From Scotland's Golf Courses by Robert Price.
Esker - ridge formed by glacial meltwater streams from 5 to 50 feet high with irregular crest lines.
Kame - glacially formed mounds of sand and gravel.
"Eleven golf courses (three per cent) are located on fluvioglacial sand and gravel in the form of kames or eskers"
"The golf courses at Dumfries, Castle Douglas, Lochmaben, Carnwath, Lanark, and Muckhart are located on kame complexes with associated kettle holes."
Anyone play any of these? Are they any good? Did the architect make good use of the kames?
"... the famous golfing centre of Gleneagles, where four courses have been developed on a large esker and kame complex, that these sand and gravel deposits form a distinctive golfing landscape. The ridges are 20 to 50 feet high, steep-sided (20-25o) and are separated by elongated troughs or enclosed hollows (kettle holes)." ... "The golf course architects have utilized the ridges for "rough" and tees and the inter-ridge troughs and hollows for fairways and greens."
How good is Gleneagles? The author suggests that esker and kame complexes are a good approximation to dunes at links courses, because they form shapes like dunes and the drain well too. Were these "pseudo-dunes" at Gleneagles used as well as dunes and good links courses? If you think they fall short of true dunes, in what fashion do they fall short?
With 50 foot high, steep-sided roughs bordering fairways in troughs, do any holes approximate the trough holes between dunes at Astoria CC?