Bouth

Rusland Pool is a small stream or beck running through the administrative county of Cumbria. Before 1974, Rusland Pool was in Lancashire. The source of Rusland Pool is to be found in Grizedale Forest Park, where several streams draining Monk Coniston Moor and Hawkshead Moor converge near Jack Gap Plantation (where Rusland Pool is known as Grizedale Beck). The beck then follows a southerly course through Grizedale Forest Park, flowing past the settlements of Grizedale and Satterthwaite (where it collects Farra Grain, becoming Force Back) and being joined by Ashes Beck at Rusland, taking its name from this settlement, before continuing its course through the Rusland Valley, before its waters join the estuarine River Leven at Pool Foot near Haverthwaite. The name of the stream has not always been Rusland Pool - John Speed's 1610 map of Lancashire records the name as Foße fl. (i.e. River Fosse - cf the tributary Force Beck). In 2007, otters were found to have returned to Rusland Pool after many years absence.

Holy Trinity Church is located to the east of the village of Colton, Cumbria, England. It is an active Anglican parish church in the deanery of Furness, the archdeaconry of Westmorland and Furness, and the diocese of Carlisle. Its benefice has been united with those of St Andrew, Coniston, St Luke, Torver, St Mary the Virgin, Egton-cum-Newland, and St Luke, Lowick. The church is recorded in the National Heritage List for England as a designated Grade II listed building.

Colton is a village and civil parish in the South Lakeland district of Cumbria, England. In the 2001 census the parish had a population of 765, decreasing at the 2011 census to 672. It was historically part of Lancashire. Its name has been recorded as Coleton (which is Old English for 'village') and Coulton, and its existence has been recorded as early as 1202.The village is in the historical district of Furness and within the boundaries of the Lake District National Park. It is about 2 km north of the A590 between Newby Bridge and Ulverston. The settlement is situated on an incline, at the top of which is Colton Church, which was built in 1575 and rebuilt 25 years later. Colton Beck, which runs beside the village, was once known as Cole, meaning 'hazel stream'. Three miles from the village there is an historic Quaker meeting house at Colthouse. The parish includes Finsthwaite, Lakeside, Oxen Park, Nibthwaite, Bouth, and Rusland within its boundaries.

Oxen Park is a hamlet in the English county of Cumbria. Oxen Park lies on the watershed between Rusland and Colton Beck valleys in South Lakeland, and is part of the greater Lake District region. The nearest town is Ulverston 7 miles (11 km) to its south. There are two former smithies (blacksmiths) here, dating from the late 17th/ early 18th century, both of which are Grade II listed buildings. The Manor House public house in Oxen Park was formerly Bank House, which was purchased by Hartleys brewery in 1933, later a Robinson's pub, and now a free house. The Reading Room (Village Hall) here was built in 1902, and underwent a major restoration in 2018/19.

The A590 is a trunk road in southern Cumbria, in the north-west of England. It runs north-east to south-west from M6 junction 36, through the towns of Ulverston and Barrow-in-Furness to terminate at Biggar Bank on Walney Island. The road is a mixture of dual carriageway and single carriageway, with the section east of Low Newton, Cumbria to the M6 being mainly dual. Further dual sections are south of Newby Bridge, south of Greenodd and south of Ulverston. The road is the main route for tourists entering the southern Lake District. It has often humorously been described as "the longest cul-de-sac in the world".

The River Leven (pron. LEV-ən) is a short river in the ceremonial county of Cumbria, falling within the historic boundaries of Lancashire. It drains Windermere from its southernmost point and flows for approximately 8 miles (13 km) into the northern reaches of Morecambe Bay. The river and its estuary are the boundary between the Cartmel Peninsula and Furness Peninsula and is part of North Lonsdale, also known as Lancashire North of the Sands. The upriver limit of tidal flow is close to the village of Haverthwaite. Also at this point is to be found Low Wood Bridge which, until the coming of the railways, was the first bridging point across the river. The Leven is navigable upstream as far as Low Wood, and downstream from Windermere to Newby Bridge. Apart from Newby Bridge and Haverthwaite, the only other settlements on the Leven are the villages of Backbarrow and Greenodd. The river's steep fall around Backbarrow allowed industrial use of the river for the ultramarine mill and also a small hydroelectric generator at Backbarrow ironworks. The River Leven has one significant tributary, Rusland Pool, which drains a substantial part of Grizedale Forest and the Rusland Valley into the upper tidal section of the river. The Leven is a noted salmon river. At spawning time the fish can be seen jumping up the waterfalls at Backbarrow. The river is popular with kayakers due to the continuous grade III+ rapids found between Newby Bridge and Haverthwaite and a relatively stable water level sustained by Windermere. In 1903 a train crossing the railway bridge over the river was derailed by high winds during the Ulysses Storm.The Leven Estuary is one of the six main estuaries in the traditional county of Lancashire.

Haverthwaite is a small village and civil parish in the Furness region of Cumbria, England. It is also within the boundaries of the Lake District National Park. It is located several miles east of Ulverston and is near the southern end of Windermere. In the 2001 census the parish had a population of 728, increasing at the 2011 census to 797.The village gets part of its name from the Old Norse word thwaite which usually refers to a clearing or settlement in the forest.

Rusland Hall is a country house in the English Lake District. The present building dates from about 1720. The Hall was owned by the Rawlinson family in the 17th and 18th centuries, and by the family of Beatrice Webb in the 19th century. For a time in the later 20th century it housed a museum of mechanical musical instruments, then becoming the home of Mike Dwan and his family.

The River Crake is a short river in the English Lake District. The name probably derives from the Celtic languages (most likely Brythonic languages; ie Cumbric language) and means rocky stream. The river drains Coniston Water from its southernmost point and flows for about 6 miles (9.5 km) in a southerly direction before joining the upper estuary of the River Leven at Greenodd. The river is in the historic county of Lancashire, but in an area that formed part of the county Cumbria after the 1974 reorganisation of local government. The villages of Water Yeat, Blawith, Lowick Bridge, Spark Bridge and Penny Bridge are located close to the river in the Crake Valley. As well as receiving the outflow from Coniston the river also drains Beacon Tarn in the Blawith Fells above the southern end of Coniston. In the 19th century numerous industries including a cotton mill and iron foundry flourished along the river, making use of the fast flowing water to drive machinery. A bobbin mill at Spark Bridge, which manufactured wooden bobbins for the Lancashire cotton industry, used water-powered lathes to turn the wood. The factory survived into the 1970s using Gilkes water turbines to generate electricity and turn the lathes. The factory was eventually forced to close by the punitive water usage charges levied by the North West Water Authority. Today there are no obvious signs of any of the riverside industries. The Crake is a noted salmon river. The River Crake is the model for the Amazon River in Arthur Ransome’s Swallows and Amazons series of children's novels according to Hugh Brogan, although the Crake flows out of Coniston Water but the Amazon flows into the Lake. The Allan Tarn at the beginning of the river became the Octopus Lagoon.

Spark Bridge is a former mill village in Cumbria, England, within the Lake District National Park, and within the historic boundaries of Lancashire. The village is situated away from the main road on the river Crake which flows from Coniston Water to Morecambe Bay at Greenodd. The village green which is next to and gives access to the river is in the middle of the village surrounded by well maintained white painted cottages.

Greenodd is a village in the Furness area of the county of Cumbria, England, but within the historical county of Lancashire. For local government purposes the village is also within the South Lakeland local area of Westmorland and Furness unitary authority. It is located 3 miles (5 km) north-east of Ulverston at the junction of the A590 trunk road and the A5092 trunk road. The village is just outside the boundary of the Lake District National Park at 54°14′N 3°3′W (OS grid ref. SD 315825). Greenodd was within the Crake Valley area of South Lakeland District. The 2001 UK census, gives a population of 1823 for the Crake Valley. Greenodd and adjacent Penny Bridge are the main districts in the Crake Valley. The River Crake flows into the estuary of the River Leven at Greenodd.

Haverthwaite railway station is a railway station on the preserved Lakeside and Haverthwaite Railway in Cumbria, England.