This paper takes a look at the geomorphology of the Bonnechere Caves.
Written in 2008; 2,313 words; 9 sources; MLA; $ 71.95
Paper Summary:
In this article the writer discusses the geomorphology of the Bonnechere caves in Eastern Ontario. Particularly, the paper examines the landscape features of the Bonnechere Caves and looks at what that appears to tell us about the forces acting upon the caves, the Bonnechere River and upon the Ottawa-Bonnechere corridor more commonly known as the Ottawa-Bonnechere graben. The writer then enters into a more detailed discussion of the formation of the caves themselves and how they have evolved over time. In the final analysis, the writer maintains that the Bonnechere Caves need to be situated within their proper geo-morphological context; that is to say, they must be understood as being - however notable - simply a simulacrum of enormously powerful tectonic and climactic shifts that re-formed the topography of Eastern Ontario long before the first humans arrived in the area.
From the Paper:
"Continuing onward, the landscape of the region also offers a peek at the isolation and undisturbed existence of the area for many millennia. To wit, given the geographic distance of the Bonnechere Caves, even today, from large metropolitan areas, it may be inferred that the landscape of the region was daunting and thus rarely penetrated by human beings; more than that, the boreal woodlands of the area were of such a nature that sedentary communities would have been largely impossible prior to the nineteenth century. Seen in that light, the pristine condition of the Bonnechere Caves until well into the nineteenth century is a tribute to the ability of natural geography to protect vulnerable ecologies and subterranean worlds from the depredation of humans."
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