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Historically, the parish of Cramond extended from the shore of the Firth of Forth in the north to the parish of [[Corstorphine]] in the south, and was bounded on the west by the parishes of [[Dalmeny]] and [[Kirkliston]] and on the east by the parish of St Cuthbert's.<ref name="geography">Wood (1794), p. 1</ref> It covered an area of fifteen square miles, and encompassed the villages of [[Granton, Edinburgh|Granton]], [[Pilton, Edinburgh|Pilton]], [[Muirhouse]], [[Davidson's Mains]], [[Blackhall, Edinburgh|Blackhall]], [[Ravelston]], [[Craigcrook]], [[Turnhouse]] and [[Craigiehall]].<ref name="parish boundaries">Brown (2000), p. 1</ref>
The area has a low, gently undulating [[topography]] that drops down from the top of Corstorphine hill to the shore in three gradual stages and is intersected by the River Almond which flows northward into the Forth.<ref name="topography">Cramond Heritage Trust (1996), p. 4</ref> [[John Philip Wood]] writing in 1794
The leaflet "Geological history of cramond" provides information about the geology of the cramond area such as that there is a coal seam visible near the beach on the south west side of the river almond estuary.<ref>"Geological history of cramond Edinburgh ... copyright 2014 lothian and borders geoconservation, a committee of the edinburgh geological society, a charity registered in Scotland. Charity no: sc008011. The cramond heritage trust is a charity registered in scotland. Charity no: sc000754”
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