Hi again all, Frittering away a bit more time on the ebird range maps for Swainson's Thrush, I came up with an alternative explanation of the crazily bouncing contours on the northern plains: There are a handful of very early SWTH reports from towns in SW Manitoba, as part of a generally sparse and strongly clustered dataset. Kriging based on these clustered points would probably produce the same phenomenon that I guessed was an edge effect. A large percentage of the North Dakota spring migration records seem to come from a few days of birding in a narrow strip along I-94 east of Bismark in May 2007 by three birders: Tim Lenz, Chris Wood, and Peder Svingen (perhaps a relative of Dan Svingen?). At each stop, all three recorded exactly the same counts as separate lists, tripling the weight of these observations. It's no wonder that the maps come out a little goofy, after feeding these data into a mathematical smoothing algorithm. Happy birding, Joel -- Joel Geier Camp Adair area north of Corvallis OBOL archives: www.freelists.org/archive/obol Manage your account or unsubscribe: //www.freelists.org/list/obol Contact moderators: obol-moderators@xxxxxxxxxxxxx