Transmogrification

Transmogrification, though it carries a slightly literary, almost mythic tone, suggests not just change but a deep and strange transformation into something fundamentally different.

For much of its recorded history, the Mojave Desert was primarily understood as a physical region. Its identity arose from terrain and climate. Dense or permanent human occupation played little role. Early travelers, surveyors, geologists, and writers described it using the language of the landform. They noted broad basins, isolated mountain ranges, dry lakes, volcanic fields, alluvial fans, dunes, washes, and the intermittent course of the Mojave River. The desert was seen as a geographical system. Uplift, erosion, aridity, and distance formed it. Its boundaries were often indistinct. The Mojave was not yet a tightly organized human landscape. It was seen as open country, with character shaped by the land’s form.

In that earlier conception, geography imposed limits upon people. Travel followed springs, canyon mouths, and natural passes through the mountains. Camps and settlements clustered where water permitted survival. Roads bent around lava flows, crossed playas, or traced older Indigenous routes refined over generations of movement through the desert. Human activity existed within conditions dictated by climate and terrain. The desert remained the dominant force, and people adapted themselves to it.

Even with these earliest permanent intrusions, the long-standing dynamic between people and landscape was not immediately overturned. Mining camps rose and disappeared as ore deposits and water supplies fluctuated. Wagon roads faded when springs failed. Small railroad towns appeared abruptly but often remained fragile in the face of the scale and hostility of the surrounding landscape. Much of the Mojave still retained the appearance of a place shaped principally by geology rather than by civilization.

Over time, a shift occurred: the Mojave, once defined by natural systems, increasingly came to be structured around human needs. The first key shift came with railroads, which established artificial centers in previously insignificant locations—places that had mattered only as crossings or water stops. Afterward, elements like highways, aqueducts, transmission corridors, military reservations, utility infrastructure, suburban expansion, recreational development, industrial agriculture along the margins, and large-scale energy production continued this trend. These forces did not simply occupy the desert; they actively reorganized it.

A modern map of the Mojave clearly reveals this shift: vast military boundaries now dominate entire valleys and mountain ranges. Meanwhile, interstate highways create strong directional corridors across what were once diffuse travel landscapes. Utility-scale solar developments, visible for miles, convert open basins into industrial energy fields. Transmission towers march across dry lakes and bajadas. Off-road recreation networks carve repeating tracks into fragile terrain. Finally, conservation areas and national preserves add another layer of organization by establishing access restrictions, managing habitats, providing tourism infrastructure, and developing preservation policies.

Increasingly, the Mojave is understood less through watersheds and landforms than through jurisdiction and use. One valley becomes associated with military training, another with renewable energy, others with recreation, habitat protection, logistics, or suburban expansion. This shift is reflected in the language used to describe the desert. Whereas earlier generations emphasized playas, volcanic mesas, spring systems, or mountain passes, modern discussions focus on renewable energy zones, conservation plans, transportation corridors, protected acreage, groundwater management, housing pressure, and recreational access.

Yet the older desert has not disappeared beneath these overlays. The geology remains the controlling framework beneath every human system. Basin-and-range topography still governs drainage and movement. Mountain ranges still create rain shadows and isolate valleys. Heat still limits settlement density. Water scarcity still defines possibility. Dry lakes still gather runoff after storms, just as they did centuries ago. In many places, the desert resists permanent transformation. Every generation is reminded that the underlying landscape remains older and more powerful than any system laid upon it.

Building on these evolving layers of meaning, what has changed most is not simply the Mojave’s physical appearance but its significance. The desert has shifted in its conceptual role: initially perceived as a natural form, then as a landscape of use, and now increasingly as a landscape of negotiation.

The central question is no longer merely “What is the Mojave?” but “What is the Mojave for?” Different groups now approach the same landscape with competing visions: energy developers see open basins suitable for solar fields and transmission infrastructure; conservationists see fragile ecosystems, migration corridors, and biological continuity; tribes see ancestral homelands, sacred sites, and cultural memory in the terrain itself. The military sees strategic training space, defined by isolation and open airspace, while residents see communities and livelihoods. Recreationists seek freedom, mobility, solitude, and escape, while cities beyond the desert offer land, water, transportation routes, and energy supplies.

As these pressures intensify, nearly every part of the Mojave acquires overlapping claims—emptiness itself becomes contestable. Open land is no longer simply open; instead, it becomes designated, managed, leased, protected, restricted, industrialized, or defended. Consequently, the future Mojave is likely to be shaped not by a single activity, but by tensions among many competing systems, all operating simultaneously across the same terrain.

In this evolving context, the Mojave is entering a third historical phase. Initially, it was defined by its physical landforms. Next, human activities and uses became the defining factors. Now, the Mojave’s identity may increasingly depend on negotiations and conflicts over its meaning, access, and purpose.

The old desert will still remain beneath these arguments. The playas will still whiten under summer heat. Winds will still sweep across creosote flats. Mountain ranges will still rise abruptly from broad basins at dusk. Seasonal floods will still cut across washes after sudden storms. The geological skeleton of the Mojave will endure. However, as human systems become more extensive and entangled, the experience and interpretation of the desert will continue to change.

The future Mojave will be governed as a layered landscape. No single authority will determine its fate: federal agencies will control vast public lands; counties will regulate roads, zoning, and development pressure; tribes will press claims rooted in sovereignty, memory, and sacred geography; energy and mining companies will seek permits, leases, and corridors; conservation groups will defend habitat and species; recreationists will demand access; and residents will argue for the right to live within the desert, not just be managed from outside. In light of these overlapping interests, governance will become less about drawing boundaries and more about arbitrating between claims. The desert will be administered through plans, lawsuits, permits, consultations, closures, leases, and exceptions. Its future will not be decided all at once; instead, it will be determined valley by valley, corridor by corridor, and project by project.

The Mojave functions as both an ancient physical landscape and a modern human one. While it is no longer shaped solely by tectonics, erosion, and climate, it is no longer defined solely by railroads, highways, military reservations, and energy development. Increasingly, the desert is formed by negotiations over how such a landscape should exist. Thus, what once was defined by its form is now shaped by the competing meanings people assign to it.

Bear Valley

Historical Timeline

Big Bear, California, began as Yuhaaviatam homeland, later drawing gold seekers, ranchers, and dam builders. From Holcomb Valley’s 1860 rush to a four-season resort, its story blends natural beauty, resource ingenuity, and mountain tradition.

Bear Valley plants and trees

Prehistory
• The Big Bear Valley has been inhabited for thousands of years by the Yuhaaviatam (Serrano) people, who live in seasonal villages and call the area “Yuhaaviat,” meaning “Pine Place.”

1845
• Benjamin Davis Wilson leads a posse into the San Bernardino Mountains in pursuit of raiders. The group encounters numerous grizzly bears and kills several, naming the area “Big Bear Valley.”

1850s
• Early trappers and cattlemen moved through the San Bernardino Mountains. The valley remains largely remote and unsettled.

1860
• William F. “Bill” Holcomb discovers gold in Holcomb Valley, triggering a rush that brings hundreds of miners and creates mining camps such as Belleville, Union Town, and Clapboard Town.

1861–1862
• The Holcomb Valley boom peaks; San Bernardino County’s population surges. Belleville nearly becomes the county seat but loses to San Bernardino by two votes.

1863–1865
• Decline of the first gold boom as surface gold plays out. Miners leave, and the valley returns to quiet ranching and logging activity.

1870s
• Elias J. “Lucky” Baldwin acquires mining claims around Baldwin Lake and forms the Gold Mountain Mining Company. A second wave of mining begins, centered on the Baldwin Mine.

1884
• Frank Elwood Brown, a Redlands citrus grower, constructs the first Bear Valley Dam, a single-arch granite structure. The reservoir created by this dam was named Big Bear Lake.

1890s
• Big Bear’s role shifts from mining to recreation. Hunters, anglers, and early tourists begin to visit the mountain lake area. Lodges and cabins start to appear.

1903
• Lower-valley growers formed the Bear Valley Mutual Water Company to manage the reservoir and water rights.

1910–1912
• A new multiple-arch dam, designed by John S. Eastwood, replaces Brown’s dam, raising the lake level by about 20 feet and greatly expanding its capacity.

1920s
• Roads improve, and the automobile brings increased tourism. The town of Pineknot develops on the lake’s south shore with lodges, stores, and resorts.

1930s
• Winter recreation grows. Early ski runs are cut, and lodges cater to both summer and winter visitors.
• 1938 – Pineknot officially changes its name to Big Bear Lake.

1940s
• Big Bear becomes a year-round resort. During World War II, mountain roads were used for military transport training, but the area remained largely a recreation destination.

1950s
• Big Bear Alpine Zoo opens as a rehabilitation center for injured wildlife (1959).
• Ski development accelerates with lifts at Snow Summit.

1960s
• Tourism and second-home construction expand rapidly.
• The Big Bear Valley Historical Society was founded in 1967.

1970s
• The community continues to grow, balancing tourism with environmental concerns.

1980
• The City of Big Bear Lake was incorporated on November 28.

1980s
• Alpine Slide at Magic Mountain opens (1983).
• Ongoing improvements in highways and infrastructure make Big Bear a popular four-season resort.

1990s
• Big Bear becomes known for altitude training by professional athletes, including world-class boxers.

2000s–Present
• Tourism, recreation, and environmental stewardship define the region.
• The old 1884 dam remains a historical landmark, sometimes visible during low water levels.
• Big Bear preserves its mountain-resort heritage while serving as a gateway to the San Bernardino National Forest.

Big Bear and the Digital Desert are closely related through geography, ecology, history, and human development. The Digital Desert’s broader Mojave focus naturally overlaps with Big Bear’s transitional mountain-desert setting in several key ways:


Geographic Connection
Big Bear sits at the top of the Santa Ana River watershed, where mountain snowmelt begins the river’s underground journey to Southern California hills and valleys.


Ecological Transition Zone
The region bridges montane and desert biomes. Pinyon-juniper woodlands, chaparral, and Joshua tree habitats meet higher-elevation conifer forests. This gradation provides examples of how altitude, temperature, and moisture shape plant and animal communities—central themes within the Digital Desert’s ecological framework.


Historical Ties
Figures like William Holcomb and Lucky Baldwin tie Big Bear’s mining story to other desert mineral ventures, including Holcomb Valley’s influence on later Mojave mining booms. Trails from Big Bear connected to routes leading toward Lucerne Valley, Johnson Valley, and beyond—pathways that also appear throughout Mojave Desert exploration and settlement history.


Water and Infrastructure
The Bear Valley dams (1884 and 1912) represent early Southern California water engineering that parallels other Digital Desert themes such as aqueducts, irrigation systems, and the transformation of desert hydrology. Big Bear’s water storage directly supported the agricultural valleys below, tying mountain runoff to desert life.


Cultural and Recreational Link
Both Big Bear and the Mojave represent frontier landscapes turned into recreation destinations. The same pioneer spirit that shaped desert communities like Apple Valley or Hesperia carried over into Big Bear’s tourism development—cabins, roads, and storytelling built around rugged independence and mountain allure.


Interpretive Relationship
Within the Digital Desert framework, Big Bear serves as a high-elevation counterpart—a living case study for water origins, ecological transition, and cultural continuity. It connects the snow-fed headwaters to the dry basins below, showing the mountain-desert system as one continuous, interdependent landscape.

Ecological Description

Big Bear Valley lies high in the San Bernardino Mountains, about 6,700 to 7,000 feet above sea level, forming a broad mountain basin surrounded by rugged granite peaks and forested ridges. The valley stretches roughly east–west, framed by Butler Peak and Delamar Mountain to the north, and Sugarloaf Mountain, Gold Mountain, and the San Gorgonio massif to the south and east.

The valley floor is relatively flat, a remnant of ancient glacial and erosional processes, with Big Bear Lake occupying its central depression. Originally a meadowed valley with creeks and marshes, it became a permanent lake after the Bear Valley Dams were built. The soils are derived from decomposed granite, supporting open forests and meadows interspersed with boulder-strewn slopes.

Ponderosa pine, Jeffrey pine, white fir, and incense cedar dominate the higher slopes. At the same time, black oak, manzanita, and chaparral fill the lower edges in sheltered meadows and along streams, willows and alders grow, creating rare wetland habitats for species such as the mountain yellow-legged frog and bald eagle.

The climate is alpine-mediterranean—cold, snowy winters and warm, dry summers—marked by dramatic seasonal shifts. Snowmelt feeds Big Bear Creek and Baldwin Lake, the latter a seasonal alkali flat on the eastern edge of the valley.

Ecologically, Big Bear Valley forms the upper boundary of the Mojave Desert drainage system. It captures mountain precipitation that ultimately seeps underground toward Lucerne and the Mojave River basin, linking the high forest to the desert below.

Timeline References

  1. Big Bear Valley Historical Museum. “History of Big Bear Valley.” Big Bear Valley Historical Society, Big Bear City, CA.
  2. BigBear.com. “Dam: The Creation of Big Bear Lake.” Big Bear Visitors Bureau.
  3. BigBearCabins.com. “About Big Bear: A History.” Big Bear Cabins Travel Guide.
  4. BigBearVacations.com. “A History of Big Bear.” Big Bear Vacations Blog.
  5. San Bernardino County Museum Archives. “Mining and Settlement in the San Bernardino Mountains.”
  6. Eastwood, John S. “The Multiple-Arch Dam of Bear Valley.” Engineering Record, 1912.
  7. U.S. Forest Service. “San Bernardino National Forest: Ecological Subsections and Watershed Overview.”
  8. Bear Valley Mutual Water Company. “Early Development and Water Rights History.”
  9. Langenheim, Jean H., and P. H. Osman. “Vegetation and Ecology of the San Bernardino Mountains.” University of California Publications in Botany, 1959.
  10. California Department of Fish and Wildlife. “Baldwin Lake Ecological Reserve Management Plan.”
  11. San Bernardino Valley Water District. “Hydrologic History of the Bear Valley and Mojave River System.”
  12. Wikipedia contributors. “Big Bear Lake, California.” Wikipedia, The Free Encyclopedia.
  13. Wikipedia contributors. “Big Bear Valley Historical Museum.” Wikipedia, The Free Encyclopedia.
  14. Brown, F. E. “The First Bear Valley Dam and the Redlands Water System.” Redlands Historical Society Papers, 1884–1905.
  15. U.S. Geological Survey. “Geology and Hydrology of the Big Bear Lake Region, San Bernardino County, California.” Professional Paper Series.

Bear Lake, Baldwin Lake and Big Bear Lake

In the summer of 1845, Benjamin D. Wilson, who owned part of the interest in the Jurupa Rancho, the site of the present city of Riverside, led a troop of Calvary in search of cattle rustlers.

Setting out from San Bernardino Valley, he divided his command. Most of the men he sent through Cajon Pass, keeping only 22 Mexican troopers with him to follow a trail across the mountains. Two days later, Wilson and his men reached the lake, where they sighted scores of grizzly bears.

Big Bear Lake

Most of the soldiers had been vaqueros. They formed in pairs and drew reatas, each pair attacking a bear. One looped a rope around the bear’s neck; his companion roped the same bear by a hind foot. Then, the men drew apart to stretch the rope taut and hold the bear a prisoner. They bagged and skinned eleven bears, stretched their hides, and continued across the mountains to join the rest of the command on the desert at Rancho Las Flores, on the Mojave River.

Here, the reunited party engaged Indians in a fight, after which Wilson and his 22 vaquero-troopers returned home by the lake. They again found the place overrun with bears, and the same 22 soldiers brought in eleven more bears—enough to give them a bear rug apiece as a trophy. It was then that Wilson gave the little body of water the name Bear Lake.

Years later, the name was changed to Baldwin Lake. The name survives, however, in Big Bear Lake, which was created at the site of the Talmadge Ranch in 1884, when a dam was built to provide a constant water supply for the Redlands District.


Adapted from ~ Pioneer Tales of San Bernardino County – WPA – 1940.