Articles – Page 22

Paleontology

PALEONTOLOGY – Mojave Desert – Glossary of Terms and Definitions

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The study of fossils and their relation to geologic time. … Paleontology Miocene fossils have been found in the cliffs of Red Rock Canyon. Scientists continue …

Mojave Desert Paleontology

The study of fossils and their relation to geologic time.

Paleontology in Red Rock Canyon

Wrightwood, Ca. Mountain Hardware Wrightwood, Ca. Canyon Cartography · DesertLink. Links to Desert Museums, Grizzly Cafe Family Dining …

Geology of the Mojave River

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The river flows below the surface for much of its length and only intermittently at the surface. The Mojave River, an arid desert lifeline, supplies water and …

Fossils, Rocks, and Time: Fossils and Rocks

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Geology : Paleontology. FOSSILS AND ROCKS. To tell the age of most layered rocks, scientists study the fossils these rocks contain. Fossils provide important …

Red Rock Canyon California State Park

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Red Rock Canyon State Park, Mojave California, Mojave Desert.

Fossils, Rocks, and Time: The Relative Time Scale

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Geology : Paleontology. THE RELATIVE TIME SCALE. Long before geologists had the means to recognize and express time in numbers of years before the present …

Fossils, Rocks, and Time: The Numeric Time Scale

digital-desert.com › paleontology › numeric

Geologic time scale showing both relative and numeric ages. Ages in millions of years are approximate. Nineteenth-century geologists and paleontologists …

Fossils, Rocks, and Time: Fossil Succession

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Geology : Paleontology. FOSSIL SUCCESSION. Three concepts are important in the study and use of fossils: (1) Fossils represent the remains of once-living …

Fossils, Rocks, and Time: Putting Events in Order

digital-desert.com › paleontology › order

Geology : Paleontology. PUTTING EVENTS IN ORDER. Scientists who study the past try to put events in their proper order. When we discuss events that happened …

Fossils, Rocks, and Time: Table of Contents

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Geology : Paleontology. FOSSILS, ROCKS, AND TIME. INTRODUCTION. We study our Earth for many reasons: to find water to drink or oil to run our cars or coal …

FOSSIL – Mojave Desert – Glossary of Terms and Definitions

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The Fossil Canyon Loop Road is an interesting route for vehicle touring. … Mojave Desert Paleontology The study of fossils and their relation to geologic …

Fossils, Rocks, and Time: Rocks and Layers

digital-desert.com › paleontology › rocks-layers

Geology : Paleontology. ROCKS AND LAYERS. We study Earth’s history by studying the record of past events that is preserved in the rocks. The layers of the …

Mojave Desert – Scavenger

mojavedesert.net › glossary › scavenger

Paleontologists are … Raven – Desert Wildlife. Raven – Raven Also see > Bird: Omnivore : Scavenger: Predator: Diurnal Mammals – Predators Mountain Lion · …

Mojave Desert Geology

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Paleontology. The scientific study of prehistoric plants and animals in their geologic context. Alluvial material in dry wash. Dry Lake – Playa Desert Varnish …

Red Rock Canyon – Mojave California

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Located in the southern El Paso Mountains, these colorful cliffs with their stark beauty and unique features have attracted hikers, geologists, paleontologists, …

Cajon Pass Geology

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Pliocene and Pleistocene evolution of the Mojave River, and associated tectonic development of the Transverse Ranges and Mojave Desert, based on borehole …

Dr. Joan S. Schneider

mojavedesert.net › people › schneider-joan

Mojave Desert History > Names in History. Dr. Joan S. Schneider. Photo of Dr Joan Schneider at Joshua Tree National Park Joan S. Schneider, Ph.D.

ANTIQUITIES – Mojave Desert – Glossary of Terms and Definitions

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ANTIQUITIES – A general term for archaeological or paleontological resources which are at least 100 years of age and which tangibly represent or have the …

Lake Mead

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Three of America’s four desert ecosystems–the Mojave, the Great Basin, and the Sonoran Deserts–meet in Lake Mead NRA. As a result, this seemingly barren area …

References – Mojave Preserve – California Mojave Desert

digital-desert.com › mojave-preserve › geology

Hewitt, D.F., 1956, Geology and mineral resources of the Ivanpah quadrangle, California and Nevada: U.S. Geological Survey Professional Paper 275, 172 p.

The Grand Canyon

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Grand Canyon National Park, a World Heritage Site, encompasses 1,218,375 acres and lies on the Colorado Plateau in northwestern Arizona. The land is semi-arid …

RELATIVE DATING – Mojave Desert – Glossary of Terms and …

mojavedesert.net › glossary › relative-dating

RELATIVE DATING – A method of dating rock layers by their relationships or proximity to each other. Both archaeologists and paleontologists use relative dating.

Elizabeth Campbell

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Elizabeth Campbell. Photo of Elizabeth Campbell, Mojave Desert archeologist. NPS photo – colorized. Elizabeth Warder Crozer was born in August of 1893 into a …

Grand Canyon natural environments

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Near the Colorado River, riparian vegetation and sandy beaches prevail. Just above the river corridor a desert scrub community exists complete with a wide …

Kokoweef Caves

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Kokoweef and the mysterious river of gold in the Mojave Desert.

Cajon Pass Heritage

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Heritage resources in the Cajon Pass region of the Mojave Desert.

Mojave Desert – Glossary of Terms and Definitions

mojavedesert.net › glossary

Mojave Desert Glossary. The following definitions may be helpful. In most instances, they may not be specific to, or, all-inclusive of, the Mojave Desert.

Kokoweef

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If there were what may be trillions of dollars in gold lying at the bottom of an ‘unrediscovered’ river running from the Great Basin under the Mojave Desert to …

Rainbow Basin

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Land ownership status can be found on the “Cuddeback Lake” Desert Access Guide. These BLM maps can be purchased from any California Desert District BLM …

The 1872 Owens Valley earthquake was a significant seismic event on March 26, 1872, in Owens Valley, California, USA. The earthquake is estimated to have had a magnitude of 7.4 to 7.9, making it one of the largest historical earthquakes in California.

Some key points about the 1872 Owens Valley earthquake:

Location: The earthquake’s epicenter was near Lone Pine in Owens Valley, in eastern California, near the eastern Sierra Nevada mountain range.
Effects: The earthquake caused extensive damage in the Owens Valley region. The town of Lone Pine suffered the most severe damage, with many buildings collapsing. In addition to the structural damage, the earthquake triggered ground ruptures, creating surface faulting along the eastern Sierra Nevada.
Surface Rupture: The earthquake is notable for the significant surface rupture that occurred along the Owens Valley fault. This rupture extended for about 30 miles (48 kilometers) and displaced the ground horizontally by as much as 15 feet (4.5 meters). This surface rupture remains visible today as a scar on the landscape.
Aftershocks: Numerous aftershocks followed the mainshock, continuing for several months. These aftershocks contributed to ongoing damage and hampered recovery efforts.
Impact on the Landscape: The earthquake caused changes to the landscape, including the formation of new fault scarps and the uplifting of land along the eastern Sierra Nevada. These changes are still studied by geologists today.
Historical Significance: The 1872 Owens Valley earthquake is historically significant in the study of seismic activity in California. It provided valuable data for understanding the behavior of faults and the effects of large earthquakes on the landscape.

It’s worth noting that the Owens Valley region remains seismically active, and scientists continue studying the area to understand future earthquakes’ potential better. The 1872 event serves as a reminder of the seismic hazards associated with the complex fault systems in California.

Lone Pine

Owens Valley

Eastern Sierra Nevada

Mormon Rocks

/mormon-rocks/

The Mormon Rocks, also known as the Rock Candy Mountains, are a series of distinctive sandstone outcrops in the Cajon Pass, a mountain pass in the San Bernardino Mountains of Southern California. The Cajon Pass is a critical transportation corridor connecting the Los Angeles Basin with the Mojave Desert and beyond.

Here are some key points about Mormon Rocks and their significance:

Location: The Mormon Rocks are within the Cajon Pass, traversed by Interstate 15 and several major railroad lines. The rocks are easily visible from the highway, making them a notable geological feature.
Geological Formation: The rocks are sedimentary sandstone and formed through tectonic and erosional processes over millions of years. The distinctive red and white banded appearance is due to iron oxide (hematite) and other minerals.
Cultural Significance: The Mormon Rocks have cultural and historical significance. The area is named after a group of Mormon pioneers who passed through the Cajon Pass in the mid-19th century during their westward migration. The rocks are a prominent landmark in the pass and have been featured in various forms of media.
Recreational Opportunities: The area around Mormon Rocks provides outdoor activities and recreation opportunities. There are trails and viewpoints where visitors can appreciate the geological formations and enjoy scenic views of the surrounding landscape.
Conservation: The Mormon Rocks are part of the San Bernardino National Forest, and efforts are made to preserve and protect the natural and cultural resources in the area.
Railroad Transportation: The Cajon Pass is a crucial route for road and rail traffic. The presence of the rocks adds to the landscape’s visual appeal and has made the pass a notable location for train enthusiasts who enjoy watching trains navigate the steep grades of the pass.

Whether you are interested in geology, history, or simply enjoying scenic landscapes, the Mormon Rocks in the Cajon Pass offer a unique and visually striking destination. If you plan to visit, be sure to follow any posted regulations and respect the natural environment.

Tejon Ranch

/beale-adobe/

The Tejon Ranch, located in California, has a rich and varied history that spans centuries.

Here is an overview of its history:

Native American Presence: The area around Tejon Ranch was originally inhabited by Native American communities, including the Kitanemuk people. These indigenous groups had a deep connection with the land, relying on its resources for their sustenance.
Spanish Era: With the arrival of Spanish explorers and missionaries in the 18th century, the Tejon Ranch area became part of the vast landholdings of the Spanish missions and the California missions system. The land was used for cattle ranching and agriculture to support the missions.
Mexican Land Grants: Following Mexico’s independence from Spain in 1821, the Mexican government began granting large tracts of land, including the Tejon Ranch, to private individuals. The Rancho El Tejon was granted to José Antonio Aguirre in 1843.
Gold Rush and Transition: The California Gold Rush of 1848-1855 brought significant changes to the region. The influx of people seeking gold and the economic and political shifts associated with the U.S.-Mexican War led to the end of Mexican land grants. 1852, the U.S. government affirmed the land grant, and Benjamin and James Roberts acquired the Rancho El Tejon.
Ranching and Agriculture: The Tejon Ranch became a center for ranching and agriculture. Cattle ranching, farming, and other activities flourished on the vast expanse of land. The ranch was crucial in supplying beef and other products to growing communities in Southern California.
Treaty of Fort Tejon: In 1854, the U.S. government negotiated the Treaty of Fort Tejon with various Native American tribes, including the Kitanemuk. However, the treaty was not fully implemented, leading to conflicts and struggles for the indigenous people.
Railroad Development: The Southern Pacific Railroad played a significant role in developing the Tejon Ranch. In the late 19th century, the railroad bypassed the Tehachapi Mountains, where the ranch is located, favoring a route through the nearby Tehachapi Pass. This decision affected the economic growth of the Tejon Ranch region.
20th Century and Beyond: The Tejon Ranch underwent various ownership and land use changes. In the 20th century, it evolved into a diversified operation involving agriculture, ranching, and commercial activities. The Tejon Ranch Company, established in the early 1900s, was key in managing and developing the property.

Today, the Tejon Ranch remains one of the largest privately-owned ranches in California, known for its conservation efforts, including partnerships with environmental organizations to preserve significant portions of the land as open space. The ranch’s history reflects the broader historical and cultural shifts in California, from indigenous habitation to Spanish colonization, Mexican land grants, and the economic transformations of the 19th and 20th centuries.

E.F. Beale and the Tejon Ranch

Edward Fitzgerald Beale, often referred to as E.F. Beale, played a significant role in the history of the Tejon Ranch.

Here’s an overview of his connection to the ranch:

Military Career: E.F. Beale was born in 1822 and had a distinguished military career. He served as a lieutenant in the U.S. Navy and later became Superintendent of Indian Affairs in California and Nevada.
Surveyor and Explorer: In the 1850s, Beale was appointed by the U.S. government to survey and explore a wagon road along the 35th parallel from Fort Defiance in Arizona to the Colorado River. This expedition, known as the Beale Wagon Road, aimed to improve transportation and communication between the East and the newly acquired territories in the West.
Tejon Ranch and the Wagon Road: The Beale Wagon Road passed through the Tejon Ranch, linking Fort Tejon to the Colorado River. Beale recognized the strategic importance of the Tejon Pass for transportation routes and recommended it as a route for the railroad.
Land Acquisition: In 1861, Beale purchased the Rancho El Tejon, which included the Tejon Ranch. He acquired the property from the prominent rancher General Edward Beale Tracy. E.F. Beale engaged in various agricultural and ranching activities on the land.
Conservation and Agriculture: Beale was not only interested in ranching but also in conservation. He introduced various agricultural improvements to the ranch, including cultivating wheat and vineyards. Beale also advocated for land conservation and recognized the need to protect natural resources.
Tejon Ranch Company: In the early 20th century, the Tejon Ranch changed ownership and management. The Tejon Ranch Company was established in 1936, and E.F. Beale’s descendants were involved in the company’s operations.
Legacy: E.F. Beale’s legacy is intertwined with the history of the Tejon Ranch. His contributions to the development of transportation routes, his role in the acquisition of the ranch, and his efforts in both ranching and conservation have left a lasting impact on the region.

Today, the Tejon Ranch remains a significant property in California, known for its historical, cultural, and environmental importance. The Tejon Ranch Company continues to manage the property, balancing agricultural activities with conservation initiatives and partnerships to preserve large portions of the land as open space.

A Yucca Moth and its Yucca

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The relationship between a yucca moth and a yucca plant is a classic example of mutualism, a symbiotic relationship where both species benefit. Yucca moths and yucca plants have coevolved over millions of years, and their interaction is highly specialized.

Pollination:
- Yucca Moths: Female yucca moths play a crucial role in pollination. They are equipped with specialized mouthparts called maxillae, which they use to collect and carry pollen. The female moth visits the flowers of the yucca plant to lay her eggs.
- Yucca Plants: Yucca plants rely on yucca moths for pollination. The female moth collects pollen from one yucca flower and then deposits it on the stigma of another flower while laying her eggs. This ensures cross-pollination, facilitating genetic diversity in the yucca plant population.
Egg-Laying and Larval Development:
- Yucca Moths: The female moth deposits her eggs inside the ovaries of the yucca flowers. She uses specialized structures called ovipositors, which also transfer the pollen. The eggs hatch into larvae.
- Yucca Plants: The yucca plant provides a place for the yucca moth to lay eggs, and the developing larvae feed on some of the developing seeds within the yucca fruit. The yucca plant sacrifices a small portion of its seeds to nourish the larvae.
Specificity and Coevolution:
- The relationship between yucca moths and yucca plants is highly specific. Each species of yucca plant is typically associated with a specific species of yucca moth.
- This specificity has arisen through coevolution, where the traits of each species have adapted to complement the other. Yucca moths have evolved to be efficient pollinators of yucca plants, while yucca plants have developed features that attract and support yucca moths.
Obligate Mutualism:
- The relationship is often considered an obligate mutualism, meaning each species depends on the other for reproduction. Yucca moths rely on yucca plants for a place to lay their eggs, and yucca plants rely on yucca moths for effective pollination.

This intricate relationship between yucca moths and yucca plants highlights the fascinating ways organisms can evolve together, developing mutual dependencies crucial for their survival and reproduction.

Saline Valley Salt Tram

/saline-valley/salt-tram/

The Saline Valley Salt Tram, also known as the Saline Valley Tramway, is a historic tramway system used to transport salt from the Saline Valley in California, USA. The Saline Valley is located within the Death Valley National Park.

The tramway was constructed in the early 20th century to facilitate the transportation of salt from the salt flats in the Saline Valley to the Owens Valley. The system consisted of cables and tramcars that carried salt over the Inyo Mountains. The salt was then transported to market via the Owens Valley.

The operation of the Saline Valley Salt Tram ceased in the mid-20th century, and the tramway itself has since fallen into disuse and disrepair. The remnants of the tramway, including some of the infrastructure and cables, can still be found in the Saline Valley. The area attracts historians, hikers, and those interested in exploring the remnants of historical infrastructure.

Ghost Towns & Sites in the Mojave Desert

/ghost-towns/

The Mojave Desert in the southwestern United States is home to several ghost towns and abandoned sites that reflect the region’s history of mining, ranching, and other activities.

Here are some notable examples:

Calico Ghost Town:
- Located near Barstow, California, Calico is one of the most famous ghost towns in the Mojave Desert. It was a silver mining town in the 1880s and 1890s. Today, Calico is a county park and tourist attraction with preserved buildings and mining equipment.
Rhyolite:
- Near Death Valley in Nevada, Rhyolite was a bustling gold mining town in the early 20th century. It had a population of several thousand people at its peak. The town had schools, banks, and even an opera house. However, it declined rapidly, and now visitors can explore the ruins of its former glory.
Ballarat:
- In California near the Panamint Mountains, Ballarat was a supply town for the nearby mines in the early 20th century. It is known for its association with the infamous outlaw Charles Manson, who briefly stayed in the area.
Bodie:
- Although technically not in the Mojave Desert (in the Eastern Sierra region), Bodie is worth mentioning. This well-preserved ghost town was a gold mining boomtown in the late 19th century. It’s now a state park; visitors can explore the abandoned buildings and artifacts.
Panamint City:
- Nestled in the Panamint Range of California, Panamint City was a silver mining town that thrived in the late 19th century. The town’s remote location contributed to its decline and was abandoned by the early 20th century. The site is accessible by hiking, and some structures remain.
Cima:
- Cima is a small ghost town in the Mojave National Preserve in California. It was a mining and railroad town in the early 20th century. While most of the buildings are gone, the area still has some remnants of its past.
Ivanpah:
- Ivanpah, located in California, was a mining town that saw activity in the late 19th and early 20th centuries. Today, only a few structures remain, including stamp mill ruins.

Building in Cima ghost town in Mojave Preserve — Cima Ghost Town

Exploring these ghost towns and abandoned sites provides a fascinating glimpse into the history of the Mojave Desert and the people who once inhabited these remote areas. Keep in mind that some of these sites may be on private land or protected areas, so it’s essential to respect any restrictions and regulations in place.

Peggy Sue’s 50s Diner

/yermo-ca/

Peggy Sue's Diner, Yermo, Route 66, nostalgia, 1950s

Peggy Sue’s 50s Diner is a well-known retro-themed diner in Yermo, California. It’s designed to resemble a classic 1950s diner, with vintage decor, neon lights, and a nostalgic atmosphere.

The diner typically offers classic American diner fare, such as burgers, shakes, fries, and other comfort food items. Additionally, Peggy Sue’s may have themed events or activities to enhance the 1950s experience for visitors.

Mojave Desert Experiences

The Mojave Desert, located in the southwestern United States, is a vast and captivating landscape known for its unique geological features and diverse ecosystems. Here are some activities you can enjoy in the Mojave Desert:

Joshua Tree National Park:
- Hiking: Explore the numerous hiking trails, such as the popular trails to Hidden Valley, Barker Dam, and Ryan Mo u ntain.
- Rock Climbing: Joshua Tree is renowned for its granite rock formations, making it a world-class destination for rock climbers of all skill levels.
- Stargazing: The park is a designated International Dark Sky Park, offering excellent stargazing opportunities.
Mojave National Preserve:
- Kelso Dunes: Hike to the top of these iconic dunes for panoramic views of the desert landscape.
- Hole-in-the-Wall: Explore the unique volcanic rock formations and hike through the scenic canyons of Hole-in-the-Wall.
Off-Highway:
- Mojave Road: Embark on the historic Mojave Road, a 140-mile trail that takes you through the heart of the Mojave Desert. It’s a popular route for off-road enthusiasts.
Red Rock Canyon State Park:
- Scenic Drive: Enjoy a scenic drive through the park, with opportunities for short hikes to view the striking red rock formations.
- Wildflower Viewing: The park comes alive in the spring with vibrant wildflowers, offering a colorful display.
Death Valley National Park:
- Badwater Basin: Visit the lowest point in North America and explore the unique salt flats.
- Artist’s Palette: Drive through this colorful area known for its mineral-stained hills.
- Zabriskie Point: Enjoy panoramic views of the badlands and eroded rock formations.
Ghost Towns:
- Calico Ghost Town: Explore this well-preserved ghost town that was once a bustling silver mining community.
- Randsburg: Visit another historic mining town known for its quirky atmosphere and vintage charm.
Mojave Air and Space Port:
- Aerospace Museum: Discover the history of aviation and space exploration at the Mojave Air and Space Port, home to innovative aerospace projects.
Bird Watching:
- The Mojave Desert is home to a variety of bird species. Bring binoculars and explore areas like the Amargosa River and nearby wetlands for birdwatching opportunities.
Photography:
- Capture the unique landscapes, rock formations, and vibrant sunsets the Mojave Desert offers. Joshua Tree’s unique Joshua trees and the play of light and shadow make for excellent photographic opportunities.
Camping:
- Enjoy camping under the desert stars at designated campgrounds in Joshua Tree National Park, Mojave National Preserve, and Death Valley National Park.

Remember to check weather conditions, carry plenty of water, and follow Leave No Trace principles when exploring the Mojave Desert. Always be aware of the desert’s extreme temperatures and take necessary precautions for a safe and enjoyable experience.

Desert Rockhounding

Desert rockhounding is a popular recreational activity that involves searching for, collecting, and identifying rocks, minerals, gemstones, and fossils in arid regions. Deserts often have unique geological formations and a diverse range of minerals, making them interesting and rewarding for rockhounding enthusiasts. Here are some tips for desert rockhounding:

Research the Area: Before heading out, research the desert area you plan to explore. Learn about the geology, rock formations, and the types of minerals or gemstones commonly found in that region. Geological maps and online resources can be valuable tools.
Check Regulations: Be aware of any regulations or restrictions in the area you plan to visit. Some areas may have rules about collecting rocks, and respecting these regulations is important to preserve the environment.
Safety First: Deserts can be challenging environments with extreme temperatures. Wear appropriate clothing, including a hat, sunscreen, and sturdy footwear. Carry plenty of water and be mindful of your surroundings to ensure a safe and enjoyable rockhounding experience.
Use the Right Tools: Bring the necessary rock-hounding tools, such as rock hammers, chisels, safety glasses, gloves, and a backpack to carry your finds. A field guide to rocks and minerals can help you identify your discoveries.
Explore Washes and Dry Creek Beds: Water action in desert washes can concentrate rocks and minerals, making these areas fruitful for rockhounding. Explore dry creek beds, washes, and areas where water has flowed in the past.
Look for Indicator Minerals: Certain minerals may indicate the presence of valuable gemstones or other interesting specimens. Learn to recognize indicator minerals and follow their trail to potential collecting sites.
Be Respectful: Leave no trace and practice ethical rockhounding. Avoid damaging plants, disturb the environment as little as possible, and fill in any holes you may dig. Remember that some areas may be protected, and it’s important to respect these conservation efforts.
Join Rockhounding Clubs: Consider joining local rockhounding clubs or groups. These organizations often have experienced members who can share knowledge about the best collecting sites and provide guidance on responsible rockhounding practices.
Time Your Visit: The best time for desert rockhounding is during the cooler months, as summer temperatures can be extremely high. Early morning and late afternoon are generally more comfortable and offer better lighting for observing and collecting.
Learn to Identify Rocks: Familiarize yourself with the characteristics of rocks and minerals commonly found in the desert. Understanding the properties, colors, and formations of different specimens will enhance your rockhounding experience.

Always be aware of your impact on the environment and prioritize conservation while enjoying the excitement of discovering rocks and minerals in the desert.

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