Silver Star Mine

The Silver Star Mine is a small mine site located off of the Zinc Mountain Road in San Bernardino County, California. The site rests at 4931 feet above sea level in the Ivanpah montains. The lonely site features a small humble cabin the miners used to survive and beat the heat. There is also a wrecked automobile near at the site, which has long since given up the battle against rust.

Silver Star Mine Cabin
Silver Star Mine Cabin

There is not much information available for this location on the Internet and hopefully I will be able to find some eventually. The mine site is also know as the Lucky Lode deposits. The route into the area is reasonably passable and should be suitable for most cars, provided the driver is used to operating on the back roads of the desert.

Silver Star Mine
Silver Star Mine rusted out auto

Some places claim that this mine produced lead, copper and zinc. The fact that this mine is found just off of Zinc Mountain Road offers some credence to a zinc mine. Other online sources claim this is a tungsten mine. A shallow mine shaft is located near the cabin. The shaft contains an old wooden ladder used by the miners and appears to be filled in, collapsed, or suspended after about 20 feet of workings.

Silver Star Mine Shaft
Silver Star Mine Shaft with ladder.

This stark hole in the ground reminds us what a challenges the life of a miner must endure. Hot, dry deserts, narrow, dark tunnels in a hostile landscape.

Silver Star Mine Trail Map

Resources

Coyote Melon (Cucurbita palmata)

Coyote Melon (Cucurbita palmata)
Coyote Melon (Cucurbita palmata)

Coyote Melon (Cucurbita palmata), also known as Coyote Gourd, is a flowering plant common in the desert southwest and known to produce spherical yellow – green melons. The vine like plant is commonly found is loose, sandy or gravely, dry, well drained soil which is common in Southern California, Arizona, Nevada and exclusively in Washington County, Utah. The primary characteristic is the growth of a green melon or gourd which is quite startling when you first see them in the hot desert climates.

Sereno Watson (December 1, 1826 in East Windsor Hill, Connecticut - March 9, 1892 in Cambridge, Massachusetts) was an American botanist
Sereno Watson (December 1, 1826 in East Windsor Hill, Connecticut – March 9, 1892 in Cambridge, Massachusetts) was an American botanist

The gourd was first described in 1876 by Sereno Waston who was a Yale graduate with a degree in Biology, The Coyote Melon features a sprawling stiff vine with rough, stiff-haired stems and leaves. Cucurbita palmata produces a large yellow bell shaped flower, while the melon itself is smooth in appearance. The striped yellow – green colored gourd is known to be quite hard, however, also thin when mature. The melons are very bitter and not edible. This hearty planet can survive the harsh desert landscape through its use of a large and hearty tap root. This root system can extend several feet into the dry soil to supply the plant with nutrients and water required for survival.

The Coyote Melon (Cucurbita palmata) is extremely fibrous and although not edible to humans is known to be on the coyotes diet during the fall, hence its name. It is quite common to find the seeds of this plant in coytoe scat during the fall months.

Despite the fibrous melon being inedible by man, the native american tribes were known to consume the ground seeds of this plant. Additionally, they used the dried gourds as rattles in various dances and other ceremonies. They also utilized the plant was as soap for cleaning.

Resources

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 on the west side.  Some sections are rough and sandy; 4 x 4 recommended. Roads can become slick, muddy and impassable after rains. Be sure to inquire about road conditions, especially if you plan to cross Soda Dry Lake.

The railroad monument along the Old Mojave Road in the Mojave National Preserve.
The railroad monument along the Old Mojave Road in the Mojave National Preserve.

The Mojave Road is party of the Old Spanish Trail, which is a 700 mile long historical trade route that connected the northern New Mexico settlements near Santa Fe, New Mexico with those of Los Angeles, California. The Old Spanish trail’s rugged terrain discouraged the use of wagons. It was always a pack route, mainly used by men and mules. Used by Indians to transport goods from the southwest to trade with the Chumash and other coastal tribes, this route later served the cause of westward expansion. Military forts were established along the route to protect key water sources and provide assistance for travelers.

The route at one time was for all intents and purposes lost until Dennis Casebier and Friends researched the route and reestablished the trail as if it know today and is a popular four-wheel drive road.

The eastern section of the Old Mojave Road leaves US 95 in Nevada near Laughlin moving westward.  The eastern section climbs up to Fort Piute and continues past an old corral one a rocky climb.  Once up on the plateau, the road continues to travel west to Nipton Road.

Bert Smith's Cabin located in the Mojave National Reserve
Bert Smith’s Cabin located in the Mojave National Reserve

The central section starts at Nipton Road and continues west to Kelbaker road near Baker, CA.  The road starts rather narrow with high brush offering the opportunity for some new desert pin-striping.

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

A short declination which offers the only real obstacle near Rock Spring.  Burt Smiths cabin and the Government Holes water offer short hikes and distractions from the trail.  Once you cross the Kelso Cima Road, about 5 miles of  “whoop de doos” will rock you to sleep.  The center section offers the most to see, and if you choose one section, this would be it in our opinion.

The western section leaves Kelbaker road and continues west into the dry soda lake south of Baker.  The western section of the route can best be described as dry and sandy.  A larger mine complex and Afton Canyon are the major sights.

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

In addition to over 100 miles of 4×4 trail, the Old Mojave road offers access to mines, old homesteads, and other 4×4 routes.  The Old Mojave can be run either way and in a single long day, or in thirds with access being provided from Kelbaker road out of Baker or the Nipton Road in the the East.  However, for the best experience, take your time and run the trail in Multiple days and overnight in one of many primitive or established Campgrounds.

Old Mojave Road Trail Map

Morning Star Mine

Located in the Ivanpah Mountains, the Morning Star Mine is a gold / silver mine located near to California / Nevada border near Mountain Pass. The mining district enjoys amazing views and lots of wild life and wild flowers during the spring of each year, which are easily accessible from a grade dirt road. Numerous lower traffic side trails will allow access of other places to explore.

A remote side road leading a old mine site in the Ivanpah Mountains near the Morning Star Mine.
A remote side road leading a old mine site in the Ivanpah Mountains near the Morning Star Mine.

The location was first worked in 1907 and was known as the Clansman mine. Operations were initially quite small and in 1931 only two miners were on location. In 1937 the owner J. B. Mighton and Brown optioned the property to Richard Malik, who worked the location significantly until 1938.

The Morning Star Mine Cutoff Road.
The Morning Star Mine Cutoff Road.

Erle P. Halliburton worked the mine with ten men, starting in April of 1939. Halliburton known today, as the founder of his name sake company, Halliburton Oil. Mr. Halliburton made his fortune in Duncan Oklahoma where he borrowed a wagon, a team of mules and a pump, he built a wooden mixing box and started an oil well cementing business. The Halliburton efforts at this site where forced closed in 1942 by the War Productions Board order to close gold mining for the war effort.

Erle P Hallibuton 1940 - SMU Central University Libraries @ Flickr CommonsSouthern Methodist University, Central University Libraries, DeGolyer Library
Erle P Hallibuton 1940 – SMU Central University Libraries @ Flickr CommonsSouthern Methodist University, Central University Libraries, DeGolyer Library

Following Halliburton’s death in 1957, the property was acquired by the Vanderbilt Gold Corporation in 1964, where upon the location was drilled and sampled. Fifteen years later, in 1979 the company finally complete a capital raise the in Morning Star mine was again on operation as an underground mine utilizing trackless mining equipment and the ore processed in nearby Vanderbilt, California. Due to the time period, this was probably the Goldome Mill and not within the town of Vanderbilt.

The modern Morning Star Mine site is not much to look at and a locked gate prevents access.
The modern Morning Star Mine site is not much to look at and a locked gate prevents access.

After just three years of operations, mining operations were again halted in 1983, due to the dropping price of Gold, however underground explorations continued with long hole drilling and testing. From 1984 – 1993 saw increased gold and silver production to the amount of about 75,000 tons per month. Water supply problems plagued the operation, however, with the price of gold between $350 and $500 per once the Vanderbilt operation made a return.

A vertical mine shaft is protected by a metal grate.
A vertical mine shaft is protected by a metal grate nearby the Morning Star Mine.

The mine was finally closed in 1993 after the gold prices dropped and several environmental violations and animal deaths caused by cyanide poisoning. With the creation of the Mojave Nation Preserve in 1994 from the California Desert Protection act, the NPS inherited an environmental problem and it slowly continues to clean up the site. At this point, access to the location is blocked with a locked gate. It was noted that several building and a milling foundations remain from this relatively modern mining endeavor.

A horizontal shaft in the Ivanpah Mountains.
A horizontal shaft in the Ivanpah Mountains.

Resources

Black Tailed Jackrabbit ( Lepus californicus )

The Black-tailed Jackrabbit (Lepus californicus), a swift and adaptable lagomorph of the American West, is often mistaken for a rabbit but is technically a hare, known for its enormous ears, powerful hind legs, and distinctive black-tipped tail. This species thrives in open, arid environments, where its speed—reaching up to 40 mph (64 km/h)—and evasive maneuvers make it a master of survival against predators like coyotes and eagles. With a mottled gray-brown coat providing camouflage against dusty landscapes, the black-tailed jackrabbit plays a key role in ecosystems as both prey and herbivore, influencing vegetation dynamics across its range.

Black Tailed Jackrabbit enjoying the shade of a Joshua Tree
Black Tailed Jackrabbit enjoying the shade of a Joshua Tree.

Classification

The Black-tailed Jackrabbit is classified within the kingdom Animalia, phylum Chordata, class Mammalia, order Lagomorpha, family Leporidae, and genus Lepus. Its scientific name, Lepus californicus, reflects its association with California, though its range extends far beyond. It is one of several North American hares, distinguished from true rabbits by its larger size, longer ears, and precocial young (born fully furred and mobile). Subspecies include variations adapted to different regions, such as L. c. californicus in coastal areas and L. c. deserticola in deserts. Fossil records trace its lineage to the Pleistocene, highlighting evolutionary adaptations to open habitats post-Ice Age.

Physical Description

Adult Black-tailed Jackrabbits measure 47–63 cm (18–25 inches) in body length, with ears extending 10–13 cm (4–5 inches), and weigh 1.4–3.6 kg (3–8 lbs), with males typically larger than females. Their fur is grizzled gray-brown on the upper body with white underparts, providing effective camouflage in scrubby terrain. The namesake black tail is white underneath, flashed as a warning signal during flight. Oversized ears, richly vascularized, aid in thermoregulation by dissipating heat, while large eyes positioned on the sides of the head offer nearly 360-degree vision for detecting threats. Long, powerful hind legs enable explosive leaps up to 3 meters (10 feet) high and 6 meters (20 feet) long, complemented by furred soles for traction on varied surfaces. Juveniles resemble adults but are smaller and fluffier at birth.

Behavior

Black-tailed Jackrabbits are primarily crepuscular and nocturnal, active during dawn, dusk, and night to avoid midday heat and predators, though they may forage diurnally in cooler weather. They are solitary except during breeding, maintaining home ranges of 0.1–1 square km (25–250 acres) that overlap with others. When threatened, they rely on speed and zigzag running patterns to evade pursuit, often freezing in place first to blend into surroundings before bolting. They spend much of the day in shallow depressions called “forms,” often under shrubs for shade and cover, emerging to forage. Communication is limited, involving thumping hind feet as alarm signals and scent marking with chin glands. In extreme heat, they pant and use their ears to cool blood; in cold, they huddle to conserve warmth. Populations fluctuate cyclically every 7–10 years, influenced by food availability, disease, and predation.

Food Sources

As herbivores, Black-tailed Jackrabbits have a diet dominated by grasses, forbs, and shrubs, adapting seasonally: green grasses and herbaceous plants in spring and summer, and woody twigs, bark, and dried vegetation in fall and winter. Favorites include alfalfa, clover, sagebrush, and mesquite, with agricultural crops like wheat and lettuce targeted in farmlands, sometimes making them pests. They obtain most water from food, rarely drinking, and can consume up to 1 kg (2.2 lbs) of vegetation daily. Their caecotrophic digestion—re-ingesting soft feces (cecotropes)—allows extraction of additional nutrients like proteins and vitamins from low-quality forage. This adaptation is crucial in nutrient-poor arid environments.

Breeding

Breeding in Black-tailed Jackrabbits is promiscuous and occurs year-round in southern ranges, peaking from December to September in northern areas, triggered by rainfall and food abundance. Females, or does, reach sexual maturity at 7–8 months, males slightly later. Courtship involves chasing and “boxing” displays where pairs rear up and strike with forepaws. Gestation lasts 41–47 days, with litters of 1–8 leverets (average 3–4), born in shallow forms lined with fur. Precocial young are born with open eyes, full fur, and mobility, weaning at 3–4 weeks and independent by 1–2 months. Females can produce 3–4 litters annually, leading to high reproductive rates that offset heavy predation.

Habitat and Range

Black-tailed Jackrabbits inhabit open, arid to semi-arid landscapes including desert scrub, prairies, grasslands, farmlands, dunes, and shrub-steppe, preferring areas with short vegetation and minimal dense understory for easy escape routes. They avoid closed-canopy forests and high elevations above 3,000 meters (9,800 feet). Their range spans the western United States from central Washington eastward to Missouri, southward through the Great Plains and Southwest to Baja California Sur and Zacatecas in Mexico, with introductions in some eastern states. Populations are non-migratory but may shift locally with food availability. Human activities, like agriculture, have expanded suitable habitats, though habitat loss and fragmentation pose threats in some areas.

Classification

Kingdom:Animalia
Phylum:Chordata
Class:Mammalia
Order:Lagomorpha
Family:Leporidae
Genus:Lepus
Species:L. californicus