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The Regents of the University of Colorado, a body corporate, contracting on behalf of the University of Colorado at Boulder for the benefit of INSTAAR Errata: The Glaciation Level and Lowest Equilibrium Line Altitude in the High Canadian Arctic: Maps and Climatic Interpretation Source: Arctic and Alpine Research, Vol. 7, No. 3 (Summer, 1975) Published by: INSTAAR, University of Colorado Stable URL: http://www.jstor.org/stable/1549996 . Accessed: 23/06/2014 02:17 Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at . http://www.jstor.org/page/info/about/policies/terms.jsp . JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. . INSTAAR, University of Colorado and The Regents of the University of Colorado, a body corporate, contracting on behalf of the University of Colorado at Boulder for the benefit of INSTAAR are collaborating with JSTOR to digitize, preserve and extend access to Arctic and Alpine Research. http://www.jstor.org This content downloaded from 91.229.229.218 on Mon, 23 Jun 2014 02:17:42 AM All use subject to JSTOR Terms and Conditions

Errata: The Glaciation Level and Lowest Equilibrium Line Altitude in the High Canadian Arctic: Maps and Climatic Interpretation

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The Regents of the University of Colorado, a body corporate, contracting on behalfof the University of Colorado at Boulder for the benefit of INSTAAR

Errata: The Glaciation Level and Lowest Equilibrium Line Altitude in the High CanadianArctic: Maps and Climatic InterpretationSource: Arctic and Alpine Research, Vol. 7, No. 3 (Summer, 1975)Published by: INSTAAR, University of ColoradoStable URL: http://www.jstor.org/stable/1549996 .

Accessed: 23/06/2014 02:17

Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at .http://www.jstor.org/page/info/about/policies/terms.jsp

.JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range ofcontent in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new formsof scholarship. For more information about JSTOR, please contact [email protected].

.

INSTAAR, University of Colorado and The Regents of the University of Colorado, a body corporate,contracting on behalf of the University of Colorado at Boulder for the benefit of INSTAAR are collaboratingwith JSTOR to digitize, preserve and extend access to Arctic and Alpine Research.

http://www.jstor.org

This content downloaded from 91.229.229.218 on Mon, 23 Jun 2014 02:17:42 AMAll use subject to JSTOR Terms and Conditions

FORTHCOMING ISSUES WILL INCLUDE FORTHCOMING ISSUES WILL INCLUDE

Geology of Umnak Island, Eastern Aleutian Is- lands, as Related to the Aleuts. R. F. Black

Postglacial Isobases and Uplift Curves from the High Canadian and Greenland Arctic. J. E. England

Cirques as Glacier Locations. W. L. Graf

Characteristics and Genesis of Some Subalpine Podzols (Spodsols), Banff National Park, Al- berta. R. H. King and G. R. Brewster

Geoecological Investigations on the Timberline of Pico de Orizaba, Mexico. W. Lauer and D. Klaus

The Energy Balance of a Mid-Latitude Alpine Site during the Growing Season, 1973. E. F. LeDrew

Geology of Umnak Island, Eastern Aleutian Is- lands, as Related to the Aleuts. R. F. Black

Postglacial Isobases and Uplift Curves from the High Canadian and Greenland Arctic. J. E. England

Cirques as Glacier Locations. W. L. Graf

Characteristics and Genesis of Some Subalpine Podzols (Spodsols), Banff National Park, Al- berta. R. H. King and G. R. Brewster

Geoecological Investigations on the Timberline of Pico de Orizaba, Mexico. W. Lauer and D. Klaus

The Energy Balance of a Mid-Latitude Alpine Site during the Growing Season, 1973. E. F. LeDrew

Ice-Blocked Tubes in the Aiyansh Flow, British Columbia. P. Marshall

Beach Freeze-up Sequence, Radstock Bay, N.W.T., Canada. S. B. McCann and R. B. Taylor

Morphology and Genesis of Soils on the Prairie Divide Deposit (Pre-Wisconsin), Front Range, Colorado. R. G. Reider

Detritus Transport by Wind in a High Arctic Ter- restrial Ecosystem. J. A. Teeri and P. E. Barrett

Influence of Late-lying Snow on Rock Weathering Rinds. C. E. Thorn

Hydrochemical Analysis to Discriminate Variable Runoff Source Areas in an Alpine Basin. L. J. Zeman and H. 0. Slaymaker

Tree-ring Record of Soil Movements on Perma- frost. S. C. Zoltai

RATA

Ice-Blocked Tubes in the Aiyansh Flow, British Columbia. P. Marshall

Beach Freeze-up Sequence, Radstock Bay, N.W.T., Canada. S. B. McCann and R. B. Taylor

Morphology and Genesis of Soils on the Prairie Divide Deposit (Pre-Wisconsin), Front Range, Colorado. R. G. Reider

Detritus Transport by Wind in a High Arctic Ter- restrial Ecosystem. J. A. Teeri and P. E. Barrett

Influence of Late-lying Snow on Rock Weathering Rinds. C. E. Thorn

Hydrochemical Analysis to Discriminate Variable Runoff Source Areas in an Alpine Basin. L. J. Zeman and H. 0. Slaymaker

Tree-ring Record of Soil Movements on Perma- frost. S. C. Zoltai

RATA

Vol. 7, No. 1, 1975, p. 85. Fig. 1 Location No. 18. General Location should read Pangnirtung hamlet.

Vol. 7, No. 2, 1975, p. 157, Col. 1, line 16, and Col. 2, line 5 Equation should read bW + b8 = 0.

Vol. 7, No. 1, 1975, p. 85. Fig. 1 Location No. 18. General Location should read Pangnirtung hamlet.

Vol. 7, No. 2, 1975, p. 157, Col. 1, line 16, and Col. 2, line 5 Equation should read bW + b8 = 0.

This content downloaded from 91.229.229.218 on Mon, 23 Jun 2014 02:17:42 AMAll use subject to JSTOR Terms and Conditions