Question: Thorne and Hatfield Moors form the largest area of lowland raised peat bog in the United Kingdom, they are situated in South Yorkshire, to the north-east and east of Doncaster near the town of Thorne, and are part of which low-lying area in South Yorkshire and North Lincolnshire, England, which was often flooded?
Context: Burns Bog is an ombrotrophic peat bog located in Delta, British Columbia, Canada.  It is the largest raised peat bog and the largest undeveloped urban land mass on the West Coast of the Americas.  Burns Bog was originally 10000 – before development.  Currently, only 3,500 ha remain of the bog. Wheatley Hills is an urban suburb of Doncaster located a mile outside of the town centre in South Yorkshire, England.  Wheatley means "wheat fields" in old English, located at the eastern end of the central ridge that runs through most of the town.  The surrounding region was often flooded in the times before the River Don was rerouted and extra drainage channels dug, and lies on the old floodplain of the Don, which peaked at today's Thorne Road.  Originally the suburb was part of the Wheatley ward of Doncaster but due to the expansion of housing during the post war era and boundary changes, the area became a separate area in its own right. Thorne and Hatfield Moors Peat Canals were a series of canals in South Yorkshire and Lincolnshire, England, which were used to carry cut peat from Thorne and Hatfield Moors to points where it could be processed or exported.  There were two phases to the canals, the first of which lasted from the 1630s until the 1830s, when coal imported on the Stainforth and Keadby Canal reduced the demand for peat as a fuel.  The second started in the 1890s, when peat found a new use as bedding for working horses, and lasted until 1922, when Moorends Mill which processed the peat was destroyed by fire. Doncaster (St. James' Bridge) railway station was situated in the Hexthorpe area of Doncaster, South Yorkshire, England and was accessed from St. James' Bridge, the main road link between Doncaster town centre and the railway community of Hexthorpe.  The station was a little nearer Doncaster than the South Yorkshire Railway's Doncaster (Cherry Tree Lane) railway station being less than a mile south of the main station, adjacent to the Sheffield line. Doncaster ( or ), is a large market town in South Yorkshire, England.  Together with its surrounding suburbs and settlements, the town forms part of the Metropolitan Borough of Doncaster, which had a mid-2016 est. population of 306,400 .  The town itself has a population of 109,805.  Historically part of the West Riding of Yorkshire, Doncaster is about 17 mi north-east of Sheffield, with which it is served jointly by an international airport, Doncaster Sheffield Airport in Finningley.  In recent years, it was also discovered that Doncaster belongs to Scotland by technicality in light of ancient agreements laid out in the Treaty of Durham, but this is not formally administered.  The Doncaster Urban Area had a population of 158,141 in 2011 and includes Doncaster and neighbouring small villages. Hatfield Chase is a low-lying area in South Yorkshire and North Lincolnshire, England, which was often flooded.  It was a royal hunting ground until Charles I appointed the Dutch engineer Cornelius Vermuyden to drain it in 1626.  The work involved the re-routing of the Rivers Don, Idle and Torne, and the construction of drainage channels.  It was not wholly successful, but changed the whole nature of a wide swathe of land including the Isle of Axholme and caused legal disputes for the rest of the century.  The civil engineer John Smeaton looked at the problem of wintertime flooding in the 1760s, and some remedial work was carried out. Thorne and Hatfield Moors form the largest area of lowland raised peat bog in the United Kingdom.  They are situated in South Yorkshire, to the north-east and east of Doncaster near the town of Thorne, and are part of Hatfield Chase.  They had been used for small-scale extraction of peat for fuel from medieval times, and probably much earlier, but commercial extraction of the peat for animal bedding began in the 1880s.  The peat was cut on the moors and, once it had dried, transported to several works on narrow gauge tramways, always called trams locally.  The wagons were pulled by horses to works at Creyke's Siding, Moorends, Medge Hall, Swinefleet and Hatfield.  There was also a network of canals supplying the Moorends Works. The Swinton–Doncaster line is a short railway line in South Yorkshire between Swinton Junction on the Wakefield Line and Doncaster South Yorkshire Junction on the East Coast Main Line.  The line comprises the former North Midland Railway's "Swinton curve" between Swinton and Mexborough and the east end of the former South Yorkshire Railway Blackburn Valley line, between Mexborough and Doncaster.  Northern operates passenger trains on the line; TransPennine Express and CrossCountry use the line but do not provide stopping service. Hatfield Colliery, also known as Hatfield Main Colliery, was a colliery in the South Yorkshire Coalfield, mining the High Hazel coal seam.  The colliery was around 1 mi northwest of Hatfield, South Yorkshire, adjacent north of the railway line from Doncaster to Scunthorpe (former South Yorkshire Railway, or "Barnsley to Barnetby Line") northeast of Hatfield and Stainforth railway station. Thorne (Old) railway station was the second railway station built by the South Yorkshire Railway to serve the town of Thorne, South Yorkshire, England.  It was situated near the town centre on the first stage of the canal-side line to Keadby, which was opened in September 1859.  The new line left the original South Yorkshire Railway just before arriving at Thorne Waterside taking a right-handed junction towards the town centre.  When the line opened this station was the terminus of the line.
Answer: Hatfield Chase