This preview shows pages 1–2. Sign up to view the full content.
This preview has intentionally blurred sections. Sign up to view the full version.View Full Document
Unformatted text preview: The debris that was on the ground was mainly dead leaves and fallen branches from the trees above. The soil was a rich, dark color indicating high amounts of accumulated organic matter from the heavy O horizon. If you look closely at the trees, you can see a faint line in all the trees where a color change occurs, indicating an elevated lichen line of where water reached at one point in time. There was probably more to see further into the creek, but with the elevation changes it was too dangerous to go wander down. The downward slope sends sediment and any surface runoff towards the bottom when it rains, therefore any hydrologic indicators on the ground may have already washed off....
View Full Document
This note was uploaded on 12/16/2011 for the course SWS 4244 taught by Professor Clark during the Spring '11 term at University of Florida.
- Spring '11