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Much and town's
Much of the town's income has traditionally come from dairy production and processing ; Gustine is the home of a Golden Valley Cheese factory and formerly a Carnation processing plant.
Much of the town's border with East Haven to the west is dominated by Lake Saltonstall, a reservoir owned by the South Central Connecticut Regional Water Authority, and Saltonstall Mountain, part of the Metacomet Ridge, a mountainous trap rock ridgeline that stretches from Long Island Sound to nearly the Vermont border.
Much of the town's acreage is dominated by Totoket Mountain, part of the Metacomet Ridge, a mountainous trap rock ridgeline that stretches from Long Island Sound almost to the Vermont border.
Much of the town's property is under the ownership of developer Wayne Mason.
Much of the town's architectural heritage from those days has been preserved.
Much of the town's land area lies outside of these villages.
Much of the town's land is protected as part of the Quabbin Reservation, a protected area surrounding the Quabbin Reservoir.
Much of the town's population is concentrated in the village and this area.
Much of the heritage and the town's name itself can be attributed to the cotton milling industry that followed.
Much of that growth can be attributed to the town's close proximity to the Research Triangle area and access to major highways such as I-40, U. S. 70, and NC 42.
Much of the town's growth was due to its position as a transportation center, first as the starting point on the Forbes Road to Pittsburgh.
Much of the town's business district was destroyed by a major fire in 1912.
Much of the town's poorer housing formerly lay in a series of narrow yards that ran northward from the marketplace and Wrawby Street.
Much of the town's population is centered on the eastern side of town, closer to the former town geographic center.
Much of the eastern mainland part of town is marshy, feeding Mud Creek, Mill River and the Rowley River, which constitutes part of the town's southern border.
Much of the northern half of town is spotted with swamps, and the town is home to three large hills, Temple Hill and Tully Mountain in the north and Chestnut Hill, the town's highest point, in the south.
Much of Enfield and Greenwich became part of the town of Ware, extending the town's lands northward.
Much of the city was destroyed during World War II and for several years during the following reconstruction the Soviet authorities prohibited the return of any of Narva's pre-war residents ( among whom ethnic Estonians had been the majority, forming 64. 8 % of the town's population of 23, 512 according to the 1934 census ), thus radically altering the city's ethnic composition.
Much of the town's early history surrounds the bishops of Durham and the establishment of a hunting lodge, which later became the main residence of the Bishops of Durham.
Much of the town's history surrounds its links with the Bishops of Durham.
Much of the town's architecture is still heavily influenced by the style of ornate building which Prince Albert popularised.
Much of the town's industry in the 19th and 20th century was centred around the linen trade.
Much of the town centre is lined with brick buildings from the 17th and 18th centuries and the town's skyline is dominated by St. James ' Church, the spire of which is tall, though shorter than both Norwich Cathedral () and Salisbury Cathedral () in terms of spire height, it is reputedly the tallest Anglican parish church in the United Kingdom.
Much of the town's history comes from this family of industrial pioneers.

Much and southern
Much of the southern border is formed by tributaries of the Congo River, with the Mbomou River in the east merging with the Uele River to form the Ubangi River.
Much of southern and western Connecticut ( along with the majority of the state's population ) is part of the New York metropolitan area ; three of Connecticut's eight counties are statistically included in the New York City combined statistical area, the same area is widely referred to as the Tri-State area.
Much of the western, southern, and central mountains are open woodland ; supporting pine forest interspersed with some oak, scrub, and grassy clearings.
Much of Khammouan Province and the eastern part of all the southern provinces are mountainous.
Much of central and western Mongolia, including Ulaanbaatar, is antipodal to southern Patagonia.
Much of the continent has just one species of rabbit, the tapeti, while most of South America's southern cone is without rabbits.
Much of the population of the Scandinavian Peninsula is naturally concentrated in its southern part, which is also its agricultural region.
Much of Baltimore County is suburban in character, straddling the border between the Piedmont plateau and, in the southern regions of the county, the Atlantic coastal plain.
Much of the southern region is semi-arid and desert.
Much of the southern portion of the county lies within the Catskill Mountains.
Much larger forms are found in the later rocks of the upper part of the Jurassic and the lower part of the Cretaceous, such as Titanites from the Portland Stone of Jurassic of southern England, which is often 53 centimetres ( 2 feet ) in diameter, and Parapuzosia seppenradensis of the Cretaceous period of Germany, which is one of the largest known ammonites, sometimes reaching 2 metres ( 6. 5 feet ) in diameter.
Much of the terrain of eastern Polk County is mountainous, including Big Frog Mountain, constituting part of the southern Appalachian Mountains.
Much of the southern border of the county runs directly along the Ohio River.
Much of the southern part of the route runs through rural areas of Salem and Gloucester counties, passing through the communities of Woodstown and Mullica Hill.
Much of the city's southern border is shared with the Talladega National Forest.
Much of southern Ontario still contains dairy farms and other agricultural farms.
Much of the southern section of town is urbanized and is difficult to distinguish from neighboring New Haven.
Much of Peru is forested, with a large portion of the northern third of town covered by a wildlife management area, and much of the southern third covered by the Peru and Middlefield State Forests.
Much of the population is concentrated in two areas ; one, the Lebanon Mills and Perrins Crossing neighborhoods in the north, and the other, the southern neighborhoods of Luthers Corners and South Seekonk, mostly located between Interstate 195 and Route 44.
Much of the central and southern part of town is covered by Monroe State Forest, which extends into neighboring Florida.
Much of Hanover's eastern and southern borders consist of three waterways, the North and Indian Head rivers along the south and southeast, and the Third Herring Brook along the east.
Much of southern Allegheny County is undermined, and the PADEP indicates that all of Bethel Park was undermined.
Much of the material culture of the Kofun period demonstrates that Japan at this time was in close political and economic contact with continental Asia, especially with the southern dynasties of China, via the countries of the Korean peninsula.
Much of central Asia and southern Russia was won over to Islam through the missionary work of the ṭarīqahs, and the majority of Indonesia's population, where a Muslim army never set foot, was converted to Islam by the perseverance of both Muslim traders and Sufi missionaries.

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