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©Hugh Mortimer
Dist:0.2km<br/>In the 18th and 19th centuries, when lime was extensively used on acid clay soil to improve cultivation, lime kilns were widespread. Beehive shaped, with a hole in the top, kilns were usually built on the sides of steep hills and against cliff faces, to make the loading of limestone and coal easier. Alternating layers of limestone and coal were burnt to produce the lime.
©Trish Steel
Dist:0.3km<br/>Gradually disappearing under a thick coat of moss.
©Christine Johnstone
Dist:0.3km<br/>A lime kiln in a reasonable state of preservation situated close to the B6270 between Gunnerside and Satron. The kiln is at the lowest point of access land which stretches from the roadside to the top of Satron Moor.
©Gordon Hatton
Dist:0.4km<br/>
©Andy Beecroft
Dist:0.4km<br/>At this point the Swale undercuts its left bank and has caused some footpath problems here. Beyond are houses on the 'sunny side' of Swaledale at Dyke Heads and Shore Gill. Most settlement along this narrow dale tends to be on the north side, where houses could be built to face the sun.
©Gordon Hatton
Dist:0.4km<br/>Jigsaw pastures in a bend of the Swale.
©Christine Johnstone
Dist:0.5km<br/>
©Bob Edmonds
Dist:0.5km<br/>
©Andy Beecroft
Dist:0.5km<br/>Why does one field encircle another on the banks of the Swale? Has the river changed its course? Is the drainage very different nearer the river's edge?
©Christine Johnstone
Dist:0.5km<br/>Unusually, on the southern shady side of Swaledale.
©Christine Johnstone
Dist:0.5km<br/>The bridge DOES slope steeply.
©Bob Jenkins
Dist:0.5km<br/>
©Hugh Mortimer
Dist:0.5km<br/>The hamlet is blessed with a telephone box. At first I thought it was in a garden but it is beside a very small road to other houses and barns.
©Trish Steel
Dist:0.5km<br/>The Swale's northern bank has been recently reinforced with large stone blocks.
©Christine Johnstone

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