Monday, January 12, 2009
Another post from that really cold early morning in mid-December. Kayak Point, like Lowell Point, Cama Beach, Breezy Point, Onamac Point, and several others, is some blend of a recurved spit, cuspate foreland, or, the term I prefer, looped barrier. The beach diverges from the coastline at the barrier's updrift end (always the south, in these examples) and then reconnects with the coastline a mile or so north, gradually merging back with the bluff. They inevitably had some sort of lagoon behind them. At some sites there may have been a tidal inlet. At Kayak Point, the remains of the old ebb tide delta are still visible on the lower beach north of the pier.
The bluffs to the south were dripping with icicles. There are some nice lakebed clays in these bluffs and the chunks that occasionally fall onto the beach in big piles display nice varves (laminations), marking the passing of individual years at the bottom of the big lake before the great glacier arrived from the north. Or at least I think that's the correct order of events.
From a warmer day, back in 2007: Kayak Point