Category: Articles

The Providence Mountains are a mountain range located in the eastern Mojave Desert of San Bernardino County, California, within the Mojave National Preserve. This range is known for its striking geological features, rich biodiversity, and historical significance. One of the highlights of the Providence Mountains is the Mitchell Caverns, part of the Providence Mountains State Recreation Area, which showcases fascinating limestone caves with various natural formations such as stalactites, stalagmites, and other speleothems.

Geologically, the Providence Mountains are part of the greater Basin and Range Province, characterized by their rugged, linear ranges and intervening valleys. They offer diverse habitats, from desert scrub at lower elevations to pinyon-juniper woodlands at higher altitudes, supporting a wide array of wildlife and plant species.

The area has a rich history, from Native American use to European exploration and mining in the 19th and 20th centuries. Indigenous peoples traversed the mountains and surrounding areas for thousands of years, and more recently, they were mined for silver, iron, and other minerals during the boom periods of the American West.

The Mojave National Preserve, where the Providence Mountains are located, provides opportunities for outdoor activities such as hiking, camping, wildlife viewing, and exploring the scenic beauty of the desert landscape. The preserve’s conservation and restoration efforts help protect this unique area’s natural and cultural resources for future generations.

Providence Mountains

Providence Mountains (Gold-Iron) The gold mines in the Providence Mountains that were first worked lay south of Foshay Pass, and were discovered as early as …

Gold and Iron in the Providence Mountains

California Ghost Town – Providence

Providence ghost town in the Mojave Preserve, California Mojave Desert.

Providence Mines

In the Trojan mining district of the Providence Mountains are located the properties of the Bonanza King Development Company of Los Angeles. This property …

Providence Mountains – Lanfair Valley: Mojave Desert Ecological …

Providence Mountains – Lanfair Valley · Lithology and Stratigraphy. The uplands in this subsection are mainly Mesozoic granitic, Tertiary volcanic, Paleozoic …

Providence Mountains Miners Run Off by Indians

For the period of the 1850s the records of mining activities on the Mojave Desert are very scant, as the prospectors were few and the work was on a minor scale.

Providence Mountains – Notes

Providence, East Mojave Desert Historical Sites

Along the steep slopes of the Providence Mountains, south of the Clark Mining District, parties of prospects from Ivanpah found extremely rich silver ore …

Providence Mountains Mining History

Stream Terraces and Older Surfaces – Mojave Preserve – California …

Note how little relief exists on this alluvial fan surface on the eastern flank of the Providence Mountains. Close-up view of a desert pavement. A close-up …

Crystal Spring, Desert Springs, California Mojave Desert

Mojave National Preserve

Located in southern California, the desert area is a land of mountain ranges, sand dunes, great mesas and extinct volcanoes. Mojave contains several diverse …

Mitchell Caverns

Located in the heart of the Providence Mountains State Recreation Area at an elevation of 4,300 feet are the Mitchell Caverns. … Mojave Geomorphic Province

California Ghost Town – Providence

Chemehuevi Indians of the Mojave Desert

The Chemehuevi territory lay off the lower Colorado River north and west toward Death Valley and west to about the Providence Mountains. A less populated …

Mitchell Caverns

by Robert M. Norris. Like most limestone caves in other parts of the world, the Providence Mountains caves seem to have had a two-stage history.

Life at Mitchell Caverns

Rock cabin. Living at the caverns was to be Jack and Ida’s second honeymoon. “Two Lovers Shipwrecked on a Deserted Island.” They would live in the desert …

Physiography – Mojave Preserve – California Mojave Desert

The Mojave Desert comprises the southwestern quadrant of the Basin and Range physiographic province, a vast region dominated by rugged mountain ranges and …

Piute Mountains Wilderness

Piute Mountains, Mojave Desert Wilderness. … Providence Mountains – Lanfair Valley, Piute Valley – Sacramento Mountains

/lake-mead/ /temple-bar/

Temple Bar, located on the Arizona side of Lake Mead, has a rich history intertwined with the development and management of the Colorado River and the creation of Lake Mead itself. Lake Mead is a man-made reservoir formed by the Colorado River damming with the completion of the Hoover Dam in 1936. This dam was a monumental engineering project of its time, aimed at controlling floods, providing irrigation water, and generating hydroelectric power for the southwestern United States.

The name “Temple Bar” predates Lake Mead and is believed to have been named after a rock formation in the area resembling a temple. As Lake Mead filled, Temple Bar became an important recreational area. It is one of the many sites around Lake Mead that offers access to the water for boating, fishing, and other water sports, along with facilities for camping and lodging.

Before Lake Mead flooded the area, the region was home to indigenous peoples who left behind petroglyphs and other archaeological sites for thousands of years. With the arrival of European settlers, the area saw various uses, including as part of trade routes, mining operations, and later, as recreational sites once the dam was completed.

The creation of Lake Mead and facilities like Temple Bar marked a significant change in how the American Southwest dealt with water, turning the arid region into a place where large-scale agriculture and urban centers could develop, thanks to the availability of controlled water resources. Over the decades, Lake Mead has become not just a utilitarian body of water but also a major recreational destination, drawing visitors worldwide.

Environmental changes and challenges have also affected Lake Mead and Temple Bar. Water levels in the lake have fluctuated significantly in recent years due to ongoing drought conditions, impacting the area’s ecology and the human activities that depend on the lake. These changes have spurred efforts to manage water resources more sustainably and to balance the needs of urban development, agriculture, and the natural environment in the Colorado River Basin.

The history of Temple Bar, like much of the region around Lake Mead, is a testament to human ingenuity and adaptation in the face of harsh environmental conditions. It reflects broader themes in American and environmental history, including the impact of human activities on natural landscapes and the ongoing challenges of managing water resources in the West.

So, this story takes place north of the Mojave. However, it is still relevant to John C Fremont’s 1843-44 survey expedition of the Mojave Desert and how he lost a cannon.

“Fremont’s Lost Cannon” refers to a historical incident involving John C. Frémont, an American explorer, military officer, and politician. During one of his expeditions in the 19th century, specifically the third expedition (1845-1846) aimed at mapping and exploring the Western United States, John C. Frémont brought along a cannon for defense purposes. This expedition was crucial in the context of the U.S. expansion westward, including the period of the Mexican-American War.

The story goes that while traversing challenging terrains, including the Rocky Mountains and the Sierra Nevada, Frémont’s party faced significant difficulties. The terrain and conditions were so harsh that the expedition had to abandon the cannon in the snow to save themselves and their other supplies. This occurred as they attempted to cross the Sierra Nevada during the winter, which was an extraordinarily difficult and risky endeavor then.

The exact location where the cannon was abandoned has been a subject of speculation and interest among historians and treasure hunters. Some attempts have been made to find the lost cannon, but as far as public records indicate, it remains lost to history. The story of Fremont’s lost cannon is often cited as an example of the challenges faced by early explorers of the American West and the lengths to which they went in their efforts to map the continent and secure it for future American settlement.

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John C. Frémont, known for his exploration and mapping of the American West, did not explicitly have permission from the U.S. government to take a cannon on his expeditions. His expeditions, particularly the one in 1845-1846 leading into the beginning of the Mexican-American War, were officially for the purpose of mapping and exploration. However, the political and military context of the time suggests that his actions were not entirely outside the interests of the U.S. government.

Frémont was a lieutenant in the U.S. Army, and his expeditions were funded and supported by the government, specifically by the Corps of Topographical Engineers. The third expedition, which is often associated with the story of the lost cannon, was aimed at mapping the Oregon Trail and further exploring the Great Basin and California, which were not yet part of the United States but were of significant interest due to the manifest destiny ideology and tensions with Mexico.

Although there might not have been explicit permission for using a cannon, the military nature of his role and the implicit support of expansionist elements within the U.S. government suggests that his actions, including arming his expedition, aligned with broader U.S. interests in the region. Using a cannon could be considered a precautionary measure for defense against potential threats, considering the hostile territories they were exploring and the uncertain political situation with Mexico at the time.

Frémont’s expeditions, especially the third one, played a significant role in the U.S. expansion westward, contributing to the outbreak of the Mexican-American War and the eventual annexation of California and other territories to the United States. The ambiguity around permission for the cannon reflects the complex mix of exploration, military reconnaissance, and political maneuvering characteristic of U.S. westward expansion during that period.

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Jessie Benton Frémont, the wife of John C. Frémont, played a significant role in her husband’s expeditions, including the suggestion to take a cannon on his third expedition. Jessie was supportive of her husband’s ventures and actively involved in planning and advocating for his work. She was the daughter of Senator Thomas Hart Benton of Missouri, a prominent advocate of westward expansion, which likely influenced her interest and involvement in her husband’s exploratory missions.

Jessie Benton Frémont was known to be a strong and intelligent woman who understood the political and military implications of her husband’s expeditions. Her suggestion to take a cannon along on the expedition can be seen as a strategic move, understanding the potential for conflict and the need for protection in the uncharted territories they were to explore. The cannon symbolized both a means of defense and a statement of American power and intent in the face of foreign claims to the territories of the West, especially with tensions rising between the United States and Mexico over territories such as California.

Her involvement went beyond mere suggestions; Jessie was instrumental in editing and preparing Frémont’s reports and writings for publication, helping to shape the narrative of his expeditions and the image of the American West in the minds of the U.S. public and policymakers. These reports played a significant role in drumming up support for westward expansion and contributed to the mythology of the American frontier.

Jessie Benton Frémont’s suggestion to take a cannon underscores her understanding of the complexities of the expedition, not only in terms of exploration but also in the context of national ambition and security.

/landers-ca/

The Integratron is a unique and historic structure located in Landers, California, near Joshua Tree National Park. Designed by George Van Tassel, who was an aeronautical engineer, ufologist, and contactee, the Integratron is a 38-foot high, 55-foot diameter, all-wooden dome that was constructed without the use of nails to ensure a perfect acoustical environment. Van Tassel claimed that the Integratron was capable of rejuvenation, anti-gravity, and time travel and that its design was inspired by Moses’ Tabernacle and the work of Nikola Tesla. The building sits on a powerful geomagnetic vortex in the Mojave Desert, adding to its mystical appeal. Today, the Integratron is known for its “Sound Bath” experiences, offering visitors deep relaxation, rejuvenation, and introspection through the use of sound waves generated within the structure’s acoustically perfect dome​

/joshua-tree/indian-cove/

Indian Cove is a popular area within Joshua Tree National Park, known for its stunning rock formations, unique desert landscapes, and accessibility for camping and rock climbing. Located in the Mojave Desert of California, this area offers a different experience than the park’s main parts due to its unique geology and vegetation. Indian Cove is characterized by its towering rock walls, which make it a favorite spot for climbers of various skill levels.

The campground at Indian Cove is nestled among the massive boulders, providing a scenic backdrop for campers. It’s one of the few campgrounds in Joshua Tree National Park that can be reserved in advance, making it a convenient option for visitors planning their trip. The area also features several hiking trails, ranging from easy walks to more challenging hikes, allowing visitors to explore the desert landscape and wildlife.

Indian Cove is accessed from a road different from the main park entrances, located off Highway 62, which makes it somewhat separate from the rest of Joshua Tree National Park. This separation adds to its secluded and exclusive feel, although it is still part of the park and subject to the same rules and regulations.

Visitors to Indian Cove can enjoy the natural beauty and outdoor activities and the opportunity to experience the quiet and solitude of the desert. Nighttime brings clear, starry skies, making it an excellent location for stargazing.

To visit Indian Cove, it’s important to check the latest information on Joshua Tree National Park’s official website or contact the park directly for current conditions, campground availability, and any specific requirements or restrictions that may be in place.

Like in many desert environments, natural erosion in the Mojave Desert is a process influenced by a combination of factors, including wind, water, temperature fluctuations, and biological activity. These forces work together to shape the landscape over time, contributing to the unique features characteristic of the desert. Here’s an overview of how these factors contribute to natural erosion in the Mojave Desert:

1. Wind Erosion: Wind is a significant agent of erosion in the Mojave Desert. Strong winds can pick up and transport sand and smaller particles in a process known as deflation, leaving behind larger rocks and creating features such as sand dunes and yardangs (streamlined rock formations carved by wind-blown sand). Wind erosion can also polish and shape rocks and landforms through a sand-blasting effect.
2. Water Erosion: Although the Mojave Desert is known for its arid climate, it does experience occasional heavy rains and flash floods, especially during thunderstorms. These sudden downpours can rapidly erode the landscape, carving out gullies and washes and shaping canyons and valleys. Water erosion is particularly effective because the dry, compacted soil and sparse vegetation offer little resistance to the force of running water.
3. Temperature Fluctuations: The Mojave Desert experiences extreme temperature variations between day and night, contributing to mechanical weathering, which breaks down rocks without chemical change. This occurs as minerals in the rocks expand and contract at different rates due to the temperature changes, leading to the formation of cracks and ultimately causing the rocks to break apart. Over time, this process further breaks down rock materials that can be more easily eroded by wind and water.
4. Biological Activity: The activity of organisms, including plants, animals, and microorganisms, can also contribute to erosion in the Mojave Desert. For example, the roots of plants can grow into cracks in rocks, eventually prying them apart. Burrowing animals can move soil and rock, exposing new surfaces to erosion. Microbial and fungal activity can also chemically weather rock surfaces, making them more susceptible to erosion.
5. Chemical Erosion: Although less visible, chemical weathering plays a role in shaping the Mojave Desert landscape. This involves the breakdown of rocks through chemical reactions, such as the dissolution of minerals by water. This process can be particularly evident in areas with saline soils and water sources, forming unique mineral deposits and features.

These natural erosion processes are slow and occur over long periods, gradually sculpting the desert’s landscape into its current form. The interaction of these factors creates a dynamic environment where landforms are continuously shaped and reshaped, contributing to the diverse and striking landscapes found in the Mojave Desert.