Sherman commonly refers to:
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Sherman is a city in and the county seat of Grayson County, Texas, United States. The city's population in 2010 was 38,521. It is also one of two principal cities in the Sherman–Denison Metropolitan Statistical Area. It is also a part of the Texoma region.
Sherman was named after General Sidney Sherman (July 23, 1805 – August 1, 1873), a hero of the Texas Revolution. The community was designated as the county seat by the act of the Texas legislature which created Grayson County on March 17, 1846. In 1847, a post office began operation. Sherman was originally located at the center of the county, but in 1848 it was moved about three miles (5 km) east to its current location. By 1850, Sherman had become an incorporated town under Texas law. It had also become a stop on the Butterfield Overland Mail route through Texas. By 1852, Sherman had a population of 300. It consisted of a public square with a log court house, and several businesses, a district clerk's office, and a church along the east side of the square.
Sherman was a suburban line of the Pacific Electric Railway, originally built in 1896 as part of the Pasadena and Pacific. Pasadena and Pacific became part of the Los Angeles Pacific Railroad. The line ran between Downtown Los Angeles and the suburb of Sherman (present-day) West Hollywood. The line is named after Moses Sherman, who built the line and built Sherman street car yard on the line in West LA. The large 5.56 acre, rail facility was on Santa Monica Boulevard just West of La Cienega Boulevard. The yard had a steam power house, a car barn and a shop building. Pacific Electric moved the yard works to 7th & Central in LA. In the 1930 buses started to run from the depot there also. The lines was discontinued on September 25, 1954. In 1974 all the rail buildings were taking down for development.
Clay is a fine-grained natural rock or soil material that combines one or more clay minerals with traces of metal oxides and organic matter. Clays are plastic due to their water content and become hard, brittle and non–plastic upon drying or firing. Geologic clay deposits are mostly composed of phyllosilicate minerals containing variable amounts of water trapped in the mineral structure. Depending on the content of the soil, clay can appear in various colours, from white to dull gray or brown to a deep orange-red.
Clays are distinguished from other fine-grained soils by differences in size and mineralogy. Silts, which are fine-grained soils that do not include clay minerals, tend to have larger particle sizes than clays. There is, however, some overlap in particle size and other physical properties, and many naturally occurring deposits include both silts and clay. The distinction between silt and clay varies by discipline. Geologists and soil scientists usually consider the separation to occur at a particle size of 2 µm (clays being finer than silts), sedimentologists often use 4–5 μm, and colloid chemists use 1 μm.Geotechnical engineers distinguish between silts and clays based on the plasticity properties of the soil, as measured by the soils' Atterberg limits. ISO 14688 grades clay particles as being smaller than 2 μm and silt particles as being larger.
Mythimna ferrago, the clay, is a moth of the family Noctuidae. It is distributed throughout Europe and is also found in Morocco, Algeria, Turkey, Asia Minor, Armenia, Syria, Turkestan, Israel, Lebanon, Iraq, Iran, Central Asia and the western parts of temperate North Asia. Also Tibet.
The forewings of this species vary from buffish to orangey brown, usually with a darker central line running longways down the wing, interrupted by a pale stigma. There are usually a few small dark spots in the basal area. The hindwings are dark grey with paler margins. The male is easily recognizable by a triangular area of black hair on the underside of the abdomen. The wingspan is 36–44 mm. This moth flies at night in July and August and is attracted to light and sugar.
The wingspan is 36–44 mm. Forewing pale greyish rufous, speckled with dark;lines indistinct, dark grey; the outer regularly lunulate-dentate, the teeth marked by black dashes on veins;reniform stigma obscure, ending in a cloudy pale spot at lower end of cell; hindwing greyish ochreous; ventral tufts black. The species varies in coloration: ferrago F. is the reddest form: - grisea Haw, is grey without any rufous admixture, with the markings generally clearer; fulvescens Tutt is rare, with fulvous in the place of red; — ab. marginata Tutt has silvery grey hindwings with broad dark border.
Clay is a 2008 Hip-hop musical loosely based on Shakespeare's Henry IV, Parts 1 and 2. The central character, Sir John, is based on Falstaff. It was written and performed by Matt Sax. The first performance was at the Edinburgh Festival Fringe.
The show opens with Sir John presenting his protégé, Clay, for his first major concert. Clay shows up an hour late, blood covering his face. In an attempt to stall for time, Sir John tells the audience the story of Clay's life.
Clay's real name is Clifford Keys. His father is an emotionally absent businessman, and his mother is a depressed chain-smoker. When he is seven years old, Clifford's parents decide to divorce, and his father manipulates the boy into asking to stay with his father. After missing three of Clifford's birthdays in a row, Clifford's mother commits suicide. His father quickly remarries.
Years pass, and Clifford is sixteen years old. To escape his dysfunctional family, he begins going to open-mic nights at a small bookstore. The MC is Sir John, a talented rapper whose face was deformed in a car accident and has no chance of getting signed to a record label. Clifford begins weekly hip-hop lessons with Sir John, and he begins his transformation from awkward novice to confident storyteller. When Sir John asks Clifford to rap about the girl he loves, Clifford reveals that he is in love with his stepmother, and they have slept together. Sir John begs Clifford to come live with him, but Clifford refuses.