Kirriemuir (/ˌkɪriˈmjʊər/ KIRR-ee-MURE, Scots: [ˌkɪreˈmeːr, -møːr]; Scottish Gaelic: Ceathramh Mhoire [ˌkʲʰɛɾə ˈvɔɾʲə]), sometimes called Kirrie or the Wee Red Toon, is a burgh in Angus, Scotland, United Kingdom.
The playwright J. M. Barrie was born and buried here and a statue of Peter Pan is in the town square.
Glamis /ˈɡlɑːmz/ is a small village in Angus, Scotland, located 5 miles (8 km) south of Kirriemuir and 5 miles (8 km) southwest of Forfar. It is the location of Glamis Castle, the childhood home of Queen Elizabeth the Queen Mother.
A Wendy house, in the United Kingdom, is a children's playhouse that is large enough for one or more children to enter. Size and solidity can vary from a plastic kit to something resembling a real house in a child's size. Usually there is one room, a doorway with a window on each side, and little or no furniture other than what the children improvise.
The original was built for Wendy Darling in J. M. Barrie's play, Peter Pan, or The Boy Who Wouldn't Grow Up. Wendy was shot by the Lost Boy Tootles after arriving in Neverland, so Peter Pan and the Lost Boys built a small house around her where she had fallen. It was inspired by the wash-house behind Barrie's childhood home in Kirriemuir and first appeared in story form in The Little White Bird in which fairies build a house around Mamie Mannering—the prototype for Wendy—so protecting her from the cold.
A kame, or knob, is a glacial landform, an irregularly shaped hill or mound composed of sand, gravel and till that accumulates in a depression on a retreating glacier, and is then deposited on the land surface with further melting of the glacier. Kames are often associated with kettles, and this is referred to as kame and kettle or knob and kettle topography. The word kame is a variant of comb (kame, or kaim is the Old Scottish word meaning 'comb'), which has the meaning "crest" among others. The geological term was introduced by Thomas Jamieson in 1874.
According to White, "kames were formed by meltwater which deposited more or less washed material at irregular places in and along melting ice. At places the material is very well washed and stratified; at others it is more poorly washed, with inclusions of till masses that fell from ice but were covered before they were completely washed. Kame gravels thus tend to be variable and range from fine to coarse grained and even to cobbly and boulder."