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Hollywood Hills
The Hollywood Hills are a residential neighborhood in the central region of Los Angeles, California. Geography The Hollywood Hills straddle the Cahuenga Pass within the Santa Monica Mountains. The neighborhood touches Studio City, Universal City and Burbank on the north, Griffith Park on the north and east, Los Feliz on the southeast, Hollywood on the south and Hollywood Hills West on the west. It includes Forest Lawn Memorial Park, Mount Sinai Memorial Park Cemetery, the Hollywood Reservoir, the Hollywood Sign, the Hollywood Bowl and the John Anson Ford Theater.''The Thomas Guide,'' 2006, pages 563 and 593 Hollywood Hills is bisected southeast–northwest by US 101. The neighborhood is bounded on the northwest and north by the Los Angeles city line, on the east by a fireroad through Griffith Park, continuing on Western Avenue, on the south by Franklin Avenue and on the west by an irregular line that includes Outpost Drive. Bedrock of the Hills is a complex asso ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neighborhoods In Los Angeles
This is a list of notable districts and neighborhoods within the city of Los Angeles, Los Angeles, California, present and past. It includes residential and commercial areas and business-improvement districts, but does not include sales subdivisions or sales tracts. The guiding precept is Wikipedia:Notability (geographic features)#Geographic regions, areas and places. AE * Adams-Normandie, Los Angeles, Adams-Normandie * Alsace, California, Alsace * Angelino Heights, Los Angeles, Angelino Heights''The Thomas Guide: Los Angeles County'', Rand McNally (2004), pages N and O * Angeles Mesa, Los Angeles, Angeles Mesa * Angelus Vista, Los Angeles, Angelus Vista * Arleta, Los Angeles, ArletaNeighborhoods , Mapping L.A., ''Los Angeles Times'' * Arlington Heights, Los Angeles, Arlington Heights * Arts Di ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hollywood Hills West
Hollywood Hills West is a neighborhood within Central Los Angeles, California. There are three city parks and one elementary school. Geography Hollywood Hills West touches Studio City on the north, Hollywood Hills on the east, Hollywood and West Hollywood on the south and Beverly Hills and Coldwater Canyon on the west. The neighborhood is bisected by Laurel Canyon Boulevard and is bordered on the east by Outpost Drive and on the south by an irregular line that includes Franklin Avenue, Fairfax Avenue and Sunset Boulevard, or the West Hollywood city limits. On the west the neighborhood ends at the Beverly Hills city line (Trousdale Estates, and on the north it stops at Mulholland Drive. "Central L.A.," Mapping L.A., ''Los Angeles Times'' [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite.Blatt, Harvey and Robert J. Tracy (1996) ''Petrology: Igneous, Sedimentary and Metamorphic'', 2nd ed., Freeman, pp. 281–292 Shale is characterized by its tendency to split into thin layers ( laminae) less than one centimeter in thickness. This property is called '' fissility''. Shale is the most common sedimentary rock. The term ''shale'' is sometimes applied more broadly, as essentially a synonym for mudrock, rather than in the more narrow sense of clay-rich fissile mudrock. Texture Shale typically exhibits varying degrees of fissility. Because of the parallel orientation of clay mineral flakes in shale, it breaks into thin layers, often splintery and usually parallel to the otherwise indistinguishable beddin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Metamorphic
Metamorphic rocks arise from the transformation of existing rock to new types of rock in a process called metamorphism. The original rock (protolith) is subjected to temperatures greater than and, often, elevated pressure of or more, causing profound physical or chemical changes. During this process, the rock remains mostly in the solid state, but gradually recrystallizes to a new texture or mineral composition. The protolith may be an igneous, sedimentary, or existing metamorphic rock. Metamorphic rocks make up a large part of the Earth's crust and form 12% of the Earth's land surface. They are classified by their protolith, their chemical and mineral makeup, and their texture. They may be formed simply by being deeply buried beneath the Earth's surface, where they are subject to high temperatures and the great pressure of the rock layers above. They can also form from tectonic processes such as continental collisions, which cause horizontal pressure, friction, and distorti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granitic
A granitoid is a generic term for a diverse category of coarse-grained igneous rocks that consist predominantly of quartz, plagioclase, and alkali feldspar. Granitoids range from plagioclase-rich tonalites to alkali-rich syenites and from quartz-poor monzonites to quartz-rich quartzolites. As only two of the three defining mineral groups (quartz, plagioclase, and alkali feldspar) need to be present for the rock to be called a granitoid, foid-bearing rocks, which predominantly contain feldspars but no quartz, are also granitoids. The terms ''granite'' and ''granitic rock'' are often used interchangeably for granitoids; however, granite is just one particular type of granitoid. Granitoids are diverse; no classification system for granitoids can give a complete and unique characterization of the origin, compositional evolution, and geodynamic environment for the genesis of a granitoid. Accordingly, multiple granitoid classification systems have been developed such as those based ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Franklin Avenue (Los Angeles)
Franklin Avenue is a street in Los Angeles. It is the northernmost thoroughfare in Hollywood, north of Hollywood Boulevard, and the southern border of the Hollywood Hills. It is the center of the neighborhood of Franklin Village. Franklin Avenue begins as a residential street off Sierra Bonita Avenue. Continuing east, Franklin is the southern border of Whitley Heights, and turns into a major east–west thoroughfare in the Hollywood Hills. Franklin Avenue ends in Los Feliz. Landmarks and neighborhoods Listing landmarks from west to east on Franklin, The Magic Castle is furthest west. The first house in the Hollywood area, built by Tomás Urquidez in 1854, was at the intersection of what would become Franklin Avenue and Outpost Drive. The corner of Franklin and Gower Street is cited as one of the better places to photograph the Hollywood Sign. The Château Élysée, a former residential apartment house for movie stars (now the Church of Scientology Celebrity Centre) is loca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Western Avenue (Los Angeles)
Western Avenue is a major four-lane street in the city of Los Angeles (west of Downtown) and through the center portion of Los Angeles County, California. It is one of the longest north–south streets in Los Angeles city and county, apart from Sepulveda Boulevard. It is about long. Description Western Avenue passes through a large diversity of residential neighborhoods in Los Angeles County. From the south, where it transitions into Paseo Del Mar near White Point and the Pacific Ocean, it begins in San Pedro, then passes through Rancho Palos Verdes, Harbor City, Gardena and South Los Angeles. It is also the easternmost border of Torrance. Around the Pico Boulevard, Olympic Boulevard, and Wilshire Boulevard intersections, Western Avenue passes through Koreatown. Further north, Western Avenue passes through the East Hollywood district. Around the Santa Monica Boulevard, Sunset Boulevard, and Hollywood Boulevard intersections, it passes through the East Hollywood neighborho ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fireroad
A firebreak or double track (also called a fire line, fuel break, fireroad and firetrail in Australia) is a gap in vegetation or other combustible material that acts as a barrier to slow or stop the progress of a bushfire or wildfire. A firebreak may occur naturally where there is a lack of vegetation or "fuel", such as a river, lake or canyon. Firebreaks may also be man-made, and many of these also serve as roads, such as a logging road, four-wheel drive trail, secondary road, or a highway. Overview In the construction of a firebreak, the primary goal is to remove deadwood and undergrowth down to mineral soil. Various methods may be used to accomplish this initially and to maintain this condition. Ideally, the firebreak will be constructed and maintained according to the established practices of sustainable forestry and fire protection engineering, also known as best management practices (BMP). The general goals are to maximize the effectiveness of the firebreak at slowing th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
City Limits
City limits or city boundaries refer to the defined boundary or border of a city. The area within the city limit can be called the city proper. Town limit/boundary and village limit/boundary apply to towns and villages. Similarly, corporate limit is a legal name that refers to the boundary of municipal corporations. In some countries, the limit of a municipality may be expanded through annexation. United Kingdom In the UK, city boundaries are more difficult to define, since British cities are defined as any town or local authority area, regardless of area or population size, that has been granted letters patent as a royal prerogative. In smaller cities, such as Wells (pop. approx. 10,000) or Gloucester (pop. approx. 100,000), the boundary will be that governed by the city council, though in certain cases such as Carlisle, this may include large rural and even uninhabited areas which are largely distinct from the main settlement. In the case of larger cities, such as Birmingham ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
John Anson Ford Amphitheatre
The John Anson Ford Theatre is a music venue in the Hollywood Hills neighborhood of Los Angeles, California. The 1,200-seat outdoor amphitheater is situated within the Cahuenga Pass within the Santa Monica Mountains. Located in a County regional park, the facility is owned by the County of Los Angeles and operated in partnership with thFord Theatre Foundationand the Los Angeles County Department of Parks and Recreation. History Christine Wetherill Stevenson and The Pilgrimage Play An amphitheatre was built in 1920 as a venue for The Pilgrimage Play. The author, Christine Wetherill Stevenson, believed the rugged beauty of the Cahuenga Pass would provide a dramatic outdoor setting for the play. Together with Mrs. Chauncey D. Clark, she purchased the land along with that on which the Hollywood Bowl now sits. A wooden, outdoor amphitheatre was built on the site and the play was performed by noted actors every summer from 1920 to 1929, until the original structure was destroyed by a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hollywood Bowl
The Hollywood Bowl is an amphitheatre in the Hollywood Hills neighborhood of Los Angeles, California. It was named one of the 10 best live music venues in America by ''Rolling Stone'' magazine in 2018. The Hollywood Bowl is known for its distinctive bandshell, originally a set of concentric arches that graced the site from 1929 through 2003, before being replaced with a larger one to begin the 2004 season. The shell is set against the backdrop of the Hollywood Hills and the famous Hollywood Sign to the northeast. The "bowl" refers to the shape of the concave hillside into which the amphitheater is carved. The Bowl is owned by the County of Los Angeles and is the home of the Hollywood Bowl Orchestra, the summer home of the Los Angeles Philharmonic, and the host venue for hundreds of musical events each year. It is located at 2301 North Highland Avenue, west of the (former) French Village. It is north of Hollywood Boulevard and approximately 1 mile (1.6 km) from the Hol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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