People v. Guntert

126 Cal. App. Supp. 3d 1, 179 Cal. Rptr. 426, 1981 Cal. App. LEXIS 2475
CourtAppellate Division of the Superior Court of California
DecidedSeptember 18, 1981
DocketCrim. A. No. 59331
StatusPublished
Cited by5 cases

This text of 126 Cal. App. Supp. 3d 1 (People v. Guntert) is published on Counsel Stack Legal Research, covering Appellate Division of the Superior Court of California primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
People v. Guntert, 126 Cal. App. Supp. 3d 1, 179 Cal. Rptr. 426, 1981 Cal. App. LEXIS 2475 (Cal. Ct. App. 1981).

Opinion

Opinion

SIMS, J.

Placer County is named after a technique of mining for gold—placer mining—that was used extensively in the Sierra foothills [1090]*1090after the discovery of gold in California and until the early years of the 20th century.1 Placer mining is basically a process by which miners build dams, divert waters through flumes or ditches, channel the waters into huge pipes and, ultimately, into nozzles large enough to make one believe that Gulliver himself might have used one to water his garden. When these giant nozzles are trained on gold bearing soil, the water discharged from the monitor washes the soil away, and the runoff mixture of soil and water is run through sluice boxes, where the heavier gold bearing ore settles to the bottom, and is caught by small ridges in the bottom of the sluice boxes.

During the second half óf the 19th century, this process of placer mining resulted simultaneously in the extraction of millions of dollars of gold and the devastation of thousands of acres of land in the Sierra foothills. Even now, more than a century later, the effects of this mining process can be seen at many locations in Placer County where small, straggling pines dot a moon-like landscape in areas that are euphemistically referred to as “the diggin’s.”

Large scale placer mining in the Sierra foothills shut down in the early part of the 20th century. The technique was not discontinued because anyone was concerned about the devastation of the foothills. Nor was the process abandoned because it became too expensive (it remains the most economical method of mining for gold). Nor did the mother lode run out of gold. Rather, placer mining stopped because mud and silt produced by the mines began to fill up the great rivers of Northern California and the agricultural irrigation systems that depended on those rivers. The courts stopped large-scale placer mining by upholding injunctions against mining operations that were obtained by residents of the Sacramento Valley. The theory of injunctive relief was nothing other than good old common law nuisance. (See, e.g., County of Sutter v. Nicols (1908) 152 Cal. 688, 691 [93 P. 872].)

The instant case arose about a century after the heyday of placer mining in Placer County. But the case represents another chapter in the ongoing conflict between placer miners and those who object to the mud and silt generated by placer mining. Here is what happened:

[1091]*1091In January of 1979, William Bakker, a gáme warden with the California Department of Fish and Game, received complaints that the Middle Fork of the American River was unusually muddy. Bakker investigated, ultimately procured a Fish and Game helicopter to fly over the muddy stretch of the river, and took aerial photographs. He also later investigated the situation on foot and by vehicle. By working up the North Fork of the Middle Fork, Bakker determined that the source of mud and silt in the river was the Pacific Slab Placer Mine (Mine), a placer mine located on the North Fork of the Middle Fork of the American River in an area surrounded by familiar landmarks such as Mosquito Ridge, Cuckoo Ridge, Deadwood Ridge, Turkey Hill and Grouse Creek. In February 1979 the river was noticeably muddy for a stretch of 15 to 18 miles. Bakker concluded that the source of river siltation was discharge from the Mine, which obtained its water from a dam on Grouse Creek and which employed classic placer mining techniques: water from Grouse Creek was funneled through pipes at high pressure and then discharged through a monitor so as to blast the earth away. The monitor at the Mine was capable of putting out 12,000 gallons of water a minute. The runoff was carried through sluice boxes and was dumped into the river.

Following Bakker’s investigation, on March 18, 1979, a Fish and Game biologist, Harry Rectenwald, made his way to a point on the river located just below the discharge point of the Mine. There, Rectenwald found three feet of silt deposited along the banks of the river. He also inspected the river for aquatic insects necessary to sustain fish life, and Rectenwald took samples of insect life from above the point of the Mine discharge and from below the point of discharge. He concluded that the river below the Mine had been subject to a significant silt buildup and that, whereas aquatic insects above the point of mine discharge were happy and jiealthy, insect life below the Mine had been destroyed to a significant degree. Silt on the river bottom also prevents fish from laying their eggs in protective spaces that ordinarily exist between rocks and gravels. Subsequently, Rectenwald obtained discharge records kept by the Mine pursuant to requirements of a permit issued to the Mine by the California Water Quality Control Board.2 [1092]*1092These discharge records indicated that the Mine dumped significant amounts of sand and gravel into the river during the month of March 1979. For example, the records indicated that on March 9, 1979, some nine days before Rectenwald’s visit, the Mine discharged some 2,400 cubic yards of solid debris into the river. This discharge was approximately the same as having 200 full sized dump trucks dump their loads into the river at the same place on the same day.

Rectenwald left the river on March 18. He returned to the river during four days in July 1979 and conducted additional experiments. Thus, Rectenwald established four,inspection stations, one located upriver from the Mine and three located within eight miles below the Mine. At each inspection point, the biologist sampled aquatic insect life. He found samples of aquatic, insect life indicated a reduction of volume of insect life of about 90 percent below the point of discharge. Rectenwald also sampled the fish population by using an electric stunning device at two inspection points, one located above the mine discharge point and one below. He found about one-third as many fish at the station below the discharge point as he did at the station above the Mine.

Rectenwald left the river on July 24, 1979.

During the month of January 1980 the river reached flood stage. Indeed, the river reached its highest point since the winter of 1955. In the vicinity of the Mine, the high water mark was 30 to 40 feet above the ordinary river channel. The force of the river was such that it moved large granite boulders and caused the ground to shake. Downstream, near Auburn, automobile bridges were submérged. Suffice it to say that, by everyone’s account, the flood of January 1979 was one remarkable display of H2G.

On February 6, 1980, the District Attorney of Placer County filed a complaint in the Foresthill Judicial District Justice Court charging defendant with violation of section 5650, subdivision (f) Fish and Game Code.3 The complaint alleged that, during the months of February and March of 1979, defendant “... did permit to pass into and deposit in [1093]*1093the American River a substance and material deleterious to fish and plant life.”

Trial of the matter commenced January 29, 1981, in the Foresthill Justice Court. At the outset of trial, the parties stipulated that defendant Guntert was responsible for the operation, supervision and management of the Mine.

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Cite This Page — Counsel Stack

Bluebook (online)
126 Cal. App. Supp. 3d 1, 179 Cal. Rptr. 426, 1981 Cal. App. LEXIS 2475, Counsel Stack Legal Research, https://law.counselstack.com/opinion/people-v-guntert-calappdeptsuper-1981.