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Home > Lifestyle, Hobbies and Home > Nature and the natural world: general interest > A Comparative Study of the Vegetation of Swamp, Clay, and Sandstone Areas in Western Wisconsin, Southeastern Minnesota, Northeastern, Central, and Southeastern Iowa
A Comparative Study of the Vegetation of Swamp, Clay, and Sandstone Areas in Western Wisconsin, Southeastern Minnesota, Northeastern, Central, and Southeastern Iowa

A Comparative Study of the Vegetation of Swamp, Clay, and Sandstone Areas in Western Wisconsin, Southeastern Minnesota, Northeastern, Central, and Southeastern Iowa


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This historic book may have numerous typos and missing text. Purchasers can usually download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1905 edition. Excerpt: ...G. arundinacca, Phalaris arundinacea, Castilleia coccinea, Burnus kalmii and Campanula aparinoides, but especially of sedges. The Scirpus lacustris and other aquatic plants no doubt were the forerunners of the present marsh vegetation surrounding the pond. Nnphar, Nymphcea, and Nclumbo, aquatic plants of the Mississippi, do not occur. Nicholas Whitford,1 in describing the development of glacial swamps in northern Michigan, states as follows: "Most swamps start as ponds or lakes, in which water-lilies and other pond plants dominate. On the borders of the pond sedges appear; these, by their decay, build up a soil, and thus prepare the way for the next zone, the Cassandra-sphagnum vegetation. The sedges encroach farther on i. Bot. Gazette, 31: 313. the original lake. The Cassandra-sphagnum zone makes conditions possible for a tamarack-spruce zone. Thus each successive zone is pushed farther and farther toward the center. Finally the lily center disappears, and then successively the sedge and Cassandra zones, until a tamarack forest may come to occupy the whole territory." The bottom of the pond consisted of peat mixture lying on a brown sandy soil. The water is derived from perennial springs. The soil is not typical peat but a mixture of considerable humus and some sand. Two other typical swamp areas may be considered. One, a tamarack marsh in the town of Campbell. This was formed by the accumulation of sand and alluvium at the mouth of the present marsh, where it joins the La Crosse River. During times of high water this area was filled with water in which aquatic plants probably like Nuphar, Nymphcea, Scirpus, and Elocharis formed the principal vegetation. These by decay formed humus which gradually filled the lake and thus gave...


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Product Details
  • ISBN-13: 9781230136462
  • Publisher: Rarebooksclub.com
  • Publisher Imprint: Rarebooksclub.com
  • Height: 246 mm
  • No of Pages: 24
  • Spine Width: 1 mm
  • Width: 189 mm
  • ISBN-10: 1230136460
  • Publisher Date: 13 Sep 2013
  • Binding: Paperback
  • Language: English
  • Returnable: N
  • Weight: 64 gr


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