Rockingham Forest is a former royal hunting forest in the county of Northamptonshire, England. It is an area of some 200 sq mi (500 km2) lying between the River Welland and River Nene and the towns of Stamford and Kettering. It has a rich and varied landscape, with farmland, open pasture, pockets of woodland and villages built from local stone.
The Blisworth Limestone Formation is a geological formation primarily consisting of limestone deposited during the Bathonian stage of the Middle Jurassic, found in the Jurassic ridge which extends north and south through England. It was laid down in the shallows of the Jurassic sea and is part of the more widely defined Great Oolite Group. It was previously known as the Great Oolite Limestone, White Limestone and the Snitterby Limestone Formation. It is the lateral equivalent of the White Limestone Formation From the Jurassic ridge it extends eastwards below the later deposits and in the North Sea terminology, it is part of the West Sole Group.
Seatearth is a British coal mining term, which is used in the geological literature. As noted by Jackson, a seatearth is the layer of sedimentary rock underlying a coal seam. Seatearths have also been called seat earth, "seat rock", or "seat stone" in the geologic literature. Depending on its physical characteristics, a number of different names, such as underclay, fireclay, flint clay, and ganister can be applied to a specific seatearth.
Edenham is a village and civil parish in the South Kesteven district of Lincolnshire, England. It is approximately 3 miles (5 km) north-west of Bourne, and on the A151 road. While the civil parish is called 'Edenham', the parish council is called Edenham, Grimsthorpe, Elsthorpe & Scottlethorpe Parish Council. The population of the civil parish at the 2011 census was 291.
The Arundel Formation, also known as the Arundel Clay, is a clay-rich sedimentary rock formation, within the Potomac Group, found in Maryland of the United States of America. It is of Aptian age. This rock unit had been economically important as a source of iron ore, but is now more notable for its dinosaur fossils. It consists of clay lenses within depressions in the upper part of the Patuxent Formation that may represent oxbow swamp facies. It is named for Anne Arundel County, Maryland.
Careby Aunby and Holywell is a civil parish in the district of South Kesteven, south-west Lincolnshire, in England. It stretches from the county border with Rutland in the west to the River West Glen in the east. The B1176 road from Corby Glen passes through Careby and on past Aunby toward Stamford. The main London to Scotland railway line passes through the parish, the line upon which Mallard took the speed record for the LNER.
Wyrobki is a village in the administrative district of Gmina Mogilno, within Mogilno County, Kuyavian-Pomeranian Voivodeship, in north-central Poland.
Blisworth railway station was a junction station on the London and North Western Railway, the Northampton and Banbury Junction Railway, and the Northampton and Peterborough Railway. As well as providing interchange between the lines, the station served the village of Blisworth in Northamptonshire and its environs. The station was opened by the London and Birmingham Railway (L&BR) in 1838.
Roade was a railway station serving the Northamptonshire village of the same name on the West Coast Main Line. Roade Station opened in 1838 as the principal station for Northampton, but its importance diminished upon the opening of the Northampton and Peterborough Railway in 1845. The construction of the Northampton Loop Line in 1875 made Roade a junction station, and it survived until 1964.
Towcester was a railway station on the Stratford-upon-Avon and Midland Junction Railway which served the Northamptonshire, England, town of Towcester between 1866 and 1964. It was one of the most important stations on the line, and once served as an interchange for services to Stratford, Banbury and Olney. It also saw substantial traffic on racedays at Towcester Racecourse. Its closure came as the various interconnecting lines to the station closed one by one in the 1950s and 1960s. Passenger services ended in 1952, predating the Beeching closures.
The Stillwater River is an 11.5-mile-long (18.5 km) side channel of the Penobscot River in Maine. From its source in Old Town, the Stillwater runs 2.3 miles (3.7 km) northwest along the northeast side of Orson Island, the site of the Penobscot Indian Reservation. It then runs 9.2 miles (14.8 km) south along the west sides of Orson and Marsh islands, over three dammed falls. The stream rejoins the main stem of the Penobscot in Orono.
The Northampton Sand Formation, sometimes called the Northamptonshire Sand, is a Middle Jurassic geological formation which is placed within the Inferior Oolite Group. It was formerly worked extensively in Northamptonshire for its ironstone.
Lenton, Keisby and Osgodby is a civil parish in South Kesteven, Lincolnshire, England. The population of the civil parish at the 2011 census was 187. It is located along the river and in the valleys of the East Glen at its headwaters near Ingoldsby, where several minor streams join together.
Coombs Quarry is a 0.5 hectare Local Nature Reserve east of Buckingham. It is owned and managed by Buckinghamshire County Council.
Warboys Clay Pit is a 12.6 hectare geological Site of Special Scientific Interest west of Warboys in Cambridgeshire. It is a Geological Conservation Review site.
Thrapston Station Quarry is a 4.5 hectare geological Site of Special Scientific Interest south of Thrapston in Northamptonshire. It is a Geological Conservation Review site. It was formerly called the Thrapston Midland Railway Station Quarry.
Blisworth Rectory Farm Quarry is a 1.0 hectare geological Site of Special Scientific Interest west of Blisworth in Northamptonshire. It is a Geological Conservation Review site.
Finedon Top Lodge Quarry, also known as Finedon Gullet is a 0.9 hectare geological Site of Special Scientific Interest east of Wellingborough in Northamptonshire. It is a Geological Conservation Review site revealing a sequence of middle Jurassic limestones, sandstones and ironstones, and is the type section for a sequence of sedimentary rocks known as the 'Wellingborough Member'. It was created by quarrying for the underlying ironstone for use at Wellingborough and Corby Steelworks; the ore was transported by the 1,000 mm gauge Wellingborough Tramway.
Cranford St John SSSI is a 2.8 hectare geological Site of Special Scientific Interest in Cranford St John, east of Kettering in Northamptonshire. It is a Geological Conservation Review site.
The Woburn Sands Formation is a geological formation in England. Part of the Lower Greensand Group, it is the only unit of the group where it occurs, and thus is sometimes simply referred to as the 'Lower Greensand' in these areas. It was deposited during the late Aptian to early Albian stages of the Early Cretaceous. The lithology consists of sandstone or loose sand with rare wisps or thin seams of clay. The formation was extensively exploited in the 19th century for the "coprolite industry", with coprolite being a local term referring to phosphate nodules of varying origins, named due to their resemblance to real coprolites. The formation contains reworked fossils of late Tithonian-Berriasian age from deposits that are no longer found locally, equivalent in age to the Sandringham Sand Formation in Norfolk and the Spilsby Sandstone of Lincolnshire, these include Dicranodonta and the ammonite Subcraspedites. Reworked dinosaur material is known from the Potton locality within the formation.
England 
