Products company mine in background. According to the
United States Census Bureau, the city has a total area of of which of it is land and , or 12.13%, is covered by water. that often fluctuate, although much has been done recently to prevent the lake from drying up, flooding, or becoming stagnant. At , the lake would spill into the outflow channel on its northeastern shore, known properly as Temescal Wash, flowing northwest along I-15, which feeds Temescal Creek, which dumps into the
Santa Ana River just northwest of the City of Corona. It then flows to
Orange County, out to the Pacific Ocean just south of
Huntington State Beach. Lake Elsinore is bordered by the
Elsinore Mountains to the west, which are a part of the larger
Santa Ana Mountain Range, and receive a few inches of snowfall a few days each year. Included in the Santa Ana Mountains is the
Cleveland National Forest and the community of
El Cariso. Lake Elsinore is northwest of
Wildomar and the northern portion is part of the
Temescal Canyon. To the east of the lake are the much older and more eroded slopes of the
Temescal Mountains.
Districts Lake Elsinore is a city which encompasses a large geographical area. To better distinguish the wide range of neighborhoods, the city is organized into 11 districts. Each district beholds its own unique geography, culture, age, and history which together make Lake Elsinore a very diverse and culturally rich city. They are the Alberhill, Ballpark, Business, Country Club Heights, East Lake, Historic, Lake Edge, Lake Elsinore Hills, Lake View, North Peak, and Riverview Districts.
Alberhill The Alberhill District is characterized by rolling terrain, vacant land, and the newly constructed Alberhill Ranch neighborhood. Much of the topography in the central areas, east and west of Lake Street, has been substantially altered as a result of the Alberhill District's long history of extractive/mining activities. Mining operations in the Alberhill District began at Terra Cotta roughly the same time the region's first railroad, the California Southern Railroad, was completed in the 1880s. A spur of the railroad originally built to Terra Cotta was extended into the central portion of the Alberhill District. The
Atchison, Topeka, and Santa Fe Railroad built a line up from Corona through Alberhill to Elsinore after the line through
Railroad Canyon was washed out in the 1920s. These events helped shape the growth of the District. Mining operations for
coal and especially
clay have continued to exist since the late 19th century, and occupy a significant portion of the Alberhill District. Through the years,
Pacific Clay Products Company has purchased the local mines and has become the sole operating clay mine in the region.
Ballpark The Ballpark District takes its name from the
Lake Elsinore Diamond Stadium, a first-class minor league baseball stadium constructed in 1994. It is home to the
Lake Elsinore Storm professional baseball team, an affiliate of the
San Diego Padres. The area was once the site of the first train depot in Lake Elsinore, but no train tracks or structures from that era remain.
Business The developed area within the Business District, in
Warm Springs Valley, is relatively new and has the strongest concentration of industrial and commercial uses within the city. In addition, it hosts several big-box retailers, the Lake Elsinore Outlets, the lake's outlet channel,
Temescal Creek, and marshlands. It is bordered by Country Club Heights to the west and
Interstate 15 to the east, with a small portion extending to the east side of I-15. Sections of the Atchison, Topeka, & Santa Fe Railroads that passed through the Business District during the 1800s have been removed. In addition, a historic ranching and homesteading site with previous ranching and homesteading activities is located nearby the route where the railroad once existed.
Country Club Heights The Country Club Heights District is distinctly marked by the steep hillsides of the
Clevelin Hills, views of the lake and the city, and is a key part of Lake Elsinore's history. The issues mentioned above have presented development constraints for Country Club Heights since its historic beginnings dating back to 1912. The area was the target of an elaborate land scheme promoted in
Los Angeles. The Mutual Benefit and Loan Society of Los Angeles acquired two pieces of dry, "hill-land" within a few miles north of "town-land" that the Press claimed was not worth ten cents an acre. The Mutual Benefit and Loan Society offered to give a lot to anyone who asked; however, the person receiving the lot had to pay ten dollars for a membership in the club, and one dollar per month dues for five years. In 1924, the Clevelin Realty Corporation, headed by Abe Corlin (President) and Henry Schultz (Treasurer-Secretary), began selling additional lots in Country Club Heights and launched a real estate sales promotion in the area. The Clevelin Hills took their name from this company. Noteworthy sites in the Country Club Heights District include: the Schultz Mansion (now Bredlau Castle) and the Corlin Mansion, both built by the Corporation on the Clevelin Hills in 1926 for Henry Schultz and Abe Corlin, respectively, who had originated the Clevelin Realty development. The Bredlau castle is over , and includes a hidden room with a sliding bookcase door that was used during
Prohibition. These stately homes overlooking the lake were the site for many social gatherings. The winding roads of Country Club Heights are adorned with historic Marbelite lampposts, designed by Henry Barkschat. In 2007, the City of Lake Elsinore restored the historic lampposts along Lakeshore Drive. In October 1928,
Aimee Semple McPherson, a renowned evangelist, commissioned Architect Edwin Dickman to design for her a palatial home in Country Club Heights, which has since won fame as "Aimee's Castle". This is said to be a house born of Hollywood, inspired by Moorish architectural design. This home served as the evangelist's part-time home until 1939, when it passed to new ownership. After changing hands many times, in 2005,
International Church of the Foursquare Gospel, the modern incarnation of McPherson's Foursquare Gospel, purchased and restored the property after years of neglect. The Clevelin Country Club (later known as the Lake Elsinore Country Club, The Spa Club and the Casino Del Elsinore) was built to be the main attraction of the Country Club Heights subdivision. Prominent members of the club included Mrs. Wallace Reid, Marie Prevost, Reginald Denny, Jack Dempsey, Bert Lytell, Damon Runyon and Joe Stecher, for whom the streets were named. This Spanish-Mediterranean Moorish accented architectural masterpiece had over 20,000 square feet of floor space and included a ballroom, banquet hall, sleeping quarters, and a tunnel system to hidden rooms. The Country Club closed during the depression, but reopened in 1951. It has closed again before 1981, at which point restoration work was being undertaken, but by 1990 the property was vacant and derelict.
East Lake The East Lake District is partially developed and contains the newly constructed Summerly neighborhood. It is a generally flat area that does not contain any registered historic structures. However, portions of the East Lake District were used during prehistoric times by Native American Indians as flaking and grinding stations. In addition, a historic ranching and homesteading site is located just outside the East Lake District along the border with
Lakeland Village to the southwest. More recently, the East Lake District has also been home to popular motocross, skydiving, glider plane, and hang gliding activities. Throughout the city's history, Lake Elsinore has alternated between severe floods and droughts. Most of the East Lake District lies within a 100-year floodplain adjacent to and southeast of the lake. As a result, the district has been significantly affected during wet seasons and high water levels in the lake. Major floods occurred in 1884 and in 1916. In 1969, of rain fell in 11 days and severely flooded the lake's shores. The East Lake District's proximity to the lake and flood storage is a key consideration in all planned development and several projects have been implemented to prevent the lake from flooding again.
Historic District The Historic District has been the focal point of the city since its incorporation in 1888. In 1925, W.R. Covington and Associates of Santa Monica purchased of lake frontage and three blocks of slightly improved land across Poe Street from Warm Springs Park. A clubhouse, swimming pool, and other facilities projected to cost $200,000 (or $ million today) were built on this property. No records have been found to provide the date when a fire destroyed the clubhouse, but remnants of the burned structure and surrounding trees examined in 1942 indicate the fire must have occurred soon after the building was constructed. The Covington resort was built in the Town of Elsinore. Today, several unregistered historic buildings exist, including the Crescent Bath House, also known as "The Chimes"; The Chamber of Commerce (Santa Fe Train Station); The Cultural Center (The Methodist Church); Armory Hall; The Ambassador Hotel (Elsinore Consolidated Bank); Jean Hayman House; and Elsinore City Park The neighborhoods in this area are the oldest in the city, and its commercial strip along Main Street is considered to be downtown.
Lake Edge District The Lake Edge District area has had a long and eventful history, with the lake as a focal point for the Native Americans, Europeans, Mexicans, early founders of the city, and the multitude of visitors and locals who continue to come to its shores for entertainment and recreation. Many developments occurred along or within proximity of the lake's edge during the second half of the 19th and the first half of the 20th centuries. The Lake Edge District encompasses the ruins of the city's oldest standing structure, the Machado Adobe House, Rancho La Laguna This site was the location of the Laguna Grande Butterfield Stage Station. This structure succumbed to arson in 2017. A structure of historical interest is Meyer & Holler designed Southern California Athletic and Country Club, former
Elsinore Naval and Military School building, located along Grand Avenue near the intersection of Ortega Highway. A newly constructed campground, marina, and boat launch is located on the northwest side of the lake.
Lake Elsinore Hills The Lake Elsinore Hills District encompasses a large and varied terrain including broad plains, rolling hills, steep slopes, sensitive habitats, and watercourses, with elevations ranging from above the sea level. Many areas of the Lake Elsinore Hills District are not readily accessible or able to be developed, so have remained vacant. Two large bodies of water located within close proximity of the Lake Elsinore Hills District are the city's lake to the southwest and
Canyon Lake to the east, which is located within the city of
Canyon Lake. Some of the higher elevations offer panoramic views of the city's lake and the
Santa Ana Mountains. The neighborhoods in this district include Tuscany Hills, Canyon Hills, and Rosetta Canyon.
Lake View The northwestern areas of the Lake View District offer beautiful views of the lake and the neighboring mountains, and are characterized by high elevations, steep slopes, and a series of canyons. The remaining areas of the Lake View District are relatively flat in the lower elevations. Historically, the northern portion of the Lake View District has remained mostly undeveloped, with the exception of the La Laguna Estates neighborhood above McVicker Canyon Park. Similar to the areas further north, the
Atchison, Topeka, and Santa Fe Railroad and abundant mining opportunities extant in the late 19th century brought both residents and visitors to the area. Historic ranching and homesteading, including Torn Ranch, were generally located to the northwest of Machado Street, which was an important roadway lined with beautiful
deodar trees. Most of the lower-lying areas of the Lake View District to the north have been recently developed and primarily include single-family homes. Other neighborhoods in this area include Northshore and Lake Terrace, which were both formerly orange groves. Another area in this district at the intersection of Riverside and Lakeshore Drives has long been to referred to as "Four Corners" by local residents.
Riverview The Riverview District is a combination of steep terrain and flat areas nestled between a knoll with steep slopes, a major watercourse, and the lake. Higher elevations and steep slopes are located in the northwest areas of the Riverview District, which function as a physical border with most of the adjacent Historic District. The San Jacinto River floodway, located within the Riverview District along the eastern and southern areas, is the city's major watercourse. The river flows southwest from
Canyon Lake through the Lake Elsinore Hills District and the Riverview District, then ultimately empties into the lake.
Climate Lake Elsinore has a
mild semi-arid climate (
Köppen climate classification BSk/BSh), with hot, almost rainless summers and mild, wetter winters. While too dry for this classification, its thermal regime and precipitation distribution resembles that of a
hot-summer Mediterranean climate (Köppen
Csa), which is present in many surrounding areas. On average, the hottest month is July, and the coolest month is December. The highest recorded temperature was , first recorded on August 12, 1933, and the lowest recorded temperature was on December 30, 1974. The maximum average precipitation occurs in January with , and the minimum average precipitation in June with , although less than half of all Junes, Julies, Augusts, and Septembers record any precipitation whatsoever. The greatest amount of precipitation ever received in one day was , on February 15, 1927.{{cite web ==Demographics==