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Black Diamond Mines Regional Preserve

The Black Diamond Mines Regional Preserve is a 6,000-acre (2,400 ha) park located north of Mount Diablo in Contra Costa County, California under the administration of the East Bay Regional Park District (EBRPD). The district acquired the property in 1973. The preserve contains relics of 3 mining towns, former coal and sand mines, and offers guided tours of a former sand mine. The 60 miles (97 km) of trails in the Preserve cross rolling foothill terrain covered with grassland, California oak woodland, California mixed evergreen forest, and chaparral.

History
Indigenous history Long before the widespread ranching and mining activity that took place in the area, indigenous people had a presence in the Bay Area for 13,000 years. Three Bay Miwok tribes, the Chupcan, Ompin, and Volvon, lived in the areas surrounding the Black Diamond Mines Regional Preserve. The Chupcan occupied territory to the west of the preserve near Concord, the Volvon occupied the territory to the south including much of Mount Diablo, and the Ompin occupied the area to the north including Pittsburg, Collinsville, and the intervening waterway. Black Diamond Mines Regional Preserve is located in a boundary area between these three tribes. At the beginning of the 19th century, these three tribes were significantly impacted by the Spanish mission system. Between 1804 and 1806, the majority of Volvon Bay Miwok were split up and baptized at either Mission Dolores or Mission San Jose. A Spanish military raid caused the Chupcans to flee to Suisun territory in 1804, and by 1811, most Chupcans were split up and baptized at either Mission Dolores or Mission San Jose. His initial attempt to mine the coal was not financially successful but soon other coal deposits were discovered nearby and mining operations grew rapidly. The area became known as the Mount Diablo Coalfield, producing more than 4 million tons of coal during this time. The area includes the remains of twelve coal mines and the sites of several long-gone coal mining towns. The Preserve contains over of mine workings. The largest and oldest town, Nortonville, had a peak population of about 1,000. Somersville, Stewartville, West Hartley and Judsonville were located in valleys to the east. The sites of Judsonville and West Hartley are located on private property outside the eastern boundary of the Preserve. The mines were the Empire, Central, Star, Corcoran, Pittsburg, Manhattan, Eureka, Independent, Union, Black Diamond, Mt. Hope, and Cumberland. The coal produced was of a low grade (sub-bituminous or lignite), but for a time in the 19th century, was the only readily accessible and economic source in California. Therefore, it was a very valuable resource and powering the railroads, ships and heavy industry of California. The mineral was often called 'black diamond." The coal was carried to the San Joaquin River by three railroads: the Empire, Pittsburg, and Black Diamond, for shipment by barge to markets in San Francisco, Sacramento, Stockton and other communities. Coal mining activity ended as better-quality imported coal became affordable and as petroleum emerged as an energy source. Park staff have maintained a public-access opening into a former coal mine known as Prospect Tunnel. Visitors can explore the first of this approximately 400-foot tunnel. Rose Hill Cemetery Rose Hill Cemetery, officially designated as a Protestant cemetery, the final resting place for over 200 residents of the coalfield, is located on a hillside between the Somersville and Nortonville townsites. After the mines closed and the nearby towns were abandoned, the cemetery fell into disuse. Many of the gravestones were stolen or destroyed by vandals, or damaged by cattle using them as scratching posts. In 1960, Ansel Adams photographed two Italian Cypress trees in the cemetery, and called the image, "Poplars, Cemetery near Mount Diablo". Those buried in the cemetery include coal miners who were killed as a result of their work in the mines. However, the majority of the buried are children from the nearby towns of Nortonville and Somersville who died of diseases such as smallpox, scarlet fever, diphtheria, and typhoid. The land the cemetery occupies was originally owned by the Black Diamond Coal Mining Company president and chief stockholder Alvinza Hayward, who left it to his daughter Emma Rose upon his death. In the 1940s she deeded the land to Contra Costa County. It was transferred to the East Bay Regional Park District in September 1973. Since that time park staff has undertaken restoration of the cemetery, including stabilizing eroded soil, repairing and reinstalling gravestones, and marking burial sites missing gravestones with brass plaques. A few whose earthly remains were laid to rest here include: • William Gething, age 36, who was killed with 10 other men in an 1876 mine explosion; 7 other men who died in the same accident are buried nearby. The citizens of Nortonville raised $300 to erect a white bronze monument to these men, located in the cemetery. The monument was stolen or destroyed sometime after the 1930s. Inside the Greathouse portal, a -long section of the entrance corridor has been made into a museum. The first section is a series of self-guided exhibits, while the larger second section (which has a separate entrance from the outside), houses a reconstruction of the Hazel-Atlas works as it would have appeared around 1940. Park staff originally repurposed the Hazel-Atlas mine as a museum in the 1970s, but storm damage in 2007 forced closure of this attraction for extensive repairs. It did not reopen for five years. == Geology ==
Geology
The rich coal deposits and sandstone hills of Black Diamond Mines Regional Preserve were formed by geological activity in the Tertiary period. In the period between the Paleocene epoch and Miocene epoch of the Tertiary era, the North American Plate and the Pacific plate came together at a subduction zone where the North American Plate was pushed over the Pacific Plate. During this era, the Pacific Ocean stretched over much of the California central valley with the coastline reaching the lower regions of the Sierra Nevada mountains. The coal that was mined from the Mount Diablo Coal Field was formed during the third marine sediment deposition cycle which took place during the middle of the Eocene epoch. At the beginning of this third cycle, tectonic activity caused an uplift of the continental shelf seafloor, resulting in the creation of shallow marshes. Erosion during this era brought an abundance of sediment into the shallow sea covering the continental shelf, with some sediment making its way into the marshlands. These sediments, along with the favorable hot and humid climate, fueled the growth of coastal marsh flora that eventually formed into coal. Tectonic activity towards the end of this sedimentation cycle caused the continental shelf to sink and resulted in sediments being deposited into deeper water. The Mount Diablo Mountain Range of today was created at the beginning of the fourth depositional cycle when the continental shelf began to rise up once again. ==Recreation==
Recreation
The trails offer views of Mount Diablo, the Sacramento-San Joaquin River Delta, and on clear days, the Sierra Nevada. The Preserve usually has an impressive variety of wildflowers in spring including the rare Mount Diablo fairy lantern (Calochortus pulchellus), Mount Diablo sunflower (Helianthella castanea), and Brewer's dwarf flax (Hesperolinon breweri). It is home to a variety of wildlife including deer, mountain lions, coyotes, foxes, bobcats, golden eagles, and a variety of hawks. The endangered San Joaquin kit fox (Vulpes macrotis mutica) and threatened California red-legged frog (Rana draytonii), California tiger salamander (Ambystoma californiense) and Alameda whipsnake (Masticophis lateralis) are present as well. The park is open year-round for hiking, mountain biking, and horseback riding from 8 am to dusk. A backpack camp and a group camp can be reserved for overnight stays. There have been many reports of a ghost in the park. ==2016 land donation==
2016 land donation
East Bay Regional Park District accepted the donation of by Antioch Holdings LLC on December 20, 2016. The property had been deeded to the holding company by Gordon Grevelle, president of Suncrest Homes, who had originally planned to build a gated residential community there when he had bought the tract in 1987. After going through an extensive permitting process and a decline in the California housing market, Grevelle decided that the project he had envisioned would be unlikely to meet his financial goals. Since the tract was already surrounded by park land, he chose to make the land available to East Bay Regional Park District, which announced its intention to add the land to the Black Diamond Mines Regional Preserve. Grevelle estimated the market value of his donation at $3.5 million in 2016 (~$ in ). ==Notes==
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