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A series of unless info 7: Lightning Traditional Cache

This cache has been archived.

Chuck Walla: Greetings from your Community Volunteer Reviewer,

Geocaching HQ flagged this cache as one that may need attention and sent you an email about it. Some time after that, I disabled your cache and requested that you check on your cache and perform any necessary maintenance. Since you have not responded to my reviewer log about your cache, nor did you post a note to your cache page telling me and others of your intention to address the issue with it, the cache has been archived at the direction of Geocaching HQ.

If you address this issue in the near future, please contact me. I can always unarchive the cache for you if needed.

Sincerely,

Chuck Walla
Community Volunteer Reviewer
Geocaching.com

Reply to: chuck.walla@hotmail.com
Please send the name of the cache and the GC code with your reply.

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Hidden : 6/12/2009
Difficulty:
1 out of 5
Terrain:
1 out of 5

Size: Size:   small (small)

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Geocache Description:

This one will hit you like a ton of rocks when you find it. It is a small container... It won't hold a whole lot. There is No Pen or pencil.This is a dawn to dusk cache. CONGRATS TO DareGuy and ParaPro for FTF!

Lightning is feared by most and admired by the rest. I have used many different things in my series. My favorite phrase used by many that know me is, "Don't try to understand her, just love her". I find a lot of different things interesting. I have spent hours upon hours following link after link after link on subjects that just tickle my fancy. A lot of the information I use to make the descriptions for these caches are found in different areas, but mostly I use Wikipedia. I have chosen to do this one on lightning because I fall in the latter category. Lightning is an atmospheric discharge of electricity. It is usually accompanied by thunder. Typically lightning will occur during thunder-storms, but also occurs during a volcanic eruption and dust-storms, as well as violent forest fires (which generate sufficient dust to create a static charge). A leader bolt, in the atmospheric discharge can travel at speeds of 60,000 M/S, and reach temperatures as high as 54,000 degrees Fahrenheit (hot enough to fuse Silica Sand into glass channels, known as Fulgurites). Some lightning strikes have particular characteristics. Scientist and the general public have given names to the various types.
1) Cloud to Ground Lightning is the best known and the second most common type. Of all other lightning the cloud to ground poses the greatest threat to life and property. This type is a discharge from a cumulonimbus cloud and the ground. It's initiated by a leader stroke moving down from the cloud.
2) Bead Lightning is a type of cloud to ground lightning. It appears to break up into strings of short, bright sections, which last longer than the usual discharge channel. This type is relatively rare. One theory, as to why this type is rare, is that the width of the lightning channel varies, as the channel of lightning cools and fades the wider sections take longer to cool, making them visible longer, appearing as a string of beads.
3) Ribbon Lightning occurs in thunderstorms with high cross winds and multiple return strokes. The wind blows each successive return stroke to one side of the last return stroke, causing a ribbon effect.
4) Staccato lightning is a cloud to ground strike that is a short duration stroke that appears as a single very bright flash and often has considerable branching.
5) Fork Lightning is a name not in formal usage. It refers to the cloud to ground lightning that exhibits branching.
6) Ground to Cloud lightning is much rarer than the ground the cloud to ground lightning. It is a discharge between the ground and a cumulonimbus cloud, initiated by a leader stroke that is moving upwards.
7) Cloud to Cloud Lightning is when lightning discharges occur between areas of cloud without contacting the ground. When it occurs between two clouds it’s know as inter-cloud lightning. When it occurs between areas of differing electric potential within one cloud it is known as intra-cloud lightning, this is the most frequently occurring type.
8) Sheet Lightning is an informally applied name of cloud to cloud lightning that exhibits a diffuse brightening of the surface of a cloud. It’s caused by the actually discharge path being hidden.
9) Heat Lightning is sheet occurs too far away for the thunder to be heard. This happens because the sound dissipates before it reaches the observer. 10) Dry Lightning is a term in the US that is used when lightning occurs without precipitation at the surface. It is the most common natural cause of wildfires.
11) Rocket Lightning is a form of cloud discharge, generally horizontal and at cloud base, with a luminous channel that appears to advance through the air with visually resolvable speed, often intermittently.
12) Positive Lightning makes up less than 5% of all lightning. It occurs when a leader forms at the positively charged cloud tops, with the consequence that a negatively charged streamer issues from the ground. Research shows that positive lightning is 6 to 10 times more powerful than negative bolts, and lasts around 10 times longer. The results of their greater power make them much more dangerous.
13) Ball Lightning is believed to be an atmospheric electrical phenomenon, which the physical nature is still controversial. It is referred to luminous, usually spherical objects, that vary in size. From pea sized to several meters. Ball lightning usually can last for several moments, unlike lightning flashes that on last a few seconds, at best. It is associated with Thunder-storms.

Additional Hints (Decrypt)

haqre n "ebpx" arkg gb fbzrguvat erq

Decryption Key

A|B|C|D|E|F|G|H|I|J|K|L|M
-------------------------
N|O|P|Q|R|S|T|U|V|W|X|Y|Z

(letter above equals below, and vice versa)