Coyote (Canis latrans)

The Coyote (Canis latrans), commonly known as the prairie wolf, brush wolf, or American jackal, is a highly adaptable medium-sized canid native to North America.

Coyote (Canis latrans) enduring a snow storm in Joshua Tree National Park - Photo by James L Rathbun
Coyote (Canis latrans) enduring a snow storm in Joshua Tree National Park – Photo by James L Rathbun

The binomial name Canis latrans translates to “barking dog,” reflecting its vocal nature. It belongs to the genus Canis, which includes wolves, dogs, and jackals. Approximately 19 subspecies are recognized, with variations in size and coloration across regions (e.g., larger northeastern forms often show some historical hybridization with wolves).

Classification

Kingdom:Animalia
Phylum:Chordata
Class:Mammalia
Order:Carnivora
Family:Canidae
Genus:Canis
Species:C. latrans

Physical Description

Coyotes are smaller and more lightly built than gray wolves (Canis lupus), but larger than most foxes. Adults typically stand about 60 cm (24 inches) at the shoulder, measure 1–1.3 meters (3.3–4.3 feet) in total length (including a 30–40 cm bushy tail), and weigh 9–23 kg (20–50 pounds), with eastern populations often heavier.

The fur is long and coarse, usually grizzled buff, grayish-brown, or yellowish-gray on the upper parts, with whitish underparts, reddish tones on the legs, and a black-tipped tail. There is considerable variation; some individuals appear silver-gray or nearly black (melanistic forms are rare). Coyotes have pointed, erect ears, a slender muzzle, and a drooping bushy tail when running. They resemble a lean German Shepherd or collie but are distinguished by their narrower build and pointed features.

Behavior

Coyotes are highly intelligent, opportunistic, and adaptable. They are primarily nocturnal or crepuscular (active at dawn and dusk), though daytime activity occurs where undisturbed. They can reach speeds up to 65 km/h (40 mph) and jump distances of 4 meters.

Social organization varies: many live solitarily or in pairs, while others form small family groups (often a mated pair and pups). They maintain territories, especially during denning season. Coyotes are famous for their vocalizations, including yips, barks, howls, and “serenades” at night for communication, territory defense, or coordination.

As efficient hunters and omnivores, they primarily prey on small mammals (e.g., rodents, rabbits, hares), but also take larger prey like white-tailed deer (especially in winter or packs), birds, insects, and carrion. They readily consume fruits, berries, and vegetation when animal prey is scarce. Hunting often occurs alone or in pairs, though packs form seasonally for larger prey. Keen senses of smell, hearing, and vision aid in locating food.

Range and Distribution

Historically centered in the western Great Plains and arid regions of North America, coyotes have dramatically expanded since the early 20th century. Today, they occupy a vast range from northern Alaska and most of Canada southward through the United States, Mexico, and into Central America (at least to Panama and parts of Costa Rica). They are found coast-to-coast in the U.S. and Canada, absent only from the northernmost tundra and some extreme southern peninsulas.

This expansion includes forests, urban areas, agricultural lands, deserts, and riparian zones, making the coyote one of the most widespread carnivores in the Americas. Highest densities occur in the Great Plains and south-central U.S. The species is classified as Least Concern by the IUCN due to its adaptability and stable/increasing populations.

The coyote’s success stems from its behavioral flexibility, omnivorous diet, and ability to thrive alongside human activity, making it a classic example of ecological resilience in modern landscapes.

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

Goodsprings, Nevada

Goodsprings is an unincorporated community and census-designated place (CDP) in Clark County, southern Nevada, located in Goodsprings Valley at the southeastern foothills of the Spring Mountains. Situated along Nevada State Route 161, about five miles northeast of Jean and Interstate 15 (roughly 30-45 minutes southwest of Las Vegas), it sits at an elevation of 3,717 feet in an arid desert environment. Once the heart of one of Clark County’s most productive mining districts, Goodsprings thrived as a boomtown in the early 20th century before declining into a small, semi-preserved settlement often described as a “living ghost town.” As of the 2020 census, its population was 162.

Goodsprings, Nevada - 1924
Goodsprings, Nevada – 1924

Pre-History and Early Settlement (Pre-1900)

The area around Goodsprings has long been a rare water source in the Mojave Desert. Indigenous peoples, including the Ancient Puebloans and later the Paiute, used the natural springs seasonally. White settlers first documented the springs in 1830 along the Old Spanish Trail.

Mining in the broader region began in 1856 when Mormon miners established a lead operation at nearby Potosi Mountain—possibly Nevada’s oldest underground lode mine. Gold was discovered in the area in 1893. In the 1860s, cattleman Joseph Good discovered silver near the springs (sometimes dated to 1861 or 1868) and established a small store while using the water for his herd. The settlement was initially called “Good’s Springs” or “Goods Springs” in his honor. By 1868, additional silver and lead deposits attracted more prospectors, forming a rudimentary mining camp. The Yellow Pine Mining District (also known as the Goodsprings Mining District) was formally organized around 1882 following further gold discoveries.

Before 1900, the area consisted mainly of tent cabins and a small mill. A post office opened in 1899 (initially at the nearby Keystone Mine, later relocated), and Lincoln County established Goodsprings Township. In 1904, Salt Lake City mining interests platted the township. Early structures were limited until transportation improved.

An old water tower located inside Goodspings, Nevada
An old water tower located inside Goodspings, Nevada

The Mining Boom and Peak Prosperity (1900s–1920s)

The arrival of railroads transformed Goodsprings. The San Pedro, Los Angeles & Salt Lake Railroad (later Union Pacific) reached nearby Jean in 1905. In 1911, the narrow-gauge Yellow Pine Railroad connected the mines to Jean, drastically reducing ore transport costs and spurring construction of permanent buildings. The Yellow Pine Mining Company consolidated claims in 1909, operating a mill and focusing on oxidized zinc, lead, silver, copper, and gold.

World War I dramatically boosted the economy, as demand for lead (for ammunition) and zinc surged. By 1916–1918, the population peaked at around 800 (some accounts cite up to 1,000), supporting a developed downtown with a hospital, luxury hotel, post office, weekly newspaper (Goodsprings Gazette, 1918–1921), stores, churches, and multiple saloons. The district became Clark County’s most productive, yielding a total of approximately $25 million in minerals—primarily lead and zinc, with lesser amounts of gold, silver, copper, and rarer elements like molybdenum, vanadium, nickel, cobalt, platinum, palladium, and uranium. It represented the greatest variety of minerals in Nevada.

Key Infrastructure and Landmarks Built During the Boom

1916: The 20-room Fayle Hotel (considered one of Nevada’s finest at the time, with modern amenities; destroyed by fire in 1966).

1913: The Pioneer Saloon (built by Clark County Commissioner George Fayle using prefabricated stamped-tin construction), General Store, and Community Church. The saloon, Nevada’s oldest continuously operating bar in southern Nevada, featured an original cherry-wood bar and quickly became the social hub.

1913: Goodsprings Schoolhouse (the oldest school in Clark County built specifically as a school; still in use today and listed on the National Register of Historic Places).

The Pioneer Saloon located in Goodsprings, Nevada is still open and quite busy
The Pioneer Saloon located in Goodsprings, Nevada is still open and quite busy

Notable events include a 1915 saloon shooting during a card game (miner Paul Coski killed by Joe Armstrong; ruled self-defense, with bullet holes still visible) and the 1942 plane crash of actress Carole Lombard on nearby Mount Potosi. Her husband, Clark Gable, waited at the Fayle Hotel and Pioneer Saloon for news of the tragedy; a memorial to the victims remains in the saloon today.

Decline and Transition (1920s–1950s)

Post-World War I, falling metal prices led to mine closures and population decline (down to about 400 by 1920). The Yellow Pine Railroad ceased operations around 1930 (tracks removed by the mid-1930s). A brief resurgence occurred during World War II due to renewed demand, but mining largely ended by the 1950s. The town contracted but never fully vanished, unlike many desert boomtowns. Fires destroyed several structures, and atomic testing occurred in the region during the 1950s. By the late 20th century, fewer than 100–200 residents remained, living among preserved and restored buildings, mobile homes, and newer structures.

Modern Era and Preservation (1960s–Present)

Goodsprings endures as a quiet desert community with a focus on historic preservation. The Goodsprings Historical Society (established in the 1990s) works to educate the public, restore buildings (e.g., roof repairs), and maintain sites like the 1886 Campbell Stone Cabin (one of the oldest structures), the cemetery, and mill ruins. The Pioneer Saloon continues operating as a tourist draw, hosting events, filming locations (The Misfits, Fear and Loathing in Las Vegas), and even inspiring a recreation in the 2010 video game Fallout: New Vegas (which has boosted visitation through annual festivals since 2022).

In 2010, the Goodsprings Waste Heat Recovery Station (a 7.5 MW geothermal-style plant using pipeline waste heat) opened as Nevada’s first renewable energy facility of its kind. The town remains accessible for day trips from Las Vegas, with the saloon, schoolhouse, and surrounding desert landscape attracting history enthusiasts and off-roaders.

Conclusion

Goodsprings exemplifies the classic Nevada mining town arc: from obscure springs and prospector camps to wartime prosperity and eventual contraction, while retaining its historic character. Its $25+ million in mineral wealth, pioneering infrastructure, and resilient landmarks like the Pioneer Saloon underscore its significance in Clark County’s development. Today, it stands not as a fully abandoned ghost town but as a preserved chapter of the American West—tied to Indigenous heritage, railroad expansion, world wars, Hollywood tragedy, and modern tourism—offering a tangible link to Nevada’s rugged past amid the Mojave Desert.

Goodsprings Mines

  • Alice Mine
  • Argentina Mine
  • Belle Mine
  • Columbia Mine
  • Cosmopolitan Mine
  • Fredrickson Mine
  • Green Copper Mine
  • Hermosa Mine
  • Hoosier Mine
  • Iron gold Mine
  • Lookout Mine
  • Keystone Mine
  • Lavina Mine
  • Middlesex Mine
  • Surprise Mine
  • Table Top Mine
  • Yellow Pine
The mill site located just outside of Goodsprings, Nevada
The mill site located just outside of Goodsprings, Nevada

Goodsprings Nevada Trailmap

Titus Canyon

Titus Canyon has it all, rugged mountains, colorful rock formations, a small ghost town, mines, petroglyphs, wildlife, rare plants and spectacular canyon narrows as a grand finale! Titus Canyon is the most popular back-country road in Death Valley National Park and just plain fun to run.  The canyon is easily accessible from Stovepipe wells and Furnace Creek.

Titus Canyon, a narrow canyon drive in Death Valley National Park, CA
Titus Canyon, a narrow canyon drive in Death Valley National Park, CA

Although the Grapevine Mountains were uplifted relatively recently, most of the rocks that make up the range are over half a billion years old. The gray rocks lining the walls of the western end of the Canyon are Cambrian limestone. These ancient Paleozoic rocks formed at a time when the Death Valley area was submerged beneath tropical seas. By the end of the Precambrian, the continental edge of North America had been planed off by erosion to a gently rounded surface of low relief. The rise and fall of the Cambrian seas periodically shifted the shoreline eastward, flooding the continent, then regressed westward, exposing the limestone layers to erosion. The sediments have since been upturned, up folded (forming anticlines), down folded (forming synclines) and folded back onto themselves (forming recumbent folds).

Leadfield Gost Town, Death Valley, California
Leadfield Gost Town, Death Valley, California

Although some of the limestone exposed in the walls of the canyon originated from thick mats of algae (stromatolites) that thrived in the warm, shallow Death Valley seas, most of the gray limestone shows little structure. Thousands of feet (hundreds of meters) of this limey goo were deposited in the Death Valley region. Similar limestone layers may be seen at Lake Mead National Recreation Area and at the bottom of the Grand Canyon.
At one of the bends in the canyon, megabreccia can be seen.

Leadfield was an unincorporated community, and historic mining town found in Titus Canyon in Death Valley National Park.

Titus Canyon Trail Map

Elizalde Cement Plant

The Elizalde Cement Plamt as seen from US 95 south to Beatty, NV
The Elizalde Cement Plamt as seen from US 95 south to Beatty, NV

While travelling north on Highway 95 from Las Vegas to Beaty, I spotted the Elizalde Cement plant from the road. We did not stop on that first passing as I was headed out to Race Track Valley, in Death Valley, CA. However, the memory of this missed destination occupied my mind for the duration of our camping trip.

A couple of quick trips across the “Interwebs” and I had misidentified the ruins I had seen as the remains of the Nevada ghost town of Carrara. Happily, I researched the “marble quarry” town of Carrara. A few months later we stopped at the location and open closer inspection, it didn’t feel “right”. Ghost Towns typically were built as tent cities and have few foundations. This site had a concrete walls, and was not laid out like a city.

Elizade Cement Plant, near Carrara, NV in Nye County
Elizade Cement Plant, near Carrara, NV in Nye County

Elizalde Cement Plant

Further research and I have found my error. The ruins I had found were of the Elizadle Cemet Plant. The Elizaldo Cement Plant was built in the early 1940’s by the Carrara Portland Cement Company. The nearby Carrara quarries were used to produce crushed marble, which was used in the white cements produced by the plant. Forty five men poured foundations for the plant between April 1941 and July of the same year.

The plant was named for Angel M. Elizalde, who was the President of Elizalde & Co. Ltd and a principal investor of the Cararra Portland Cement Co. Plans were already under-weigh to build a large advanced cement plant when Mr. Elizalde was elected President.

A large “fiesta” was scheduled for the opening on the plant in August, 1941. However, before a single pound of concrete is produced, a fire engulfed the site and the plant was badly burned. The fire claimed the machine shop, field office, blacksmith shop. This set back stopped construction at the site while the company searched for capital and replacement equipment.

Despite plans made for expanded production levels and reinvestment in the plant site, the start of World War 2 and increase in fuel costs doomed the plant. Today, a lot of concrete foundations lie in testimony to the unseen victims of World War 2. The plant is fenced off to curtail access, however, it has fallen prey to those with spray paint cans.

Now, I need to go back and find Carrara and its marble quarry! oh darn….

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