UK UWMN Sites
Situated in the North York Moors, Danby Beck is a recent addition to the Network, with systematic chemical and biological sampling commencing in 2011. Surface water acidity data however has been collected since 1990 by Environet, a local volunteer group. The long-term historic pH record plus the site's geographical location in an area of high acid deposition, not originally represented within the UK AWMN, led to the decision to incorporate Danby Beck into the Network.
A sub-catchment in the headwaters of the River Esk, the 77 hectare Danby Beck catchment lies between an elevation of 299m at the sampling point/biological survey section and an altitude of 432m at the trig point to the south east.
The underlying geology is Jurassic, sedimentary and largely consists of two main formations, with another two present at the bottom of the catchment. Transitions between them broadly follow the contour lines of the valley. Capping the higher areas is sedimentary bedrock of the Scarborough Formation. Below this lie the undifferentiated sandstone, siltstone and mudstone of the Saltwick and Cloughton Formations. A thin band of Dogger Formation sandstone then overlies Whitby Mudstone, which is only present in the area immediately around the sampling station at the bottom of the catchment.
The site is highly designated. Both the Beck and the catchment lie within the North York Moors SAC, SPA, SSSI and National Park. The catchment also falls within the North York Moors Upland land Management Initiative, a Catchment Sensitive Farming area and is under Entry plus Higher Level Stewardship.
In the biological survey stretch the stream is approximately 1.5m wide, with a number of pools, riffles and small waterfalls. The substrate is a mixture of cobbles, pebbles, sand and gravel but there are also several areas of large boulders and exposed bedrock.
Page last modified: 3rd February, 2016