Croft is a small village and civil parish in the East Lindsey district of Lincolnshire, England. The village is situated approximately 2 miles (3 km) north-east from Wainfleet, and 4 miles (6 km) south-west from Skegness.
Croft is listed in the 1086 Domesday Book with 15 households, 120 acres (0.5 km2) of meadow and a salthouse.
The parish church is dedicated to All Saints and is a Grade I listed building built of greenstone, dating from the 14th century. Monuments inside the church include kneeling alabaster effigies to Sir Valentine Browne (d.1600) and Elizabeth (Monson) his wife, with their fifteen children in relief below. Its inscription states that Browne was "Treasurer and Vittleter of Barwicke and dyed (about 1600) Treasurer of Ireland". A related alabaster monument is to Valentine Browne's son John Browne (d.1614), and his wife Cicely (Kirkman). A further (ashlar) monument is to William Bonde (d.1559), erected by his son Nicholas, President of Magdalen College, Oxford. In the floor of the south aisle and chantry is a late 13th or early 14th century brass, the half effigy of a knight in banded mail. A tablet on the south side of the tower mentions a restoration of 1656; the church was again restored in 1857.
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Gibraltar Point national nature reserve is an area of about 4.3 km2 (1.7 sq mi) on the coast of Lincolnshire, England.
The reserve is owned by Lincolnshire County Council and East Lindsey District Council and is administered by the Lincolnshire Wildlife Trust. The reserve comprises two parallel ridges of sand dunes—the "east dunes" and the "west dunes"—separated by about half a kilometre (550 yards) of salt marsh; and an area on the seaward side with further salt marsh and sand, shingle and muddy beaches. The reserve extends for a distance of about 5 km (3 mi) along the coast, from the southern end of Skegness to the northern corner of The Wash (Gibraltar Point itself is at the southernmost tip, and marks the point where the North Sea coast turns southwest towards Boston). A golf course occupies much of the west dunes (the inland side) at the Skegness end of the area. Gibraltar Point is an area of coastal deposition—at the end of the 18th century the west dunes were by the shore, but they are now a kilometre inland.
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