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Morgan Hill is approximately 39 km (24 mi) south of downtown San Jose , 21 km (13 mi) north of Gilroy , and 24 km (15 mi) inland from the Pacific coast . Lying in a roughly 6 km-wide (4-mi-wide) southern extension of the Santa Clara Valley , it is bounded by the Santa Cruz Mountains to the west and the Diablo Range to the east. At the valley floor, Morgan Hill lies at an elevation of about 107 m (350 ft) above MSL .
According to the U.S. Census Bureau , the city encompasses an area of 12.9 square miles (33 km 2 ), all land. Although there are no natural lakes or ponds within the city limits, there are several flood-control and water storage reservoirs in the adjacent hills which are operated by the Santa Clara Valley Water District , with recreational activities such as boating, etc., administered by the Santa Clara County Department of Parks and Recreation.
Morgan Hill is located within the seismically active San Francisco Bay region . The significant earthquakes in the region are generally associated with crustal movements along well-defined, active fault zones. The nearest known active faults are the San Andreas Fault , approximately 19 km (12 mi) southwest, and the Calaveras Fault , approximately 1.6 km (0.99 mi) northeast. Both faults have produced major earthquakes in the past, and have estimated maximum credible Richter magnitudes of 8.3 and 7.3 respectively.
The Sargent-Berrocal Fault, a potentially active fault, lies 16 km (9.9 mi) away from the sites and has an estimated maximum credible Richter magnitude of 7.4. The Coyote Creek Fault is located in Morgan Hill and is classified as potentially active as well. In addition, several unnamed faults traverse the western slopes of the upland areas. Geomorphic evidence suggests that these faults were active during recent geologic time. However, these fault-related geomorphic features are not as fresh as those of the active Calaveras Fault and are considered to be somewhat older.
Morgan Hill is one of very few sources for a type of semi-precious gemstone marketed under the name "Morgan Hill poppy jasper ". According to geologists, this local variety of orbicular jasper formed through a combination of volcanic and seismic activity on the slopes of El Toro. Known extant deposits of the mineral are located on private lands, not accessible to the public. A local business, El Toro Brewing Company, has a collection of poppy jasper on display at their rural Morgan Hill brewery and on a large bar top inlaid with the stone at their brewpub in downtown Morgan Hill. Examples are also on display at the Morgan Hill Museum and at the Morgan Hill Community and Cultural Center. The local Poppy Jasper Film Festival is also named after the mineral.
The highlight of local geography is El Toro . According to a local legend of the early 1900s, author Bret Harte named the hill when he climbed it and discovered two bulls fighting near the summit (they subsequently chased him back down). The official name shown on the U.S. Geological Survey 's maps is simply "El Toro", although locals may refer to the hill as "Murphy's Peak". Visitors, not aware of the origin of the town's name, often mistakenly assume that El Toro is "Morgan" Hill. It is USGS Feature ID# 223063 in the Geographic Names Information System (GNIS), maintained by the United States Board on Geographic Names . Elevation at the summit is about 435 m (1427 ft). The iconic hill overshadowing the town to the west, has been incorporated into the city's seal and official logo.