Last night, I heard the first calls of courting Woodcocks from
the prairies of Blue Jay Barrens. This
was a reminder to me that I had to complete my winter mowing before the female
Woodcock began selecting nesting sites.
I only planned on mowing about two acres this winter and should have
completed that back in November.
However, frequent rains and warm temperatures kept some of the areas too
wet and soft to mow without making a mess.
I found myself with about an acre left to mow as we entered
February. This is one of the larger
areas, the valley though which one of the main trails begins.
At one time, this valley was choked with Smooth Sumac and a
hefty dose of Multiflora Rose. Removal
of the shrubs allowed prairie vegetation to move into the area.
The deep soil of the valley supports a healthy population of
Monarda. The flowers attract a wide
range of butterfly and moth species during the summer. Soil depth decreases rapidly as you leave the
valley. The slope in the background has
less than a foot of soil over the bedrock.
Indian Grass crowds this section of trail. As it grows, it leans into the open
area. The leaning grass was trimmed back
several times during the late summer to keep the trail open. Heavy snow sometimes bends the grass towards
the trail, but our precipitation this year has been primarily rain, so the
Indian Grass has remained upright.
The contours of the valley are easy to see following a
mowing. The steep hillsides terminate
suddenly into the flat valley floor. Underlying
limestone bedrock follows the grade of the hillsides and continues that same
angle to a point beneath the valley center.
Soil eroded from the hillsides has been trapped in the valley, gradually
changing the shape from a sharp V to a gentle bowl.
A strange feature of this valley is the fact that a large
portion of the storm runoff water travels through channels below the
ground. Under certain conditions you can
hear the water rushing beneath your feet.
The water all emerges at the head of a stream farther down the
valley. Seasonal springs also discharge
through this same system, but at a much lower volume. The springs normally flow from January to
July.
The sumacs cleared from this valley produced several large
brush piles. The remains of one can
still be seen just right of center in the photo. This pile remains because it contained several
rot resistant Eastern Red Cedars along with the sumac. Piles of all sumac, one of which was in the
center of the photo behind the crooked Ash and another just downhill from the
cedar on the left, decomposed quickly and disappeared back into the soil.
I don’t mow the fields every year, but I always take at
least one pass along the trail edges.
This keeps the dead grass stalks, which will eventually fall, from
dropping out into the trail. A couple of
years ago, I began blowing the cut grass onto the trail in an attempt to
increase organic matter and nutrient cycling.
After 25 years of maintaining this trail with a lawn mower, I had unintentionally
subjected it to a type of management known as soil impoverishment. This is where you continue to remove
vegetation and the nutrients it contains, without replacing the loss with soil
additives. Over time, this activity
diminishes the supply of essential elements required for plant growth and
plants grow poorly. Each time I mowed,
the cut grass was blown into the edge of the field. Eventually, the grass on the trail began to
thin out and the grass at the field edge prospered. Trail grass seems to be responding well to my
new strategy.
With the mowing comes the flags marking woody invaders that
need to be removed in order to protect the desired mix of plant species. Control of woody vegetation is the reason
these areas get mowed. Red flags mark
small trees that need to be killed. Most
of these flags are marking Black Walnut seedlings that grew from nuts produced
by those Black Walnut trees showing in the foreground.
Only one patch of nasty invasives in this mowing. A clump of young Multiflora Rose. I suspect the seeds came from a bird that
rested in this tree. My encounters with
non-native invasives become more rare each year. It’s a nice thing to see happening. I should finish my mowing tomorrow and hope to
see just as few non-native invasives then.
Nice set of pictures. They give a good sense of what part of the property is like.
ReplyDeleteHi, Stew. This shape is typical of the low gradient valleys near the upper end of the watershed. As grade increases, the valley shape becomes more narrow and V shaped.
DeleteDo you know what kind of rock is under your property? I am curious as to whether you "hearing the water rushing beneath" is possibly some sort of small cave.
ReplyDeleteHi, Jared. The bedrock beneath the valley is dolomite, but the rock is a couple of feet lower than the flowing water. The water is moving through the soil in a channel not more than two feet below the surface. The path of the water is marked by several blow holes formed by water under pressure escaping to the surface. If you clear the dead vegetation from a hole, you can see the flowing water. The situation is similar to a deteriorating clay tile subsurface drainage system, but there was never any tile here.
Delete