Time=clinoptilolite;NOW so, I wrote that old-original-founder Rockwell engineer Partner a while back when we almost decided to non renew Chuca Butte in the Rabbitfoot Claims at Rt 66 this past August, I (we) get our kicks on Route 66:
auctionbuy.com
The Zeolite deposit near the wilderness study area is a
clinoptilite-mordenite deposit. Drilling was done by Occidental Minerals and
Phelps Dodge (aka Rockwell) identified 1 million st with an inferred resource
of 2MM st. The ammonium exchange capacity ranges from 0.79 millequivalents
NH/g to 1.72............The grade of the zeolite minerals is too low for use
in ammonium absorption.
Average ammonium exchange capacity must be more than 1.6 NH/g to be used for
ammonium absorption. Although this deposit does not meet the requirements for
ammonia absorption it may be suitable for other uses........
CG:
WE HAVE THE RATE OF EXCHANGE THAT is rare! Thus value able ...if THE Rate at $465<sic- sb $485> is at CNA mining which IS OUR SAME RATE EXCHANGE EXACT amount...as in USG report..S-Gravities etal...
<<..clinoptilolite..>>
Chucka URL below
Clinoptilolite is the most abundant member of the 48 minerals in the zeolite group. The mineral occurs in extensive deposits throughout the world. Although more clinoptilolite is produced than any other zeolite mineral, most of the end use applications are construction aggregates, building stone, soil additives, and animal adsorbents. Only a very small percentage of these deposits are capable of producing high purity clinoptilolite suitable for ion exchange, and sorption applications.
The two clinoptilolite products specially selected for sale by GSA Resources are ZS403H and ZK406H. Both of these products are high purity products which have unique yet different properties. Though both minerals are clinoptilolite, each has unique chemical and physical properties which determine its applications.
ZK406H is a potassium clinoptilolite which excels in odor control, and high tech agricultural products. It is also the product of choice for most coated and carrier applications.
ZK403H is a sodium clinoptilolite which is the finest product available for ammonia control in waste water and aquariums. It also has the highest attrition resistance of any clinoptilolite we have tested which had a high rate of ion exchange. This product also can be used in radio active waste treatments.
GSA Resources is always searching for and testing zeolite minerals in an effort to make available the very finest product tailored to each customer's needs. Our corporate goal is excellence.
gsaresources.com
OUR C ZEO:
( We decide to promote as All Should on great Auxilliary Elements)
.We then need to do a 5 acre Permit with NV BLM to run a quarry Operation if Big John can deal there or go to Kingman Office to set up the Permit.
>The Delay in getting the report out onto the web wil delay in getting us some RETURN on INVESTMENT...we must think og us as a Zeolite Play and get on who to how to with what Golf Cources to ( a sub page on Golf is also needed as that iss the biggest market for 'C" type Zeolite!@ Tom..I need some hours to re build the focus of the web Site..Chuca Butte will be the need Front Page Click Name rather than Rabbittfoot..Let's Use this years spelling..Chucka Butte! LOL
>
>
> Geologist
>Has a file for 40 pages on OUR ZEOLITE with Tables and charts on DRILL HOLLS ON out property from a 1988 report in which the 1990 report that old found the few sentances in the Wilderness Study
>
>
>OTHER INFO:
>
Minerals | By_Name | By_Class | By_Groupings | Search | Properties | Silicates
Hey, I just thought of a wild question, dies SM or ORXX have anything to do with this comapny? They at this thread learned I was DAN BAR correct there, so now things change ands they find...ZEOLITE, the Mr C type, LOL. RE:
Subject 8516
Subject 8516
Read the last FEW posts...then go back and see the Financial Court Case that I was DAM BAR RIGHT about from day one 2 years ago.
ChucauptzeoC2-below is great and we have 500,000 tons as a RESOUCE by BLM Docs and Drills ten years ago INFO- $450+ per ton! LOL.
Message 11030199
Message 11030199
OUR are IN Range VIA ...BLM guys contract..Professor Pitkin my TEXTBOOK author of the USGS report LOL:
Zeolite Grade/Classification:
The zeolite capacity for absorbing pollutants is a quality factor that determines the price per tonne and is measured by the Caton Exchange Capacity, or CEC factor. To be good, marketable zeolite CEC factors must range from 80-120+, depending on their grade and size, the Clinoptilolite zeolites sell for as high as US$485/tonne.
OURs at WMA8- <<..>The Zeolite deposit near the wilderness study area is a
>clinoptilite-mordenite deposit. Drilling was done by Occidental Minerals and
>Phelps Dodge (aka Rockwell) identified 1 million st with an inferred resource
>of 2MM st. The ammonium exchange capacity ranges from 0.79 millequivalents
>NH/g ..>>
>
>and :
>
>
>
>>From: Chuca Marsh <chucalo@aol.com> (All Golf Course Builders E mail Right Away! LOL)
>>Subject: Zeo-
>>
>>A zeolite can be thought of in terms of a house, where the structure of the house (the doors, windows, walls and roof) is the zeolite while the furniture and people are the water and ammonia molecules and ions that can pass in and out of the structure. Clinoptilolite's sheet-like structure produces the prominent pinacoid faces, the perfect cleavage and the unique luster on those faces.
>>
>>
>>PHYSICAL CHARACTERISTICS:
>>Color is colorless, white, pink, yellow, reddish and pale brown.
>>Luster is vitreous to pearly on the most prominent pinacoid face and on cleavage surfaces.
>>Transparency: Crystals are transparent to translucent.
>>Crystal System is monoclinic; 2/m
>>Crystal Habits include blocky or tabular crystals with good monoclinic crystal form. More tabular and proportioned than heulandite. Also commonly found in acicular (needle thin) crystal sprays.
>>Cleavage is perfect in one direction parallel to the prominent pinacoid face.
>>Fracture is uneven.
>>Hardness is 3.5 - 4, maybe softer on cleavage surfaces.
>>Specific Gravity is approximately 2.2 (very light)
>>Streak is white.
>>Other Characteristics: Can absorb a significant amount of water after drying and will retain its structure even if heated to almost the temperature of melted glass.
>>Associated Minerals are calcite, aragonite, thenardite, hectorite, quartz, apophyllite, opal, clays, pyrite, halite, mordenite, heulandite, chabazite, analcime, erionite, ferrierite, harmotome, dachiardite, phillipsite and several borate minerals
>>Notable Occurrences include the widespread tuffaceous volcanic rocks of Arizona; the type locality of Hoodoo Mountains and the Yucca Mountains of Nevada; Altoona, Washington; Agate Beach and Madres, Oregon and several sites in California, USA. Also found at Styria, Austria; Bulgaria; British Columbia, Canada; Ortenberg Quarry, Germany; Alpe di Siusi, Italy; Kuruma Pass, Japan; McQueens Valley and Moeraki, New Zealand and Chinchwad, India.
>>Best Field Indicators are crystal habit, density, locality, water absorption, heat tolerance and associations.
mineral.galleries.com
>>The zeolites are a popular group of minerals for collectors and an important group of minerals for industrial and other purposes. They combine rarity, beauty, complexity and unique crystal habits. Typically forming in the cavities, or vesicles, of volcanic rocks, zeolites are the result of very low grade metamorphism. Some form from just subtle amounts of heat and pressure and can just barely be called metamorphic while others are found in obviously metamorphic regimes. Zeolite crystals have been grown on board the space shuttle and are undergoing extensive research into their formation and unique properties.
>>The zeolites are framework silicates consisting of interlocking tetrahedrons of SiO4 and AlO4. In order to be a zeolite the ratio (Si +Al)/O must equal 1/2. The alumino-silicate structure is negatively charged and attracts the positive cations that reside within. Unlike most other tectosilicates, zeolites have large vacant spaces or cages in their structures that allow space for large cations such as sodium, potassium, barium and calcium and even relatively large molecules and cation groups such as water, ammonia, carbonate ions and nitrate ions. In the more useful zeolites, the spaces are interconnected and form long wide channels of varying sizes depending on the mineral. These channels allow the easy movement of the resident ions and molecules into and out of the structure. Zeolites are characterized by their ability to lose and absorb water without damage to their crystal structures. The large channels explain the consistent low specific gravity of these minerals.
>>
>>Zeolites have many useful purposes. They can perform ion exchange, filtering, odor removal, chemical sieve and gas absorption tasks. The most well known use for zeolites is in water softeners. Calcium in water can cause it to be "hard" and capable of forming scum and other problems. Zeolites charged with the much less damaging sodium ions can allow the hard water to pass through its structure and exchange the calcium for the sodium ions. This process is reversable. In a similar way zeolites can absorb ions and molecules and thus act as a filter for odor control, toxin removal and as a chemical sieve. Zeolites can have the water in their structures driven off by heat with the basic structure left intact. Then other solutions can be pushed through the structure. The zeolites can then act as a delivery system for the new fluid. This process has applications in medicine, livestock feeds and other types of research. Zeolites added to livestock feed have been shown to absorb toxins that are damaging and even fatal to the growth of the animals, while the basic structure of the zeolite is biologically neutral. Aquarium hobbyists are seeing more zeolite products in pet stores as zeolites make excellent removers of ammonia and other toxins. Most municipal water supplies are processed through zeolites before public consumption. These uses of zeolites are extremely important for industry, although synthetic zeolites are now doing the bulk of the work.
>>
>>Zeolites have basically three different structural variations.
>>
>>There are chain-like structures whose minerals form acicular or needle-like prismatic crystals, ie natrolite.
>>Sheet-like structures where the crystals are flattened platy or tabular with usually good basal cleavages, ie heulandite.
>>And framework structures
>>http://mineral.galleries.com/minerals/silicate/zeolites.htm
>
>>say on this...AMMONIA ZEOs is what we have so thusly, do we MAYBE have these new C Zeos???Chucka
>>
>>
>>THE MINERAL CLINOPTILOLITE
>>Chemistry: (Na, K, Ca)2 - 3Al3(Al, Si)2Si13O36-12H2O, Hydrated Sodium Potassium Calcium Aluminum Silicate
>>Class: Silicates
>>Subclass: Tectosilicates
>>Group: Zeolites
>>Zeolite Family: Heulandite
>>Uses: As a chemical filter, chemical absorber, water purifier and as mineral specimens.
>>Specimens
>>Clinoptilolite is not the most well known, but is one of the more useful natural zeolites. Clinoptilolite is used in many applications such as a chemical sieve, a gas absorber, a feed additive, a food additive, an odor control agent and as a water filter for municipal and residential drinking water and aquariums. Clinoptilolite is well suited for these applications due to its large amount of pore space, high resistance to extreme temperatures and chemically neutral basic structure. What might strike many as odd is the food and feed additives. Clinoptilolite has been used for several years now as an additive to feed for cows, pigs, horses and chickens. It absorbs toxins in the feed that are created by molds and microscopic parasites and has enhance food absorption by these animals. Similar uses in actual people food is being tested.
>>
>>***********************************SEE
OURS? Ammonia Rate Different!???Clinoptilolite can easily absorb ammonia and other toxic gases from air and water...YES!!!
>>
>>
>>
>>Clinoptilolite can easily absorb ammonia and other toxic gases from air and water and thus can be used in filters, both for health reasons and for odor removal.
>>Clinoptilolite forms as a devitrification product (the conversion of glass to crystalline material) of volcanic glass in tuffs. Tuffs are consolidated pyroclastic rocks. The devitrification occurs when the glass is in contact with saline waters. Clinoptilolite is also found in the vesicles of volcanic rocks such as basalts, rhyolites and andesites. It forms as an alteration of phillipsite in deep-sea sediments and with borate minerals in playa lakes. Clinoptilolite, which means "oblique feather stone" in Greek, received its name because it was thought to be the monoclinic (or obliquely inclined) phase of the mineral ptilolite, as in "oblique ptilolite". But ptilolite was later found to be the earlier named mineral mordenite; consequently ptilolite is no longer in use.
>>
>>Clinoptilolite is very closely related to heulandite and is currently being considered for disuse itself as it may just be a variety of huelandite. It differs from heulandite significantly only in its enrichment in potassium and slightly more silica and it is argued that a separate mineral is not needed. The name clinoptilolite is widely recognized and used among zeolite industries, mineral collectors and mineralogists. For now at least, clinoptilolite is recognized as a legitimate, distinct mineral.
>>
>>The structure of clinoptilolite is the same as heulandite and is sheet-like. Although still a true tectosilicate where every oxygen is connected to either a silicon or an aluminum ion (at a ratio of [Al + Si]/O = 1/2), there still is a sheet-like structural organization. The sheets are connected to each other by a few bonds that are relatively widely separated from each other. The sheets contain open rings of alternating eight and ten sides. These rings stack together from sheet to sheet to form channels throughout the crystal structure. The size of these channels controls the size of the molecules or ions that can pass through them and therefore a zeolite like clinoptilolite can act as a chemical sieve, allowing some ions to pass through while blocking others. A zeolite can be thought of in terms of a house, where the structure of the house (the doors, windows, walls and roof) is the zeolite while the furniture and people are the water and ammonia molecules and ions that can pass in and out of the structure. Clinoptilolite's sheet-like structure produces the prominent pinacoid faces, the perfect cleavage and the unique luster on those faces.
>>
>>
>>PHYSICAL CHARACTERISTICS:
>>Color is colorless, white, pink, yellow, reddish and pale brown.
>>Luster is vitreous to pearly on the most prominent pinacoid face and on cleavage surfaces.
>>Transparency: Crystals are transparent to translucent.
>>Crystal System is monoclinic; 2/m
>>Crystal Habits include blocky or tabular crystals with good monoclinic crystal form. More tabular and proportioned than heulandite. Also commonly found in acicular (needle thin) crystal sprays.
>>Cleavage is perfect in one direction parallel to the prominent pinacoid face.
>>Fracture is uneven.
>>Hardness is 3.5 - 4, maybe softer on cleavage surfaces.
>>Specific Gravity is approximately 2.2 (very light)
>>Streak is white.
>>Other Characteristics: Can absorb a significant amount of water after drying and will retain its structure even if heated to almost the temperature of melted glass.
>>Associated Minerals are calcite, aragonite, thenardite, hectorite, quartz, apophyllite, opal, clays, pyrite, halite, mordenite, heulandite, chabazite, analcime, erionite, ferrierite, harmotome, dachiardite, phillipsite and several borate minerals
>>Notable Occurrences include the widespread tuffaceous volcanic rocks of Arizona; the type locality of Hoodoo Mountains and the Yucca Mountains of Nevada; Altoona, Washington; Agate Beach and Madres, Oregon and several sites in California, USA. Also found at Styria, Austria; Bulgaria; British Columbia, Canada; Ortenberg Quarry, Germany; Alpe di Siusi, Italy; Kuruma Pass, Japan; McQueens Valley and Moeraki, New Zealand and Chinchwad, India.
>>Best Field Indicators are crystal habit, density, locality, water absorption, heat tolerance and associations.
>>
>>--------------------------------------------------------------------------------
>>
>>Minerals | By_Name | By_Class | By_Groupings | Search | Properties | Silicates
>>
Chucks...yes but WE have AZ claims with a RESOURCE of 500,000 TONS that is an auxilliary Element WORTH $232 Million at Surface in the Ground on a State Road at our Chuca Butte Claim and that ain't hay! I will be happy to spend my Saturday Morning & Evenings Posting my Reseach on such weird auxillary elements for my families share of the EIGHT ( + ) in WMA8. Go auxillaiary Elements ...then, go the PGMs. We suceeded as Naxos did, in HOLDING CLAIMS; now, we reseach. We wait.
PS- clinoptilolite= WHITE GOLD- We form a Claim Group foor NEWTECH PGMs and find: clinoptiloliteclinoptiloliteclinoptiloliteclinoptiloliteclinoptiloliteclinoptiloliteclinoptiloliteclinoptiloliteclinoptiloliteclinoptiloliteclinoptiloliteclinoptiloliteclinoptiloliteclinoptiloliteclinoptiloliteclinoptiloliteclinoptiloliteclinoptiloliteclinoptiloliteclinoptiloliteclinoptilolite...worth $250 Million USD LOL clinoptilolite is where you find it, same with BORON and PGMs and what was that other Naxos Element? |
