More information : (SK 17467096). CAMP (LB). Fin Cop (TI). (1) Fin Cop: A hill-fort with its north and west sides formed by the steep scarp above the Wye, and its east and south by two banks and ditches, the outer only preserved at the north end. A simple entrance is through the east side, 370' from the north end. (2) Plan (see Illust. card) (3) 160 yards outside the main work was another ditch and vallum. (4) Scheduled. (5) The only suggestion of Rooke's additional ditch and vallum on APs is a linear marking between SK 17707112 and 17707075; there are two ponds on it. (6) Resurveyed at 1/2500. The work has been badly robbed and mutilated by quarrying and agriculture, but along the whole east side there are evident footings of a strong stone-built rampart; these continue, but deteriorate, to the south-west. The outer rampart and ditch can only be traced at the north end. The entrance is inturned and strongly marked. The AP line between SK 17707122 and SK 17707075 marks a covered water main, and no evidence of Rooke's extra ditch and vallum was found. (7) Listed by Challis and Harding as an Iron Age hillfort, of 10 acres, with bank, ditch and counterscarp. (8) Additonal references. (9-10)
SK 175 710. Fin Cop. Listed in gazetteer as a multivallate hillfort covering 4.0ha. (11)
Additional references (not consulted). (12-13)
The Iron Age hillfort of Fin Cop is visible as earthworks on air photographs, centred at SK 1743 7101. The fort is visible on the west and south as large earthwork banks, with some areas of an external ditch visible. Centred at SK 1752 7101 is an entrance, defined by two large banks curving inward on the hillfort. The west and north limits of the hillfort are defined as very low relief banks and are only visible under snow cover in low light. Much of the southern half of the hillfort has been mutilated by limestone quarrying (UID 1465160), extraction pits (UID 1501137) and medieval ridge and furrow (UID 1501140). Within the limits of the fort a possible Bronze Age round barrow was also identified (UID 1501144). The feature is extant on the latest Google.Earth.com 12-SEP-2005 photography (accessed on 09-JUL-2009). (14-17) |