Former Remco Hydraulics Facility

The Former Remco Hydraulics Facility (Facility) at 934 S. Main Street is an elongated, fenced parcel of approximately seven acres, located immediately adjacent to and west of U.S. Highway 101 (Main Street) in the southern portion of the City of Willits. The original Facility building was constructed on the property in 1945. A growing industrial machining and manufacturing business was operated under numerous owners at the Remco Facility from approximately 1945 until 1995. Chrome plating operations were conducted between approximately 1963 and 1995. The last owners, Remco Hydraulics, Inc. and its parent company, MC Industries, both declared bankruptcy in 1995 and the Facility was closed in 1996. As of August 22, 1997, the Final Consent Decree established the current owner of the facility, the Willits Trust, to investigate and remediate the Site. So far, over 821 soil, 2,929 groundwater, and 109 air samples have been collected while investigating this Site and multiple remedial actions have been completed. Further information regarding these activities can be found on the Document Depository.

The primary chemicals detected at the Remco Site are volatile organic compounds (VOCs) and hexavalent chromium. In addition, other metals, petroleum hydrocarbons, polyaromatic hydrocarbons (PAHs), and polychlorinated biphenyls (PCBs) were detected in on a more limited basis at the Remco Facility.

During the rainy season, the Facility storm water system collects and channels runoff into a system of catch basins and underground storm-drain pipes that carry the water to the northeast corner of the Facility, where it enters the City of Willits’ storm-drain system and discharges to Baechtel Creek. The raised railroad tracks to the south of the Facility prevent water from flowing onto the Facility from the south and form the South Drainage Ditch, which acts as a small stream during the rains.

Three groundwater-bearing zones have been identified at the Site and are referred to, from shallowest to deepest, as the A-, B- and C-Zones. Each of these zones flows generally toward the northeast. In most locations investigated, fine grained low-permeability soil exists between the aquifers, limiting groundwater movement between the zones.