continued to be a central gathering place for the residents of Jarbidge, hosting everything from weddings and birthday parties to town meetings and political rallies.
Today, the Jarbidge Community Hall remains an important part of the town’s identity. It is still used for community events and social gatherings, and it serves as a reminder of the town’s rich history and strong sense of community. The hall has been listed on the National Register of Historic Places since 1990, and it is considered one of the most significant Art Deco buildings in rural Nevada.
In recent years, the Jarbidge Community Hall has undergone several renovations to ensure that it remains a functional and attractive venue for the town’s residents. The building’s stone façade has been restored, and the interior has been updated with new flooring and lighting. The hall is now fully accessible, with a wheelchair ramp and updated restrooms.
Despite its small size, the Jarbidge Community Hall is a testament to the resilience and determination of the people of Jarbidge. It is a symbol of the town’s enduring spirit and its commitment to preserving its history and traditions for future generations.
Nevada State Historic Marker Text
Gold discoveries by Dave Bourne in 1909 created the town of Jarbidge.
With 1,500 population in Jarbidge Canyon by 1910, citizens built this pioneer-type community hail with a “floating” maple floor. Support from the Nevada Commission for Cultural Affairs and the community funded the restoration of the building.
STATE HISTORIC MARKER NO. 153
STATE HISTORIC PRESERVATION OFFICE
JARBIDGE COMMERCIAL HALL FUND AND IMPROVEMENT CLUB
Nevada State Historic Marker 153 Location
Jarbidge Community Hall Summary
| Name | Jarbidge Community Hall |
| Location | Jarbidge, Elko County, Nevada |
| Latitude, Longitude | 41.8783, -115.4303 |
| Nevada State Historic Maker | 153 |
References
Chuck Yeagers NF-104 Crash Site
On December 10, 1963, Chuck Yeager, a legendary test pilot, crashed while flying an F-104 Starfighter at Edwards Air Force Base in the Mohave Desert of California. The incident resulted in serious injuries for Yeager and the grounding of the entire NF-104 fleet.
Background
The NF-104 and F-104 are both variants of the Lockheed F-104 Starfighter aircraft, but they have some significant differences.
The F-104 is a supersonic jet fighter aircraft that was developed in the late 1950s for the United States Air Force (USAF). It was widely used by many countries, including Canada, Italy, Germany, and Japan. The F-104 had a single engine and was designed to be a high-performance interceptor aircraft. It had a maximum speed of Mach 2.2 and was capable of flying at high altitudes.
The NF-104, on the other hand, was a modified version of the F-104 that was used for high-altitude flight training. The “NF” stands for “NASA Flight” because it was used by the National Aeronautics and Space Administration (NASA) for astronaut training. The NF-104 was fitted with a rocket engine that allowed it to climb to higher altitudes than the F-104. The ceiling of the aircraft was supposed to be 125,000 feet. It was also equipped with a reaction control system (RCS) that allowed it to simulate the handling characteristics of a spacecraft.
Overall, the main differences between the F-104 and the NF-104 are that the latter had a rocket engine and RCS, which made it suitable for high-altitude flight training, while the former was a high-performance interceptor aircraft.
Chuck Yeager, on the other hand, was a highly experienced test pilot with a distinguished career. He was the first person to break the sound barrier in level flight, flying the Bell X-1 in 1947. Yeager was also known for his contributions to the development of several other aircraft, including the F-86 Sabre, the F-100 Super Sabre, and the B-58 Hustler.
The Crash
On December 10, 1963, Yeager was conducting a test flight of an NF-104 Starfighter equipped with a rocket engine at Edwards Air Force Base in California. The purpose of the flight was to evaluate the aircraft’s performance at high altitudes and high speeds. Yeager was flying at an altitude of 80,000 feet and a speed of Mach 1.5 when he experienced a loss of control.
According to Yeager’s account of the incident, he had just completed a steep climb to 108,000 feet and was beginning to level off when the aircraft suddenly pitched up and rolled to the left. Yeager attempted to recover the aircraft using the reaction control thrusters on. and applying opposite rudder and aileron, but the NF-104 continued to roll and dive and eventually fell into a flat spin.. Yeager ejected from the aircraft at an altitude of around 8,500 feet and landed safely, but he suffered several injuries, including a broken collarbone, several ribs, a punctured lung and severe burns to his face.
Investigation
Following the crash, the United States Air Force launched an investigation to determine the cause of the incident. The investigation revealed that the F-104 had a notoriously difficult flight envelope, with a high stall speed and a tendency to enter a flat spin at high angles of attack. The investigation also revealed that Yeager had been flying with a faulty attitude indicator, which may have contributed to the loss of control.
However, the investigation ultimately concluded that the cause of the crash was pilot error. The investigation found that Yeager had exceeded the aircraft’s design limitations by flying at an altitude and speed that were beyond the F-104’s safe operating range. The investigation also found that Yeager had not received adequate training on the F-104 and had not been briefed on the risks associated with flying the aircraft at high altitudes and speeds.
Consequences
The consequences of the NF-104 crash were significant. The incident highlighted the dangers of flying high-performance aircraft without adequate training and briefing. As a result, the United States Air Force grounded the entire NF-104 fleet until additional training and safety measures could be implemented. The incident also led to changes in the way that test pilots were trained and briefed on new aircraft.
In 1922, the movie Top Gun: Maverick featured a similar incident written into the story of the movie. Tom Cruise’s character, Maverick is attempting to reach a new speed record or Mach 10, when, at high alititude he is forced to bail our of the experimental plane he was piloting.
Crash Location
Chuck Yeager’s NF-104 cam to rest in the Mohave Desert, just west of I-14 and south of California City Blvd.
Summary
| Name | Chuck Yeagers NF-104 Crash Site |
| Location | Mojave Desert, Los Angles County, California |
| Date of Incident | December 10th, 1963 |
| Latitude, Longitude | 35.1236, -118.1469 |