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On July 29, 2008, a magnitude 5.4 earthquake was located 3 miles (4.8 km) southwest of Chino Hills that was felt throughout Southern California and felt as far east as the Las Vegas Valley and as far south as San Diego.
"Map of faults in southern California," By Natural Hazards Mission Area Photographer, Kate Scharer, USGS Sources/Usage, Public Domain Accessed 10-20-2024 You cannot overwrite this file. File usage
This image is a derivative work of the following images: USA California location map.svg licensed with Cc-by-3.0, GFDL . 2009-06-05T19:17:46Z NordNordWest 1022x1171 (491838 Bytes) more detailed
Chino Hills is served by Omnitrans' OmniLink demand-response service open to the general public. For $2.50 each way, one can travel throughout the city and transfer for free to the Omnitrans public bus at the Chino Hills Marketplace and the Chino Hills Civic Center. The dial-a-ride service operates five days a week, mostly during daytime hours ...
The cities of Chino Hills and Chino comprise the Chino Valley. The two cities have a combined population of approximately 175,000, and are part of the Inland Empire region. The Chino Valley is east of the low Chino Hills mountain range. Chino Creek flows through the western side of the valley.
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The Chino Fault and Whittier Fault are the two upper branches of the Elsinore Fault Zone, [2] which is part of the trilateral split of the San Andreas Fault system. The right-lateral strike-slip fault has a slip rate of 1.0 millimeter/year and is capable of producing anywhere from a M w 6.0 to a M w 7.0 earthquake.
Essentially, the mountain ranges separate southern California into two distinct climatic regions: The heavy-populated coastal area west of these mountains is the one most associated with the term "southern California" and is characterized by pleasant weather all-year round, without frequent heat spells in the summer and without low temperatures ...