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Anchor Inn: Late 18th or early 19th century: A public house in stone with quoins and a stone-slate roof in two storeys. The doorway is in Palladian style, with rusticated jambs, a frieze, a pediment, and a fanlight. [12] II
Woburn Sands (/ ˈ w oʊ b ər n /) is a town that straddles the border between Buckinghamshire and Bedfordshire in England, and is part of the Milton Keynes urban area. [2] The larger part of the town is in Woburn Sands civil parish, which is in the City of Milton Keynes, [3] Smaller parts of the town are in the neighbouring parishes of Aspley Guise and Aspley Heath (in Central Bedfordshire). [1]
Anchor Inn may refer to: The Anchor Inn (Birmingham), a public house in Digbeth, Birmingham, England; Anchor Inn (Dorset), a public house in Dorset, England; The Anchor Inn (Combwich), a public house in Somerset, England; The Anchor Inn (Wheaton, Maryland), a former restaurant and business development in Wheaton, Maryland
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Woburn (/ ˈ w oʊ b ər n /, meaning twisted or crooked stream) [1] is a town and civil parish in Bedfordshire, England, about 5 miles (8 km) southeast of Milton Keynes and 3 miles (5 km) south of junction 13 of the M1 motorway. At the 2011 census, it had a population of 933.
Woburn Sands has a black and white "cottage" station building, one of four of the same design that are unique to this line. Two of the others remain at Fenny Stratford and Milbrook. The building is in a half-timbered Gothic Revival style that had been insisted upon by the 7th Duke of Bedford for stations close to the Woburn Estate.
The total land utilized in Auburn for the interstate is about 200 acres. I-290: The first three miles of the 20 mile long eastbound (heads north in Auburn) Interstate 290 is in Auburn along with exits 7 (I-90), 8 (Rt. 12), and 9 (Swanson Rd EB, Auburn St. WB). I-395: Two miles of Interstate 395 are in Auburn which becomes I-290 after Exit 6 (US ...
The Woburn Sands Formation is a geological formation in England. Part of the Lower Greensand Group, it is the only unit of the group where it occurs, and thus is sometimes simply referred to as the 'Lower Greensand' in these areas. It was deposited during the late Aptian to early Albian stages of the Early Cretaceous.