This message is truncating…

This message is truncating.

Which is weird.

It doesn't like the Niagara Escarpment.  It really doesn't like the NE.

Niagara Escarpment important recharge area in Melancth water surplus recharges the dolostone Aquifers upgradient of the 455 m asl contour Escarpment slope spring line. The local water surplus is equivalent to 30 to 40% of the dry season base flow at Wasaga Beach. The late summer dry weather flow observations in the Pine River Valley above Terra Nova are about 1,000 L/sec, further downstream at Everett at about 750 L/sec and in the Nottawasaga River at Edenvale upstream of Wasaga Beach at about 5,000 L/sec. Downstream losses on the Pine River valley are likely due to recharge and groundwater underflow at stream gauging stations and near Everett due to agricultural irrigation withdrawals.

Note:  The underlying data and groundwater elevation charts are available upon request.

[Original Comment ID: 213464]