Late Pleistocene diatoms from the Trempealeau Valley, Wisconsin by George William Andrews

Cover of: Late Pleistocene diatoms from the Trempealeau Valley, Wisconsin | George William Andrews

Published by U.S. Govt. Print. Off. in Washington .

Written in English

Read online

Places:

  • Wisconsin,
  • Trempealeau Valley.

Subjects:

  • Diatoms, Fossil -- Wisconsin -- Trempealeau Valley.,
  • Paleontology -- Pleistocene.,
  • Paleontology -- Wisconsin -- Trempealeau Valley.

Edition Notes

Bibliography: p. 23.

Book details

Statementby George W. Andrews.
SeriesGeological Survey professional paper;, 523-A., Contributions to paleontology, Geological Survey professional paper ;, 523-A., Geological Survey professional paper.
Classifications
LC ClassificationsQE75 .P9 no. 523-A
The Physical Object
Paginationiii, 27, [8] p.
Number of Pages27
ID Numbers
Open LibraryOL4066481M
LC Control Number79604966

Download Late Pleistocene diatoms from the Trempealeau Valley, Wisconsin

LATE PLEISTOCENE DIATOMS FROM THE TREMPEALEAU VALLEY, WISCONSIN By GEORGE w. ANDREWS ABSTRACT The Trempealeau Valley trends in a generally southwestward,direction across the Driftless Area of west-central Wisconsin!between the central Wisconsin lowland and the Mississippi 'Valley.

It contains an upper Pleistocene alluvial fill. Rem­Cited by: 5. Get this from a library. Late Pleistocene diatoms from the Trempealeau Valley, Wisconsin. [George William Andrews] -- A late Pleistocene diatom assemblage from west-central Wisconsin and its paleoecologic and stratigraphic significance.

R.B. Owen, R.W. Renaut, R. Potts, A.K. BehrensmeyerGeochemical trends through time and lateral variability of diatom floras in the Pleistocene Olorgesailie Formation, southern Kenya Rift Valley Quaternary Research, 76 (), pp. Cited by: Late Pleistocene diatoms from the Trempealeau Valley, Wisconsin.

Geological Survey Professional Paper, Contributions to Paleontology (A) pp., pls. ANDREWS, G.W. [ref. New names for late Pleistocene diatom species. The Wisconsin Valley and Langlade Lobes of the Laurentide Ice Sheet formed when the southern flank of the Superior Lobe spilled southward over a high bedrock divide and into north-central Wisconsin ().This divide is underlain by early and middle Precambrian volcanic and metasedimentary rock that is part of the Wisconsin dome (Morey et al., ; Mudrey et al., ).

The l and post-glacial diatom succession in the Kentmere Valley deposit. New Phytologist, 56, The diatoms of a core from Esthwaite Water. Barrett, S.A.,Field studies for the Catlinite and Quartzite groups: Year Book of the Public Museum of the City of Milwaukee, v. 4, p. Beard, R.,Wisconsin’s Quartz Hill – Precambrian gems sparkling in the North Woods: Rock and Gem, v.

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The wide flat-bottomed valley occupies a broad structural depression between the volcanic arc of the Cascade Range to the east and the uplifted marine sedimentary and volcanic rocks of the Coast Range to the west (Gannett and Caldwell, ).

INTRODUCTION, pages ix - xv CONTENTS (the following items will be added and linked here as they are transcribed) CHAPTER 1 - EARLY WISCONSIN, pages 1 - 16 CHAPTER 2 - GEOLOGY, pages 17 - 25 CHAPTER 3 - ARCHAEOLOGY, pages 26 - 35 CHAPTER 4 - GOVERNMENTAL JURISDICTION, pages 36 - 40 CHAPTER 5 - REIGN OF THE INDIANS, pages 41 - 51 CHAPTER 6 - EXPLORERS AT TREMPEALEAU.

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POST‐PLEISTOCENE DIATOM SUCCESSION IN DOUGLAS LAKE, MICHIGAN, POST‐PLEISTOCENE DIATOM SUCCESSION IN DOUGLAS LAKE, MICHIGAN, Stoermer, E. ABSTRACT Analysis of fossil diatom assemblages recovered from a m core reveals a series of distinct floristic associations. The associations present are correlated with sediment type.

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