ABSTRACT: The internal architecture and timing of development were determined for 29 beach ridges from the Baileys Harbor embayment, at the Ridges Sanctuary, Wisconsin. Elevations of foreshore sediments were used to determine the relative elevations of Lake Michigan when each ridge formed. To determine the age of the ridges and the timing of their development, 12 peat samples were dated from basal wetland sediments between ridges. A least squares regression was calculated through these dates to assign ages to unsampled wetlands. In this study, it is assumed that the age of the base of the wetland is a minimum age for the ridge lakeward of it. Ridges were found to have formed between 1050 and 250 calendar years before present (B.P.). The foreshore deposits between ridges in the Baileys Harbor embayment are nearly horizontal and show only a slight lakeward decrease in elevation of about 1.75 ft along the entire transect. The elevations of most basal foreshore deposits are at or near the historical average for Lake Michigan during the development of the entire strandplain, suggesting that the Baileys Harbor embayment is at or very near the zero isoline that extends through the Port Huron outlet for Lakes Michigan and Huron. The Coordinating Committee on Great Lakes Basic Hydraulic and Hydrologic Data (1977) showed that the Platte Lake embayment (studied during one year of this project) has experienced roughly the same vertical uplift as the Baileys Harbor embayment. Therefore, data from these two sites can be combined producing a longer relative lake-level curve. Similar to the other sites studied, the average timing of development of a single beach ridge is about 30 years. Rises and falls in foreshore elevations of 1.5 to 4 ft among four to six ridges occur in the data. The foreshore elevations show five groups, although the fourth group in the series is not well defined. The rise and fall in foreshore elevations are interpreted to indicate a longer-term and possibly larger amplitude quasi-periodic variation of about 150 years. Similar groups were observed at all of the study areas examined in this research program.
Thompson, T. A., Baedke, S. 1995, Preliminary report of Late Holocene lake-level variation in northern Lake Michigan: part 4: Indiana Geological Survey Open-File Study 95-14, 13 p.
Notes: Publications in the Indiana Geological Survey Open-File series have been inconsistently named using a variety of series titles including "Open-File Report," "Open-File Map," and "Open-File Study." Prior to 1994, a publication in this series was generally referred to as an "Open-File Report" (but not always). To help reduce confusion created by these inconsistencies, the IGS now refers to every publication in the Open-File series as an "Open-File Study." To be entirely correct in writing a bibliographic reference for a publication, one should use the series name and number that appears on the publication itself.
You may also like:
Can't find what you're looking for? Feel free to contact us directly:
Publication Sales Office
Indiana Geological and Water Survey
420 N. Walnut St.
Bloomington, IN 47404
IGS Return Policy
All sales are final. Materials may not be returned after they have been accepted by the customer. Any discrepencies in mail orders must be reported to IGWS within 10 days of receipt of order.
The Indiana Geological and Water Survey will refund the purchase price and sales tax of products if returned with the original sales receipt within 10 days of receipt of order. Refunds will be issued with the same method of payment as indicated on the original receipt except for cash purchases, which will be refunded by check. Items must be returned in the same condition as purchased. Refunds on digital products and services are not allowed, except for defective media such as CD-ROMs, flash drives, and so on. The customer is responsible for paying shipping costs to return items.