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The Deconsolidators: Trees EarthCache

This cache has been archived.

frograil: Am retiring from cache ownership, as I no longer am able to take care of my caches.

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Hidden : 8/2/2010
Difficulty:
1 out of 5
Terrain:
1 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

Park on the right, just before the small info building.  If the lot is full, go thru the gate, and there is room for several more cars on the right.



Trees?  Effectors of geological change?  You bet!  Trees cumulatively contribute mightily to the erosion of land mass.

Consolidated rock is a solid, coherent whole; anything that plays a part in deconsolidating rocks is a contributor to erosion.  Trees are thieves -- they steal sunlight, water, and minerals from the plants and soil under their leaves.  We will look at how erosion is aided by trees in a lawn, and then you'll have to answer logging questions concerning how trees effect deconsolidation in a more "natural" setting.

Paucity Ring

In this photo, you see what I call (my words only -- I'm sure there is a technical term for it) a paucity ring, because outside of it, organic detritis, minerals and water are abundant, but on the inside, the roots of the tree are sucking them out of the soil, and the grass and other plants face a paucity of the things they need in order to thrive.  If a hot, dry spell occurs, much of the grass inside the ring will perish. Grass and any other plants act to reduce erosion when it rains or the wind blows; remove the plants and the rate of erosion increases dramatically.  As you go further towards the trunk of the tree, to the left in this photo, more and more sunlight is blocked by the tree's leaves.

If you were blindfolded and barefoot, and walking from the right side of the photo to the left, your feet would tell you immediately when you had crossed the paucity ring. The grass is stiffer, sparse, and there are innumerable pebbles.

Inside the paucity ring

Here in the second photo, we're looking from further west of the tree, towards its trunk, which is about 18" across at chest level.  Immediately above "C" is the paucity ring at the top of the prior photo.  If you had followed the ring from top to bottom and clockwise in the first photo, the two spots labeled "B" would also be on the ring.  Finally, the line labeled A-A' consists of 4 yardsticks laid end to end.  What you can see is that there is little grass along and around this 12' length,  What you can't see from the photo is that the white areas (without any grass) are as much as 2 inches in elevation lower than those areas that still have grass.

Desertafication

This third photo is scary.  It is taken in a location similar to the previous one -- just two trees over.  It is obvious that any "topsoil" has been eroded away, and all that's left is a gravelly ground cover.  This so-called lawn is in serious trouble.  On a much wider scale, this process is called "desertification", and for good reason, as the countryside is on the way to becoming a desert.  Here, there is no danger of becoming a desert, but the area under this tree, and many, many millions like it in lawns around the country, are losing their topsoil to erosion, with trees being the culprit.  The only way to avoid this is to apply generous, constant amounts of water and nutrients (take a look at Augusta National Golf Course), but Mother Nature usually won't do that for us.

Newly exposed rock

To add insult to injury, photo four shows a rock, about 5" x 3.25" x 1.25" which has magically been uncovered and eroded out of the soil in the past three years.  It is harder than the surrounding rocks were, but now is exposed to weathering -- the boulders you'll be looking at shortly have been revealed by precisely the same process, just on a larger scale.

So, we've looked at the effect that trees in a lawn have on the underlying topsoil, but is that true in all lawns, or just the lawn in which the photos were taken?  Also, what about their effect on a more natural environment? Obviously, under natural conditions, no one comes along and mows the lawn regularly.  We will now look at two areas at the entrance to Morrow Mountain State Park.  The first will verify or refute what we inferred from the area in which the photos were taken, and the second will be "au naturale".

Other Educational Information:  

     Logging Questions:

Send me an e-mail – not part of your log – responding to the following:

1.  Make the first line of the e-mail “GC2CR55, The Deconsolidators:  Trees”

2.  How many people were in your party?

3.  From the parking area, walk across the road to the opening in the split rail fence, walk thru it, and then take a right.  Walk about 25 yards, and you'll see a 2-3' rock "emerging" from the ground.  Describe the soil in the vicinity of this rock, with regard to:

     a.  Vegetation

     b.  Slope

     c.  Estimate of depth of topsoil

4.  Walk back across the road to the paved parking lot, and walk to the first rocky outcrop (do not go to the one closest to the road -- go about 20' to the SSE (~210º)).  The outcrop looks kind of like a ship's bottom upside down.  Describe the soil in the vicinity of this rocky outcrop, with regard to:

     a.  Vegetation

     b.  Slope

     c.  Estimate of depth of topsoil

5.    Mental heavy lifting:

     a.  Here at the outcrop, try to describe the relationship between the trees, soil and exposed rock, as it relates to deconsolidation and erosion.

     b.  Besides the tree-aided erosion, what other erosion-aiding agents are present here at the outcrop?

6.  Optional:  Please post a photo of your party at the iconic info building at the entrance to the Park.



Note: For other EarthCaches in The Deconsolidators, the Gold Hill fault zone and mining district, and the Uwharrie Mountains series, go here.

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