THE KINGSTON PLAINS Logging and milling had begun in earnest between 1830 and 1840. In general, the pine lands and the central, southern, and eastern areas were logged first and most completely, and were then subject to damaging fires which followed. These were the drier sites which had most pine to begin with, and were so situated and continuous as to be in the paths of many fires which raced from west to east with the prevailing winds. These were also the areas in which ill-advised agricultural efforts, encouraged by land speculators, stimulated land clearing by early settlers. Patches of timber of varying size, protected on the west by either open water or wet swamps, or to a lesser extent, hardwood sites, escaped some of the fires which swept around them, but sooner or later many of these burned too. Northern hardwood (maple, beech, basswood) forests seem to have suffered less from the combination of drastic cutting and fires. Swamp conifer stands, in wet sites, were least subject to loss from fire. Settlers were not tempted to clear these wet lands for farming. Once the old white pines were cut from the swamps, in many places natural regeneration and growth followed, resulting in the continuation of the forest conditions. Forest fires in many extensive areas not only killed the trees and consumed the thin mantle of topsoil and eliminated every possible source of seed or sprouts to bring back the previous forest. In some areas, notably parts of Kalkaska, Missaukee, Crawford, Osceola, Wexford, Luce and Clare counties, even today areas of fire-charred pine stumps on otherwise almost barren sand plains are to be found. The Kingston Plains is an excellent example of this type of landscape. Early farming efforts, many of which failed, were responsible for completely denuding land, which was then (of course!) later abandoned. After the great logging era of the late 1800's, most of the
pine lands were piled with "slash" -- branches and drying wood scraps. These
quickly burned, and often repeatedly burned. The image below shows the Kingston Plains in 1968. Source: Image Courtesy of Loren Berndt And again, here (below) is what the landscape looked like in 1995. It is still a
stumped landscape! Source: Photograph by Randy Schaetzl, Professor of Geography - Michigan State University The real question is, "Why has this landscape not revegetated?" Geographer
Linda Barrett studied this question and concluded that the "pure" white pine
areas were so vast and the slash must have burned so hot in those areas, that few trees
(and hence, few seeds) were left to provide for new seedlings. Also, the fires were
probably so hot in this area that the soil---dry, infertile, and sandy to begin
with---literally "cooked" itself.
Source: Photograph by Randy Schaetzl, Professor of Geography - Michigan
State University
Source: Photograph by Randy Schaetzl, Professor of Geography - Michigan
State University This material has
been compiled for educational use only, and may not be reproduced without
permission. One copy may be printed for personal use. Please contact
Randall Schaetzl (soils@msu.edu)
for more information or permissions. |