That's correct, Larry. When spring runoff hits, the water will carry silt further down lake, dropping it throughout more of the reservoir, but the bulk of it drops where the rivers and washes hit the still water. And of those, nothing drops more than the Colorado. The north end up around Trachyte and White canyons is getting totally hammered with silt from it. As you move farther down lake and into the deeper parts, the water just gets more and more clear because the silt doesn't have any more flow to push it down there. When floods hit, all of the canyons contribute, of course, but nothing like the big rivers do.