Skip to content

Soils of RI #32: Rainbow EarthCache

This cache has been archived.

Twohig260: There are no plans to reopen this soil pit. Fortunately, another Rainbow pit is open at the nearby URI campus. A new Earthcache has been submitted to replace this cache. Finding either this cache or its replacement will count towards earning a place on the "SoRI Hall of Fame" found at SoRI Survivor Series: Bjm3rd Tribute.

More
Hidden : 8/11/2011
Difficulty:
3 out of 5
Terrain:
2 out of 5

Size: Size:   not chosen (not chosen)

Join now to view geocache location details. It's free!

Watch

How Geocaching Works

Please note Use of geocaching.com services is subject to the terms and conditions in our disclaimer.

Geocache Description:

This is the 32nd in a series of caches honoring the 58 different types of soils found within the State of Rhode Island. Soils were a major factor in the settling and early farming of RI, and soils continue to influence our industry, recreation, wildlife, and homes. As you complete this series, please take note of how the soil is determined in-part by the landscape position (summit, sideslope, drainageway), which in turn affects the vegetation.

As I have written in previous SoRI cache descriptions, soils are important natural features on our landscape. One of the most obvious influences soils have on humans is that we build our homes and businesses on and in soil. However, not all soils are wel suited to development. One of the most significant limitations to development is the depth to the seasonal high water table (SHWT). The SHWT is the minimum depth to free water in a soil. This depth changes throughout the year. The water table is at its deepest during late summer, as plants have actively drawn water up through their roots all summer. Water tables rise during the fall and winter and reach a maximum during the spring.

In RI, most homes have basements, and many have septic systems. Rising water tables can flood basements (as many, including myself, witnessed during the March 2010 floods) and impair septic systems. Floods like those in 2010 are uncommon, but what about soils that regularly have a water table that comes to within 20" of the soil surface? This land would be unsuitable to build upon. Is there any way a landowner or developer could determine know how high the water table gets within a soil?

The answer is yes. Rising water tables typically leave signs called redoximorphic (redox) features. These features come in two forms - concentrations (rust colored), and depletions (gray soil particles). See the included picture for an example. To keep this simple, these features are basically areas where iron has moved within the soil profile. Soil evaluators can examine a soil profile and find the depth at which redox features first appear. This gives an excellent estimate to the SHWT.

This Earthcache is placed within an area of Rainbow soil. Rainbow soils are not suitable for development because the parent material is dense till, an unsorted mixture of soil materials that was compressed under the massive weight of glaciers 14,000 - 18,000 years ago. This material is extremely difficult to dig through. It also "perches" infiltrating water, causing a high water table. This Earthcache will give you some experience in describing a soil profile and identifying the features that make Rainbow unsuitable for development.

Your Assignment:

You will need: A measuring device (a roll tape will work best) and a small trowel, knife, or shovel to help you clear the profile and obtain samples.

The posted coordinates will bring you to the northwest corner of an old field. You should see some orange snowfencing around an excavated area approximately 4 feet deep. Use caution going down the slope. There is a wooden pallet at the bottom of the pit to stand on, and there is plenty of room for several people to stand. The bottom foot or so of this pit may fill with water during the winter and spring. I do not advise anyone to attempt this cache if there is water in the pit!

Clear off the soil face, and measure the distance from where the grass meets the soil to where you see a very obvious color change from very dark brown to a more yellowish brown. This layer is the A horizon. It is dark because decaying plant material is a major component of this soil layer. Record the depth of this soil layer.

Next, begin digging small clods of soil from the orange soil materials (B horizon) below the A horizon with your knife or trowel. Break open the clods and look carefully for rust colored redox features. Once you find these features, carefully continue higher in the soil profile to make sure they do not appear higher. Record the depth that the redox features first appear in the soil profile. This is the estimated depth of the SHWT!

You will notice a strange "seat" of gray soil material further down. This is the dense till parent material (C horizon). Record the depth at which the dense till appears in the soil profile. You'll notice just how dense this material is if you try to dig into it!

Congratulations! You just performed some real-life soil evaluating! To log your find, you must answer all three bold questions and email them to me. Do not post any answers in your log.

Congrats to BBWolf+3Pigs for the FTF!

Additional Hints (No hints available.)