Quaternary geology and environmental geochemistry of the Flin Flon Region, Manitoba and Saskatchewan.

Abstract

Your file Voire reference Our tile Notre refe'rence The author has granted a nonexclusive licence allowing the National Library of Canada to reproduce, loan, distribute or sell copies of this thesis in microform, paper or electronic formats. The author retains ownership of the copyright in this thesis. Neither the thesis nor substantial extracts from it may be printed or otherwise reproduced without the author's permission. L'auteur a accorde une licence non exclusive permettant a la Bibliotheque nationale du Canada de reproduire, preter, distribuer ou vendre des copies de cette these sous la forme de microfiche/film, de reproduction sur papier ou sur format electronique. L'auteur conserve la propriete du droit d'auteur qui protege cette these. Ni la these ni des extraits substantias de celle-ci ne doivent etre imprimes ou autrement reproduits sans son autorisation.

Regional subglacial quarrying and abrasion below hard‐bedded palaeo‐ice streams crossing the Shield–Palaeozoic boundary of central Canada: the importance of substrate control

“…It can be noted for example, that the Shield-Palaeozoic boundary on the floor of Lake Winnipeg is marked by a prominent limestone escarpment (Todd et al 1998); similarly, Hall et al (2020) draw attention to long escarpments of Palaeozoic carbonates on the floor and margins of the glacially scoured Baltic Basin in Scandinavia ('klints': Tuuling & Flod en 2001;Rattas & Kalm 2004;Hall & Van Boeckel 2020). McMartin (2000) mapped the Reed Lake Moraine along the S-PBz of the Flin Flon Region of northern Manitoba and Saskatchewan (B in Fig. 14) and its description closely resembles the Dummer rubble terrain described herein.…”