Spring Saturation Points
March 29, 2014
There was more rain, more pooling of water. We'd had enough warmer days for the ground to
finally thaw, so water was able to seep into the ground instead of running
across the surface.
Seeds buried in the ground, waiting through the long winter,
were able to absorb moisture, swell, and send down root, then send up stalk.
Roots could find their way around soil particles, gathering
nutrition with the help of water. Almost
overnight, new plants were sending up stems and unfurling leaves,
Jewelweed
Waterleaf just beginning
Waterleaf further along
some had developed flower buds,
Spring Beauty
Cut-Leaved Toothwort
Prairie Trillium in bud
and some were blooming.
Mosses were turning bright green and succulent,
and some getting a head start by growing sporophytes.
Mushrooms, too, were softening, or developing from latent
spores in the warmer, wet environment.
Snails found this environment very habitable, too.
The Creek was flowing steadily and musically as the spring
songs of birds darted from various parts of the woods.
The Pond-like Place was prominent again.
Cottonwood Pond was full.
In fact, it was well overflowing from the northwest corner into the
Seep, which was full of water all the way to the Creek.
I hopped onto the Very Rotten Log and used it to walk
over to the pond. I could feel the
softness of the rotting wood through my soles and heard a slight squish as my
boots squeezed a little water from the spongy decay.
I had a better view of the Seep, and saw a
spot of green near the log.
More mud was piling up under the root ball at the north end.
Here is a view of the south end of the pond. The Very Rotten Log continues along the
edge. It has served almost as a border,
but I noticed that there was also water on the other side of the log, at its
far end. The Young Maple stands at the edge with its feet in the water, acting
as a good measuring device for changing water depth. The Bent Blue Beech, with it clinging amber
leaves, arches gracefully over the pond near the far end (its top, not seen
here, leans on the root ball). The
Barkless Log serves as a border for the south end of the pond, with the Very
Rotten Log extending under and beyond it.
I saw a “light at the end of the tunnel” below the
intersection of the Very Rotten Log and Barkless Log. Had the New Inlet become even wider? Also, there was more water under the Barkless
Log near the Root Ball, and a glimmer of light below the log there, too. Last time, I had suspected that a Newer Inlet
was forming from the rush of excess water.
I went to the other side of the pond and Barkless Log to have
a look.
A stream of water was flowing down to the pond, and the
New Inlet appeared wider. But, water had
spread to either side and did appear to be creating a Newer Inlet to the right,
and possibly another to the left (Newest?).
The Very Rotten Log was extremely rotten at this end, appearing to
gradually melt into the ground. The
excess water that had been rushing and pooling in this area was surely
expediting that process. And, that
left-most possible inlet, to the left of the Very Rotten Log, was showing more
space and light under the log, as I had noticed from the other side.
I looked to the East and saw that there was still a
temporary creek, of sorts, flowing along the base of the slopes and heading
toward Cottonwood Pond. I am sure water
was seeping down the slopes and gathering in that “creek”.
And, yes, the New Inlet, alongside Very Rotten Log, had
most definitely become wider. In fact,
it looked more as if the pond was beginning to extend beyond Barkless Log.
Nearby, Crawdad chimneys were saturated with water down in
their holes.
Nearer the Root Ball, I had a close look at Newer
Inlet, where water was certainly increasing.
Looking between the fork of Barkless Log, I had a good
view of the increasing amount of water in the corner, as well as an increase in
the pile-up of mud, both at the corner of the pond and root ball and on top of
the log, where it surely was washing off and collecting below.
An abundance of water was also flowing along the slope
bases toward the Fallen Cottonwood Trunk.
There was more water here than what was flowing toward the new inlets of
Cottonwood Pond.
Water flowing under the trunk was running or seeping
into “little pond”, at the topside of the Root Ball.
In fact, so much had flowed to this area that “little
pond” had greatly increased in size since lat year. It was extending beyond the trunk and across
the ground around it.
The whole area was well saturated. Silas gingerly
walked his light body over the place, but I could not walk here without my
boots sinking and leaving pools of water.
Here, a Bush Honeysuckle has taken hold. I must remove this very invasive species and
all other of its kind from these woods, or there will be nothing but Bush
Honeysuckle. It is interesting, though,
to wonder what would happen if this particular area became filled with this
kind of plant. Would the roots drink up
much of the water, and the plants serve as a catchment for soil and debris,
turning the space into a comparatively drier place? Interesting, but not an experiment that I
will allow to happen.
Again, “little pond” and Cottonwood Pond had become
linked around the north end of the Root Ball.
Water was gathering around the Two-Trunk Tree, spilling into the larger
pond, and then spilling into the Seep, on its way to the Creek. Previous to this visit, the water had been
higher. I have seen it that way before,
when this “isthmus” between ponds was so great that it seemed like one big
circled-around pond.
view of the Seep, north end of Cottonwood Pond,
“isthmus”, and north edge of “little pond”.
view of Cottonwood trunk, root ball and surroundings
from up hill, looking southwest.
Looking at this place as a whole, seeing what has happened to
it and how it has changed, has brought to mind new questions:
–
How far might Cottonwood Pond extend beyond its
south edge?
–
How much more will those three inlets enlarge,
and what affect would this have on the pond? Will the divisions between inlets
someday disappear?
–
How far might “little pond” extend beyond the
trunk, and beyond its other banks? Will
it someday be as large as Cottonwood Pond?
–
How much more rain will we have during the rest
of the year? Or, will we have another
drought this summer? After the great
influx of water so far this winter and early spring, how much would drought
bring down the pond's water level (compared to last summer's “Cottonwood
Puddle”)?
–
I do think that there has been an increase in
the tilt of the Root Ball toward Cottonwood Pond, and that this tilt has been
caused by the Root Ball (and trunk base) sinking further, due to immense
saturation of the ground below. How much
more would this happen? How much farther might it all sink? As the Root Ball
tilts farther and creates more of a sheltered, dark area, how might this affect
how wildlife (frogs, birds, water insects, etc.) use the area?
–
Will there someday be no distinction between a
Cottonwood Pond and “little pond”? Will
there someday be one big, round pond with a sunken Cottonwood root ball
“island” in the middle? Will it become “Cottonwood Pond” and “Cottonwood
Island”?
–
Or, will the whole thing, someday, become
“Cottonwood Swamp”?
New names for use in the blog: New Inlet, Newer Inlet, Two-Trunk Tree.
Possible future names: Newest Inlet, The Isthmus, The Influx,
The Temporary Creek
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