Great Plains Studies, Center for
Date of this Version
August 1993
Abstract
Data collected during 1957-1989 on the Platte and North Platte rivers was analyzed to detect changes in the temporal and spacial distribution of staging sandhill cranes. The data indicate that a significant west-to-east shift in crane distribution has developed since the late 1960s. The most negative changes have occurred between Lexington and Kearney, Nebraska, where vegetation encroachment has been most pronounced. A significant increase in crane numbers between the Wood River and Highway 34 bridges is attributed to the result of vegetation scouring flows and active removal of woody vegetation.
Comments
Published in Great Plains Research 3:1 (August 1993). Copyright © 1993 The Center for Great Plains Studies, University of Nebraska–Lincoln. Used by permission. http://www.unl.edu/plains/publications/GPR/gpr.shtml