Journal Entry 3

Journal Entry #3


11/15/2020


It seems like I’m able now to actually understand what I’m looking at when looking at the soil of forests! I recall covering in class relatively recently that there are certain ways to identify new forests from old forests; this is also, quite often, and indicator of not only age but how recently natural forest fires may have happened.

In my last entry, I made note that the soil of the wheeling trail seems very compact, and I found as I examined my area more that this was kind of a consistent feature of this tiny bit of landscape. The soil wasn’t all that loose, it seemed very compact in most areas; even the hollows around this spot, all the way to the banks of the Ashuelot, aren’t that dense with underbrush.

I think I have to conclude, essentially, that I am again seeing a major sign of constant human interaction in this area. I would assume natural fires might be the cause for the lack of “swishy” soil, or that perhaps the area is young, but I know the area isn’t that young; all of Keene, after all, is essentially a relatively old flood plain. Instead, it’s possible I’m still seeing the remnants of old fires from colonial and revolutionary eras, and the contemporary residents are simply utilizing it in a different fashion!


Comments

Popular posts from this blog

Journal Entry #2

Journal Entry 1 / Journal Paper