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Herkimer Diamond Quartz Crystals:
Quartz in general
This quartz specifically
When, How & Why
Where
The Crystals
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Picking & Rating when buying
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Novice Digging
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Glossary (the first use of these words is " * " starred*)
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More Herkimer Facts
Herkimer Diamond Quartz Crystals:
Herkimer Diamonds are a uniquely beautiful, natural occurrence* of quartz that come only from a small area around Little Falls, NY. Though there are quartz crystals roughly similar in appearance and occurrence from several other locations throughout the world they really never match the brightness and clarity of actual Herkimer Diamonds. I cannot count the number of times I've explained to stunned and disbelieving people that these sparkling crystals are natural, not cut and not polished.
Quartz in general:
Before we talk more about Herkimers or Herkimer-like crystals, let me say something about quartz crystals in general: Unless you count water-ice, quartz is by far the most common mineral on the surface of Earth; yet quartz is so varied it's often unique enough that you can tell exactly where, sometimes within meters, on/in the surface of this planet it is from! I'm not going to list any different types of quartz crystals or other types of quartz here, it would never be complete anyway; suffice it to say most quartz crystals are found in dirt/clay or in volcanic rock and have prisms* that are several to many times longer than wide, often with one termination* and the other end of the prism attached to matrix* or broken from it.
Photos of some other types of quartz, from left to right: Druze* quartz crystals over Chrysocolla, Citrine crystal with Mica, Cross section of amethyst/agate geode, detail of same. Likely all of the above photoed quartzes are volcanic or hydrothermal. The amethyst makes an excellent example of volcanic formation since it is essentially a horizontal cross-section of crystals that precipitated* within a gas bubble that became trapped in lava, first as it cooled quickly the very small crystals that combine to make up the banded agate at the outer edge coated the inside of the bubble followed by the larger amethyst crystals.
This quartz specifically:
Herkimer Diamond quartz crystals though, are a short-prism, usually doubly-terminated variety* of the Quartz species*: Rock Crystal that precipitated* in water within fossil pockets left in dolomitic limestone (dolomite), a sedimentary rock. The pockets (vugs*) within certain dolomite layers in central NY state they're found in were left by stromatalites, an ancient algae/lichen among the earliest living things on Earth.
I found this wonderful little matrix piece my first day ever mining in Middleville, NY, the Herkimers here are bigger than nickles and have grown around cubic dolomite crystals; the detail on the right is of the upper crystal in the specimen as pictured with a dolomite cube in its bottom right side.
When, How & Why:
As I understand it, the story of the Herkimer's formation is something like this: A very long time ago, 400,000,000 years or so, the portion of the Adirondack mountains of New York where these crystals are found was coastline, during this time stromatalites grew there. As time passed, this area became ocean and the stromatalites were covered in sediment, this sediment eventually became dolomite. I'm told that where the overburden of dolomite is ten feet thick was originally over a hundred feet of sediment. At any rate, in water under the ocean is where the Herkimers precipitated, they are aqueous quartz.
There are many mineral associations (other minerals found) with herkimers including pyrite and calcite, leaving aside dolomite, anthraxolite is by far the most common, usually the vugs are lined with it. Since anthraxolite is a carbon mineral it's likely this is the remnants of the stromatalites.
It is a matter of great speculation at the mine and among enthusiasts why Herkimers are so clear and bright, it's my personal suspicion that it was the anthraxolite acting as a charged-carbon type filter in the fluid that precipitated the crystals. Whatever it was, it's clear something acted on these crystals making them remarkably bright, like leaded-glass in some cases. Also a matter of great speculation, is whether or not there is any such thing as a "floater", that is, did any of the crystals precipitate purely out of solution without attachment to anything or do they all have a core? Every miner and enthusiast has their theories, but no one knows for sure.
Where:
As I mentioned, there are other Quartz crystals of similar occurrence around the world, this means found within stromatalite pockets in dolomite, yet these are easily spotted so something's different. These other crystals are found in Mexico but are very obviously dull (lots of anhydros* though) and often called "Meximers"; and in Patagonia, Argentina, where they're brighter than in Mexico but still you can see the difference. I'm sure there's occurrences of quartz like this elsewhere in the world too, but it's inappropriate at best and misleading at worst to call crystals from locals other than NY "Herkimer Diamonds".
The Crystals:
So there is a virtually infinite variety of quartz crystals around, of which Herkimer Diamonds are a type; differentiated by their uniquely beautiful habit* (shape and appearance) and occurrence (situation in which they're formed and found). Herkimer Diamond crystals are sometimes found in dirt only due to weathering over time, they've all come from two types of layers in the dolomite: what at the mine are called "Pockets" and "The Ledge".
"Pockets" are more or less what they sound like, relatively large vugs found in almost regular spacing along certain layers, they can range in size from about that of a basketball to upwards of the size a truck tire might occupy or larger. There can be virtually any type of Herkimer crystals within these pockets: big, broken, rust-covered cloudy ones packed in mud, or small perfect crystals and clusters in anthraxolite powder (though this is rare) and anything in between. Any clusters may already be popped apart or still be "naturals". There are also what are called "skeletal" crystals found in the pockets, these are usually larger than a small peach, and seem to be folded into themselves, leaving radial growth lines often trapping anhydros.
"The Ledge" layer is so called because it is below the pocket layer, miners cleaned off the pocket layer leaving a ledge. I'm told for a long time diggers disregarded or didn't realize this lower layer was crystal bearing, but now most will agree the ledge is where the finest crystals come from. The vugs within the ledge are usually lined with anthraxolite and are random in spacing and size, but seem to run in layers and it is unusual for them to be bigger than apples; it follows that the single crystals and clusters found in this layer are not as large as many pocket crystals, and in general skeletal crystals are not found in the ledge.
I expect most gentile readers of this guide will already be familiar with the most common, 18 or more sided, single crystal habit of the Herkimer Diamond; but I want to add more about the clusters and anhydros.
Herkimer Diamond crystal clusters are notoriously delicate in their natural form; and it is the rule rather than the exception that when you find a cluster it's already popped apart at the contacts between crystals. The best thing to be done in such a case is reconstruct the cluster which is what most diggers do, "natural" (un-popped apart) clusters are rare and treasured. If a digger finds a large pocket of small, popped apart clusters, it is literally a puzzle that can have 10s of thousands of pieces, all the same color and an added dimension, the 3rd., most miners consider the sorting and reconstructing of found crystals to be as fundamental in the process as breaking rock and finding crystal to begin with; so they're not "done" until they've been reconstructed.
Crystals with anhydros can be stunning and are a lot of fun. If you're looking at or for crystals with these you want to be sure to get one that is easy to see if that's important to you, some can be difficult but on the other hand some folks just want to know it's there. Also be sure that it's not somewhere in the crystal where it could escape, like next to or attached to a fracture that reaches the surface, especially if it's a freshly dug crystal. I'm told that some anhydro Herkimers shatter upon being in the Sun's light for the first time, since I've learned this any crystals I've found have been very quickly shaded, just in case, once they've been out of the Earth for a while they're ok. So if you have an anhydro crystal, be sure to take care of it properly: never leave it in a sunny or hot place like a window sill or a car in the sun since some may dry up (not all will). Worst of all for your anhydro crystal is letting it freeze, say by leaving it in your car or garden, this can break most any anhydro bearing crystal.
Herkimer anhydro with a mote of anthraxolite that moves when turned.
Picking and Rating when buying:
The clearest answer is to pick a crystal that makes you happy, whatever it is about it that does, whether it's its flawlessness or the rainbows refracted from fractures present.
Because natural clusters are so delicate you should expect that any Herkimer Diamond crystal cluster on the market is reconstructed unless noted otherwise, and if buying Herkimer cluster jewelry you should insist on it: natural Herkimer contacts will never hold to wear.
Many collectors are interested in rarity, regarding the perfectly flawless Herkimers, I'm fond of saying that one could easily get 10s of thousands of flawless 1 or 2 mm crystals, but that if one had a flawless 2 inch (50 mm) Herkimer they could easily get 10s of thousands of dollars for it: as the crystals get larger not only are they more rare, it also becomes exponentially more rare for them to be flawless. In terms of single crystals, "perfect" 1/4ths-1/2 inch crystals are often found, 1 inch ones are very seldom seen. Single crystals and small clusters like this are highly prized as collectables, healing tools and for jewelry. "Pocket" crystals & clusters and skeletal crystals can be rather large and are collected as specimens and tools.
There is no standard grading or rating system for crystals of this type, so most miners and dealers create their own if they use one. I personally don't use a rating system at the moment, preferring to describe the crystals individually, so I'm going to refer you to a digging friend's rating system for Herkimers that I may adapt for use in the future, (I think this system can use an additional category in the "A" rating since in my opinion there's a good deal of difference between a crystal at the top of the "A" rating and one at the bottom) check it out & more information about Herkimers on Herkmon's page.
As in buying any valuable mineral specimen or gemstone, be sure to deal with a scrupulous dealer who represents their offerings honestly and knows and stands behind what they're talking about and dealing with, and you're sure to get a crystal you'll be happy with.
Novice Digging:
(coming soon;)
Smokey Herkimer Diamond Crystal
You can see creations of mine featuring Herkimer Diamond quartz crystals in my store, Rainbow Zen Crystals; thanks for visiting my guide to these lovely, natural beauties, I hope that you've found it helpful & that you are having a lovely day~
Namaste~
Allen, aka intuitivelyinspired
Glossary:
Anhydro: A water filled void within a crystal or mineral, sometimes also with gas or other minerals within.
Druze: Descriptive term referring to crystals grown together side by side as in many geodes.
Habit: The outer and inner form of a crystal, it's faces', edges', and sufaces' characteristics.
Matrix: The host rock or mineral of a particular specimen. A Herkimer on calcite crystals is on calcite matrix; a calcite crystal on a Herkimer is on Herkimer matrix.
Occurrence: The physical situation a mineral specimen is found in, i.e. in clay or stone, refers to layers and associations.
Precipitate: To change from a lighter form of matter to a heavier one, as in from gas to liquid or liquid to solid, to condense, the opposite of evaporate or melt.
Prism: The "Body" of the C-axis of a crystal form, not always but usually the longest axis and faces. In Quartz crystals the (usually 6) non-terminal faces.
Species: A recognized sub-set of a mineral or mineral group with unique characteristics.
Termination: The point or points of completion of a crystal's growth.
Variety: A recognized sub-set of a mineral species with unique characteristics.
Vug: a mineral bearing opening in a rock.

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