Skip to content

Mr. Johnny's Lake EarthCache

Hidden : 7/4/2011
Difficulty:
1 out of 5
Terrain:
1 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 location holds a special 4th of July memory for me, so I wanted to commemorate this beautiful area with an earthcache. Please take the time to sit and enjoy the lake while thinking about what went into creating it. Ample parking is available at this public park, and it is wheelchair accessible. This cache is named after the very nice man whom you will probably see sitting on the bench near the marker. Feel free to say hi to him!

Lakes are extremely varied in terms of origin, occurrence, size, shape, depth, water chemistry, and other features. Lakes can be only a few hectares in surface area (i.e., less than a square kilometer), or they can be thousands of square kilometers. Their average depth can range from a few meters to more than a thousand meters. Lakes can be nearly uniformly round, or they can be irregularly shaped.

Their water can be highly acidic (as in some caldera lakes), nearly neutral, or highly alkaline (as in soda lakes). Lakes can be low in nutrients (oligotrophic), moderately enriched (mesotrophic), or highly enriched (eutrophic). Lakes may be fresh-water or salt-water (saline). Fresh-water lakes contains less than 1 gram per liter of salt, whereas saline or hypersaline lakes, such as the Great Salt Lake (Utah), may contain more than 250 grams per liter. For comparison, sea water contains about 35 grams per liter. Saline lakes typically occur in arid climates, and occupy closed basins (low areas which lack stream outflow).

Lakes can be formed in many different ways. Below are listed a few of the more common types and methods of formation:
• Periglacial lake: Part of the lake's margin is formed by an ice sheet, ice cap or glacier, the ice having obstructed the natural drainage of the land.
• Glacial lake: a lake with origins in a melted glacier, such as a kettle lake.
• Artificial lake: A lake created by flooding land behind a dam, called an impoundment or reservoir, by deliberate human excavation, or by the flooding of an excavation incident to a mineral-extraction operation such as an open pit mine.
• Endorheic lake, A lake which has no significant outflow, either through rivers or underground diffusion.
• Crater lake: A lake which forms in a volcanic caldera or crater after the volcano has been inactive for some time.
• Lava lake: A pool of molten lava contained in a volcanic crater or other depression. Lava lakes that have partly or completely solidified are also referred to as lava lakes.
• Ephemeral lake: A seasonal lake that exists as a body of water during only part of the year.
• Intermittent lake: A lake with no water during a part of the year.

To log this cache, please email me the answers to the following two questions. As with all earthcaches, please do not include the answers in your log. The photo is optional, but I love to see them!

1) Based on the information above and the marker at this location, determine which type of lake this is.
2) Using the information on the marker, hypothesize how this lake came into being.
3) Optional: Take a photo of yourself with the lake in the background. Please do not take a picture of the information marker!

Additional Hints (No hints available.)