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This work is in the public domain in the United States because it is a work prepared by an officer or employee of the United States Government as part of that person’s official duties under the terms of Title 17, Chapter 1, Section 105 of the US Code.
Bear Creek Golf Club (Murrieta, California) – 1982; The Country Club at Muirfield Village (Dublin, Ohio) – 1982; Atlanta Country Club (Atlanta, Georgia) – 1983 (redesign) Park Meadows Country Club (Park City, Utah) – 1983; Bear Lakes Country Club (West Palm Beach, Florida) – 1984 Lakes course – 1985; Links course – 1987
The course of Bear Creek is entirely contained within San Bernardino County, and primarily within the San Bernardino National Forest. It rises near the community of Woodlands, and flows north into Baldwin Lake in the eastern Big Bear Valley .
The Bear Creek Redwoods Open Space Preserve is a public open space preserve in Santa Clara County, California, United States, in the Santa Cruz Mountains.The preserve is located along both sides of Bear Creek Road, west of State Route 17 and Lexington Reservoir, and mostly north and east of the Skyline Boulevard and Summit Road sections of State Route 35.
The tributary Bear Creek joins the Sammamish from the east, also containing the waters from Evans Creek and Cottage Lake Creek. After passing through Redmond and parts of unincorporated King County, the Sammamish enters Woodinville where it turns northwest and then west. Little Bear Creek joins the Sammamish at this western turning point from ...
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The park and trails are a central component of a larger regional multi-use trail system, a connected destination from the south and north on protected multi-use trails as well as the west through Morrison and east along the Bear Creek Trail corridor. Within the park there are miles of quiet dirt paths along streams as well as paved multiple-use ...
West Bear Creek is a small tributary to Bear Creek located in eastern North Carolina. The West Bear Creek watershed is a tiny contributing area of the Neuse River basin. The geology of the area is mostly siliclastic sediments and organic soils. Deep groundwater is fed to the creek by the Black Creek aquifer.