Aire Gap

Geologically the Aire Gap lies between the Craven Fault and the limestone uplands of the Yorkshire Dales to the north and the Forest of Bowland and the millstone grit moors of the South Pennines. The South Pennines is the system between the Aire Gap and the Peak District. The gap was formed by the dropping of the Craven Faults in the Carboniferous through Jurassic periods combined with glacial scouring by ice sheets in the Pleistocene Ice Age. The Aire Gap splits the Pennines into north and south by allying with the River Ribble. The Pennine chain is divided into two sections by the Aire Gap formed by the River Aire flowing south, a member of the Humber basin, and the Ribble flowing west and entering the Irish sea. ==Geography==

The term Aire Gap is used in both Ribblesdale and Pendle to denote a hypsograph (watershed) between those rivers and Airedale. Two locations are so described: • Ribblesdale's Aire Gap designates a precise point at just east of Hellifield near Settle at , and is labelled Aire Gap on some maps. It is the watershed of that pass and lies between the "Little" North Western Railway and the A65 road. • The head of Pendle Water valley culminates in Foulridge near Colne. In literature Colne commonly describes itself as being in the Aire Gap. When the Leeds and Liverpool Canal was being constructed they dug a tunnel at altitude beneath Foulridge's to make a route even lower than the 160m pass near Hellifield. ==Transport route==

The Pennines form a natural barrier to east–west communications, but the Tyne Gap links Carlisle and Newcastle and the Aire Gap links Lancashire and Yorkshire. Its extent is vague, a 19th-century author wrote: The Aire Gap is of considerable strategic importance and historically Skipton Castle controlled the area. Skipton is now considered more central to the Aire Gap than terminal. ==Topography==

or the Aire Gap. These contrast with the heights of the mountains of the Yorkshire Dales National Park to the north shows as a blue line, and also with the heights of the Forest of Bowland and the South Pennine Moors to the south marked as a yellow line. The treeless moorland gives no shelter and modern Pennine transport can find it a formidable barrier when roads are blocked by snow for several days. The Aire Gap route is a sheltered passageway, and inhabited along its length. The Aire Gap was of topographic significance for the historic North of England providing a low-altitude pass through "the backbone of England". It was the Pennine transport corridor from Cumbria and Strathclyde to the Vale of York. Neolithic long-distance trade is proved by many finds of stone axes from central Cumbria. To the north stand limestone hills of up to above mean sea level and to its south lie bleak sandstone moors, that above grow little but bracken. The builders of the "Little" North Western Railway sought the lowest course through the Aire Gap and found that to be near Giggleswick scar at , and just east of Hellifield at a point labelled Aire Gap on maps. to the north that climbs to and its climate is classed as sub-arctic in places. == References ==