sailaway
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- Mar 2, 2014
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The Spanish used a little known secret of egg shells in their long lasting concrete mix that they borrowed from the Romans.
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<emphasis mine, not in the original text, a very ancient method of mining hard rock dating well past Roman times>ALTO MINES
These present an extensive development and have been very richly productive. The ground included was among the early discoveries of the Jesuits, who are said to have continued operations in their primitive and desultory way rather steadily for about 150 years. Their facilities for development, ore extraction and reduction were crude and ineffective. Drill steel and blasting powder were unknown. With rough iron bars they drilled to depths of several feet into the rocks large round holes several inches in diameter, which were filled with lime, plugged securely and water poured in. The swelling lime rent the rocks, and when thrown out of place they were broken further with hammers.
The Spanish used a little known secret of egg shells in their long lasting concrete mix that they borrowed from the Romans.
Re: Jesuit Code Book ?- A Standard of the Kings Codes ? Post Number:#264
Post by: strackjoseph Tue Mar 11, 2014 3:25 am
I've been treasure hunting for 51 years......20 of those years was in colo. The rest has been it Ariz. If it wasn't for C.Kenworth books .....Yes I got them all... Ive got Mike Picketts also ....not to mention many many more. I didn't really get in to Spanish treasures.....till 1986 , With C . K . books I've found a fine treasure of 635 Bars of silver. As they say pick you'll partner wisely .....I'll leave at that ... In 1999 or 98 I also found the Guadalupe mine ....a lot of people think I am crazy and don't know what I am talking about. From the Molina Document I took photos of the area to prove the find ,the P.S.R. the doc. talks about I have a photo of it.not to mention many more photos of the mine it self and the area in and around it .The silver bars were found east of the mine a ridge over. The Purisima Concepcion Mine was found first everything as been taking out of it . The OPatas is still filled with treasure I haven't pin pointed the location yet but I know I am close say 200 varas . At this time its not a safe place to be ,in Jan. 2014 we found a snipers nest . found no weapon but found the ammo. in Nov 2013 my partner found where the sniper was living in a hi-cave . The lost Dutchman was found in 1978 by C.K. he took out 17 and a half million in Gold before forest sev. kick him out . The Iron door mine I,am surprised no body has found it ,with all the signs and symbols on those mountains ' you can't miss finding it. I've not tried to find it, I am not fit to try and tackle a trail up to it. thanks for you'll time it is time for bed.
Ancient Lost Treasures ? View topic - Jesuit Code Book ?- A Standard of the Kings Codes ?- Eight K
then the other part of this tractNational mineral assessment tract SB24 (Distal disseminated Ag-Au)
Tract SB24
Geographic region Southern Basin and Range
Deposit type Distal disseminated Ag-Au
Deposit age Mesozoic - Tertiary
Title Descriptive model of distal disseminated Ag-Au
Authors Dennis P. Cox
URL Distal disseminated Ag-Au
Source Developments in mineral deposit modeling
Estimators ; Church, D. Cox, L. Cox, Diggles, Force, Titley
Explained by Leslie J. Cox
On the choice of deposit models
Distal disseminated Ag-Au deposits form in sedimentary rocks distal to plutons. The deposits are somewhat similar to sediment-hosted Au deposits, but have significantly higher Ag grades and base-metal contents. They are associated with hypabyssal or subvolcanic intrusions. Arizona has at least two known distal disseminated Ag-Au deposits.
On the delineation of permissive tracts
The permissive tract was delineated by modifying the tracts for porphyry Cu deposits, and including Late Cretaceous to early Tertiary muscovite-garnet-bearing peraluminous granite and associated pegmatite (unit TKgm, Reynolds, 1988). We then outlined areas within that modified tract that are known to contain limestones and other carbonate rocks. The tract also includes all pertinent known mineral districts.
Important examples of this type of deposit
Two deposits in Arizona, Hardshell and Tombstone, are part of the grade and tonnage models (Cox and Singer, 1992), but both are below the median tonnage. Tombstone is classified as a distal disseminated Ag-Au deposit rather than as a polymetallic replacement deposit because it contains no massive replacement bodies and lacks a clear relationship to a plutonic contact. The Vekol district might be classified as distal disseminated Ag-Au, but it produced less than 100,000 metric tons of ore and is not a significant deposit.
On the numerical estimates made
Estimators thought that deposits of this type might be both commonly formed and readily concealed in Arizona, because they are low in sulfide content and relatively inconspicuous. This type of mineralization was not widely recognized as ore until the 1970s, because of its low-grade, disseminated nature. For the 50th percentile, estimators noted that the number of known distal-disseminated deposits is near that of polymetallic-replacement deposits: about 2 to 7. Therefore, some argued that there should be perhaps 4 to 10 total known plus undiscovered (the estimate for undiscovered polymetallic-replacement deposits at the 50th percentile is 3). For the 90th, 50th, 10th, 5th, and 1st percentiles, the team estimated 1, 2, 5, 7, and 10 or more deposits consistent with the grade and tonnage model of Cox and Singer (1992).
References
Cox, D.P., 1992, Descriptive model of distal disseminated Ag-Au, in Bliss, J.D., ed., Developments in mineral deposit modeling: U.S. Geological Survey Bulletin 2004, p. 19.
Cox, D.P., and Singer, D.A., 1992, Grade and tonnage model of distal disseminated Ag-Au, in Bliss, J.D., ed., Developments in mineral deposit modeling: U.S. Geological Survey Bulletin 2004, p. 20-22.
Reynolds, S.J., 1988, Geologic map of Arizona: Arizona Geological Survey Map 26, scale 1:1,000,000.
National mineral assessment Tract SB17 ( Porphyry Cu-Au )
Tract SB17
Geographic region Southern Basin and Range
Deposit type Porphyry Cu-Au
Deposit age Laramide
Title Descriptive model of porphyry Cu-Au
Authors Dennis P. Cox
URL Descriptive model of Porphyry Cu-Au
Source Mineral deposit models
Estimators; Carlson, Church, D. Cox, L. Cox, Diggles, Force, Guthrie, Kamilli. Kleinkopf, Richa
Explained by Leslie J. Cox and Michael F. Diggles
On the choice of deposit models
The rationale for the choice of the porphyry copper-gold model of Cox and Singer (1992) was based on our ability to identify characteristics in the known Arizona deposits that are unique to the porphyry Cu-Au deposit model and on our ability to distinguish a geologic setting for gold-rich porphyries that is different from the general porphyry-copper environment. It is argued that gold-rich porphyries tend to be associated with alkaline igneous rocks (Gilmour, 1982, Lowell, 1989). Wilt (1993), however, contends that gold-rich porphyry deposits occur in calc-alkaline settings as well, but possesses an oxidation state that is determined by the rocks through which the magma rises: the gold-poor porphyries are oxidized, whereas the gold-rich porphyries are weakly oxidized. Our estimates for undiscovered porphyry Cu-Au deposits were guided by Wilt's delineation of oxidized versus weakly oxidized calc-alkaline rocks in Arizona.
On the delineation of permissive tracts
The tract for porphyry copper-gold consists of all six of the general porphyry copper tracts for Arizona. The most favorable rocks consist of porphyritic igneous rocks of Laramide age in the Basin and Range and Transition Zone of Arizona and their interpreted geophysical extensions beneath cover. The team identified and excluded areas that would not be permissive for the occurrence of porphyry copper deposits because of parameters such as geologic setting, rock composition, and depth of cover.
Important examples of this type of deposit
Only a few of the many significant Arizona porphyry copper deposits are gold-rich: Dos Pobres (Langton and Williams, 1982), Ajo-New Cornelia (Hagstrom and others, 1987), and Sanchez. Of the three known deposits, all have tonnages below the median for the porphyry Cu-Au model (Singer and Cox, 1986).
On the numerical estimates made
Estimates for porphyry Cu-Au deposits were weighted toward areas characterized by weakly oxidized calc-alkaline intrusions as defined by ferric:ferrous ratios in unaltered plutons. In southwestern Arizona, the potential for Laramide Cu-Au porphyries in the identified weakly oxidized area is relatively small, because the shallow Laramide intrusions have been largely destroyed by erosion. This is indicated by the fact that volcanic rocks of Oligocene age rest unconformably upon eroded plutons of Laramide age. Only a small part of the tract is favorable for porphyry Cu-Au deposits.
The theory that porphyry Cu-Au deposits are emplaced close to the surface and should be situated within their associated volcanic rocks was considered and Laramide intrusions adjacent to volcanic rocks of the same age were examined. To arrive at estimates of undiscovered porphyry Cu-Au deposits, the team considered first the probability of there being zero deposits, the maximum number likely, and the most likely number. Using this estimation technique, the team reached a consensus of an expected value of about 1 undiscovered porphyry Cu-Au deposit. For the 90th, 50th, 10th, 5th, and 1st percentiles, the team estimated 0, 1, 2, 3, and 4 or more deposits consistent with the grade and tonnage model of Singer and Cox (1986).
References
Cox, D.P., and Singer, D.A., 1992, Distribution of gold in porphyry copper deposits, in DeYoung, J.H., Jr., and Hammarstrom, J.M., eds., Contributions to commodity geology research: U.S. Geological Survey Bulletin 1877, p. C1-C14.
Gilmour, Paul, 1982, Grades and tonnages of porphyry copper deposits in Titley, S.R., ed., Advances in geology of the porphyry copper deposits: Tucson, University of Arizona Press, p. 7-36.
Hagstrum, J.T., Cox, D.P., and Miller, R.J., l987, Structural reinterpretation of the Ajo Mining District, Pima County Arizona based on paleomagnetic and geochronologic studies: Economic Geology, v. 82, no. 4, p. l348-l36l.
Langton, J.M., and Williams, S.A., 1982, Structural petrological, and mineralogical controls for the Dos Pobres ore body, in Titley, S.R., ed., Advances in geology of the porphyry copper deposits, southwestern North America: Tucson, University of Arizona Press, p. 335-352.
Lowell, J.D., 1989, Gold mineralization in porphyry copper deposits discussed: Mining Engineering, v. 41, no. 4, p. 227-231.
Singer, D.A., and Cox, D.P., 1986, Grade and tonnage model of porphyry Cu-Au, in Cox, D.P., and Singer, D.A., eds., Mineral deposit models: U.S. Geological Survey Bulletin 1693, p. 110-114.
Wilt, J.C., 1993, Geochemical patterns of hydrothermal mineral deposits associated with calc-alkalic and alkali-calcic igneous rocks as evaluated with neural networks: Tucson, University of Arizona, Ph.D. dissertation, 721 p.
GEOCHEMICAL SIGNATURES: Ag+Pb+Zn+Cu+Sb+As+Zn+Pb+Mn+Cu+Ag+Au+As+ Sb+Hg+Te; Mn introduced at Cove, Candelaria, and Star Pointer. Ag:Au ratios are highly variable: Candelaria 400:1; Taylor, 143:1; Tecoma, 60:1; Purisima Concepcion, 51:1; Hilltop, <2:1.
Too crazy for me….much of the lost or hidden treasures are from extremely wide geographic locations, mostly unrelated to the location of the finds/treasures……
It would seem the owner of the land has more right to anything found…...
But, but the church has officially denied amy minng How can they have any claim
........AND BINGO WAS HIS NAME-O!
Both the Jesuit Order and the Catholic Church have denied any involvement in mining activities in the area during Colonial Times. The proper thing to do would be to have an attorney ask the Pope and Jesuit General to sign a notarized affidavit stating that neither the Church nor the Jesuit Order were ever involved in any illegal mining activities during colonial times.
Bet they won't!
Mike