The Caaf Water in western Scotland (Keaff in 1747 also Caff) drains from the Caaf Reservoir above Dalry which is fed from Knockendon Reservoir. The Caaf Water's origins are springs below Green Hill and it is joined by the Bught Burn, the Reeves Burn, the Bradshaw Burn and the Stock Burn, passing the old Bradshaw (previously Broadshaw) shooting lodge before passing the old farms of Knockendon, Birkheadsteel, and Birkhead.
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The Tower Burn entering the Caaf Water near Drumastle mill and Peden's Pulpit
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Peden's waterfall and rock-cut basin near Drumastle Mill
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Peden's Pulpit at Pinnoch or Pinnioch (meaning Many Points) Point on the Caaf Water
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The other possible Peden's pulpit or point in the Lynn Glen
At Giffordland Bridge the old Giffordlandmill is passed before the Caaf joins with the Caddell Burn and Tower Burn near Drumastle and enters the Lynn Glen with its picturesque spouts or waterfalls and finally enters the River Garnock south of Dalry.
Read more about Caaf Water: Drumastle Mill, Lynn Glen, The Natural History
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—Henry David Thoreau (1817–1862)