Top 5 Natural Monuments around Billingsley

The Wyre Forest Beaver enclosure is worth stopping at. Can't guarantee to see any but you never know 😁

Fine man-made lake, with an excellent view across to Dudmaston Hall. The path on the west side may be closed on Fridays and Saturdays, so best check.

Beautiful, peaceful, wildlife-rich pond set in National Trust parkland at Dudmaston.

Discover this tranquil little lake tucked away in the Shropshire Hills. The lake makes a great picnic spot, or if you're feeling daring, a wild swimming spot, too.

Worcestershire Natural Flood Management (NFM) Project in the Wyre Forest. The aim of this project is to reduce flooding in the Dowles Brook catchment, by implementing at large number of small scale, natural interventions in upstream areas to help slow the flow of water and hold it back during times of high flows. These measures involve working on the tributaries of the Dowles Brook and could include things such as planting hedges, creating wetland areas. attenuation ponds, leaky dams, soll aeration and other land management techniques The intention is to slow the flood peak on the Dowdes so it does not coincide with the flood peak on the River Severn at Bewdley. Water moving at speed through the landscape is incredibly destructive and leads to erosion, soil loss and widespread damage, therefore slowing down the water has a wealth of positive impacts. It is the intention that many more features will be installed over the riext few years with the aim of slowing the flow throughout the catchment. If you would like more information, or are a landowner who is keen to get involved. please contact the NFM Project Officer al Worcestershire County Council. www.worcestershire.gov.uk/NFM Natural Flood Management - Leaky Dams Trees are sourced from the immediate stream side and used to build a lattice. Over time, especially in high flow, smaller woody debris accumulates naturally, and this increases the effectiveness of the leaky dam. The dars are wedged behind living tree stumps to prevent them moving or floating away, over time they bed in and naturalise as part of the landscape. Leaky dams work with nature, providing a food source and habitat for wildlife. This timber lattice allows wildlife, such as fish, to move freely upstream and downstream. Leaky dams are constructed to allow free passage of water in normal flows, and only hold water back when required during high rainfall. The backed up water is pushed out of the channel into appropriate sites upstream where silts are deposited. A single structure has little impact, but a series of leaky dams at various locations can help reduce the risk of flooding downstream. Felling by the river bank allows more sunlight to reach the watercourse and its banks. This leads to the growth of marginal vegetation, creating further food sources and habitats for wildlife.

This area of the Wyre Forest Site of Special Scientific Interest belongs to John Ruskin's charity, the Guild of St George and is managed by the Wyre Community Land Trust. We are managing this area to support a mixture of high forest and heathland, which are valuable habitats for bats, birds and other species. In large areas of the woodland, the trees. are relatively young, and mainly comprise oak with bracken and bramble. This lack of diversity is a result of changes in woodland management following World War 1. when much of the woodland was no longer coppiced because of a collapse in the charcoal industry. In order to improve the habitat diversity, some trees have been removed to give those remaining more space to grow into large mature trees. The trees that are felled are extracted and processed at the Wyre Community land Trust's woodyard and sawmill at St George's Farm and used to make a variety of timber products and firewood. Volunteers have helped plant trees to ensure the forest has a diverse mixture of tree species that is more resilient to pests, disease and the effects of climate change.

Obviously not wild swim today, but a great spot to consider in the summer months, if wild swimming is your thing. https://myoutdoors.co.uk/adventure/dark-adventures-in-the-shropshire-hills-katy-goes-wild-swimming

The cutting is through beds of Highley Sandstone. They were deposited in the river channels on swampy deltas 310 million years ago. Their characteristic grey-green tinge indicates deposition in oxygen-poor conditions of a humid swamp. This is in contrast to the red Alveley Sandstone, seen earlier, formed in the oxygen-rich environment of a semi-arid desert. The pronounced 'bedding planes' running almost horizontally across the rock face, represent breaks in deposition. 'Cross-bedded' or 'current-bedded' layers are inclined at angles to each other. This cross cutting relationship is a result of changing directions in the river current that deposited the sediments, in the same way as changes in wind direction caused the dune-bedding seen in the Bridgnorth Sandstone