A previously unrecognized path of early Holocene base flow and elevated discharge from Lake Minong to Lake Chippewa across eastern Upper Michigan
It has long been hypothesized that flux of fresh meltwater from glacial Lake Minong in North America's Superior Basin to the North Atlantic Ocean triggered rapid climatic shifts during the early Holocene. The spatial context of recent support for this idea demands a reevaluation of the exit poi...
Main Authors: | , , , , , |
---|---|
Format: | Text |
Language: | unknown |
Published: |
NMU Commons
2014
|
Subjects: | |
Online Access: | https://commons.nmu.edu/facwork_bookchapters/59 http://specialpapers.gsapubs.org/content/508/1 |