Working with partners, Nature After Minerals is here to offer and share best-practice advice on biodiversity-led minerals restoration.
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- Active Quarries
- Agriculture
- Arable
- Coastal
- Grassland
- Habitat Creation on Active Quarries
- Heathland
- Landscape Scale
- Open mosaic habitat
- Restoration Report
- Wetland
- Woodland
Artificial Rafts
Rafts are a useful way of providing island habitat in areas of deep open water, where the depth is greater than 45-50cm. Their purpose is to improve breeding success by providing areas safe from flooding, disturbance or predation.
Purple moor grass and rush pastures
This species-rich habitat occurs in areas of high rainfall, mostly in south-west England, on poorly drained, shallow peat or peaty mineral soils with a range of pH conditions. They have low available nutrient concentrations and are usually maintained by low intensity grazing or mowing.
Nature Before Minerals at Sandy Heath Quarry
Sandy Heath is an active sand and gravel quarry, adjacent to the RSPB’s headquarters and nature reserve at The Lodge in Bedfordshire.
Natural regeneration: Its role in mineral site restoration
Mineral sites provide excellent opportunities for natural regeneration and natural habitat succession. Once common in the wider countryside, these important ecological processes and the habitats they support are now limited due to changes in agriculture and an intensification of land use.
Lowland wood-pasture and parkland
Lowland wood-pasture and parklandis a woodland type that has developed through past management, rather than being a particular vegetation community. Where woodland has been grazed at moderate stocking levels for many years, it will develop an open park-like character.
Lowland meadows
Unimproved, semi-natural, neutral grasslands are rare – only 3% of the area of this species-rich grassland found in the UK in the 1930s remains. They are found on moist, low fertility, mineral soils with a pH of 5-7. Former mineral workings can be ideal opportunities for creation.
Lowland heathland
Lowland heathland is found below 300 m altitude, on generally sandy soils, which also contain botanically important valley mires. Former mineral workings can be ideal opportunities for creation. It will take several years for the full assemblage of heathland vegetation and features to develop, but a heath-like sward can be achieved in 3-5 years in favourable circumstances.
Lowland dry acid grassland
Unimproved, semi-natural, acidic grasslands occur on free draining, usually sandy, low fertility mineral soils with a pH of 3-5.5. Former mineral workings can be ideal opportunities for creation. The precise composition of the vegetation community will depend on the climate, aspect and particular soil characteristics. It will take several years for the sward to fully establish.
Lowland calcareous grassland
Calcareous grasslands occur on shallow chalk and limestone soils (pH 6.5-8.5). Former mineral workings can be ideal opportunities for creation. The precise composition of the vegetation community will depend on the climate, aspect and particular soil characteristics. It will take several years, once the grassland is established, for it to develop the full characteristics of the community.
Lowland beech and yew woodland
Lowland beech and yew woodland includes a number of similar woodland types, where beech is the common factor. They occur on both acidic and calcareous freely draining soils. Oak is a common associate on acidic soils, and ash and whitebeam on calcareous soils.
Case studies
Our Case Studies pages showcase the great work which is already being undertaken across the minerals and planning sectors to help enhance and protect the natural world and leave a lasting legacy for the benefit and enjoyment of future generations.
