A bit of trail trivia for you. First I’ll post some pictures to see if anyone volunteers an answer as to what’s going on in them. I’ll put the answers at the end of this post. Click on the pics to enlarge.
Here is another version:
Something different. What caused all these cracks?
Seen on the side of the slope.
Why did this tree fall?
What is this?
You can probably guess this one.
Why are these embedded rocks smooth and round?
1, 2 and 3: When I first noticed this phenomenon some years ago I was momentarily stumped. What is happening is that on windy days the branches and stems touching the ground are being swept back and forth creating this half-circle pattern in the dirt. In the first one, it actually dug grooves in the ground. This was after that very windy day that I mentioned in a previous post. 4. This is sandstone, a relatively soft rock. When it rains and is simultaneously freezing weather, water gets into the cracks and then expands. This is called Frost Wedging. 5. and 6. Rain falling steadily from the leaves of trees above create this little pitting pattern on the sides of slopes below. You can see where small rocks and a long stem shielded the ground under them. 7. The precipitator was a long soaking rain that softened the ground enough. Strong wind can do it too. 8. Strata, layers of sand laid down horizontally, then subsequently thrust up by geologic action. These layers are like pages in the book of time. 9. Beaver :-B 10. These common rocks, like many people find on trails well inland, have been eroded by the action of water and time. It is constant rolling in ocean waves over the sea bed and on beaches, and inland in rivers and streams, helped by the abrasive action of flowing sand and rubbing against each other that rounds off the edges of once hard edged rocks. Of course over time the shoreline can advance or recede, sometimes hundreds of miles and rocks may be buried. Later the land may be thrust up at odd angles by earth movement, and those rocks, once buried, re-exposed.