Thanks, curious what creates it. Up to 8 or 9" now, on a ridge with eastern exposure so drifting is an issue. Band seems to reform overhead with good inflow from GOM still showing. Hopefully it expands west to get you into the goods.
What creates that attenuation angle running thru Sanford down to Rochester-Dover? Looks like the heart of the band extends Farmington to well off Kennebunk including under that attenuated wedge?