Superstition Mountains Geology and Prospecting 

 

 

Gold in the Superstition’s

 

Part I

 

 Gold Sample FW0047 

By 

Fred Williams 

Alan Zink

Matthew Roberts

 

 

The official search for gold in the Superstition Mountains began in earnest, sometime around 1864 when the first serious prospectors entered the range and began looking for signs of mineralization. No one knows what degree of success those early prospectors may have had as much of what they found and their mining activity was largely undocumented. It is known that those early anglo prospectors encountered numerous excavations throughout the range, some of them extensive. Much speculation exists over their origins. Most agree the Mexicans surely mined in the Superstitions from the 1840s onward while still others believe the Spanish who predated them had their own workings. It is agreed upon by all, the Superstition Mountains have a long and colorful history regarding the search for gold.

Nothing so drastically changed the search for that gold in those mountains as did the Wilderness Act of 1964. The Wilderness Act of 1964 (WA64) was first proposed by congress in 1934 but was not enacted by the House of Representatives and the Senate until September 3, 1964 when they passed legislative act P.L. 88-577,78 Stat.890; 16 U.S.C. 1121, 1131-1136. thereby creating the Superstition Mountain Wilderness Area (SMWA).

From it’s beginning, the Superstition Mountain Wilderness area was a contradiction in terms. The Act itself describes the wilderness as an area where earth and its community of life are untrammeled by man, where man himself is a visitor who does not remain. An area retaining it’s primeval character and influence, without permanent improvements or human habitation, the imprint of man substantially unnoticeable.

If ever a description did not fit the Superstition Mountains, the Wilderness Act description was it. By 1964 the SMWA had been colonized by several ranches beginning in 1877 with the Cavaness ranch which would later become Tex Barkleys Quarter Circle U Ranch. Thousands of head of cattle grazed the entire range. Watering holes, windmills, stone structures, line shacks, fences, earth and rock dams as well as corrals dotted the entire landscape. Some of these structures had stood for almost a century. In addition, numerous mines and prospects within the SMWA were in use and more being explored all the time. The Superstition Mountains did not fit the definition of a wilderness area yet the plans to create a wilderness in those mountains went forward with disregard. This was just one of a long line of questionable and contrary decisions that would surface and evolve over the next 20 years as the wilderness process moved toward it’s final completion.

                                                                             

                                                 Old mine tunnel, now buried.

 

Under Section 3 subsection a. of the 1964 Wilderness Act a provision was made in which within one year after September 3, 1964, a file map and legal description (survey) of the Superstition Mountain Wilderness Area boundaries must be filed with the Department of the Interior and Insular Affairs Committee of the United States Senate and House of Representatives. To this date, 43 years later, that specific legal description remains unfinished and has never been officially submitted to the Department of the Interior or the Insular committees. It was the responsibility of the Secretary of the Interior and the Secretary of Agriculture to submit the findings of their assigned studies to the President of the United States and Congress. The Secretary of the Interior was tasked with the responsibility of conducting an in depth survey of the mineralization of the Superstition Mountains with regard to mines, mining and prospecting within the SMWA.

The US Department of the Interior assigned this mineral survey to the US Geological Survey and Bureau of Mines Intermountain Field Operations Center in Denver, Colorado. The survey was authorized under Public Law 88-577 and the Joint Conference Report on Senate Bill 4 of the 88th Congress. The survey was officially designated the Mineral Investigation of the Superstition Wilderness and Contiguous Rare II Further Planning Areas, Gila, Maricopa, and Pinal Counties, Arizona. Known also as MLA 136-82.

The first phase of the field survey work began in October of 1973 and continued through March of 1974. This early field work was done by Geologists Henry Meeves and Frank Williams of the US Geological Survey (USGS) office in Denver. Their work was aided by a parallel study that had been ongoing since 1970 in the Superstition Mountains by Dr. Martin Stout, a geologist at Cal State University in Los Angeles. Dr. Stouts ongoing work on the volcanic venting and fault zone mineralization within the Superstition Mountains was of great value to the early survey. Stouts meticulous field notes as well as his detailed drawings, diagrams and maps pinpointed hundreds of fault lines, fault zones, volcanic vents and the mineralization found in conjunction with these features. Since most metallic mineralization such as gold is found close to these features, his findings and documentation of mineralization was highly important and helpful in determining a systematic pattern for taking samples. Dr. Stouts passion was felsic volcanism and the resulting surface venting and fumaroles associated with surface magma flows. A geological science that dovetails perfectly with the exploration of gold. Meeves and Williams spent the fall and winter of 1973-1974 taking mineral samples and analyzing them .

 

       Pit in the mountains, now buried.     

 

The method for their sampling was as follows. Standard chip samples were taken across mineralized, altered and sheared zones as well as across country or host rock in related areas. Altered or visually mineralized samples and fragments were taken from any mining dump or prospect pile the geologists encountered. Chip samples were taken inside tunnels and shafts where the mineralized veins were visible. All samples taken were fire assayed for gold and silver and wet assayed or spectrographically analyzed for copper, lead, tungsten, chromium, and zinc. Atomic absorption was used to further analyze samples of copper, lead and zinc whose spectrum analysis was between .03 and 1.0 percent. Results of all analysis and assay work was reported in oz./ton. Where trace amounts of mineralization occurred, the report entry was either Tr. (trace) or ND (not determined).

In the early days of the survey, every area of the SMWA was sampled, including all mining dumps, prospect holes, tunnels and shafts. This criteria would change drastically later on in the survey. A detailed description of the host rock, quartz and associated mineralization was meticulously noted by the early sample takers. Later on in the survey this criteria would become almost generic. Detailed diagrams and locations of fault planes, fault zones, fault lines and related mineral locations were made by the early survey geologists, this would become non existent as the survey progressed. It was almost as if the entire focus and purpose of the mineral survey changed as the sampling and analysis progressed.

A good question to explore is what exactly was the purpose and focus of the original SMWA mineral survey ?

For that answer, one must refer back to the wording of the Wilderness Act of September 3, 1964. The geological survey was conducted to determine the mineralized locations lying within the boundaries of the SMWA and to determine their value. The SMWA Act specifically made a provision ( Section 4 d. ) in which prospecting and mining could continue within the SMWA providing the location, claim and or patent was filed before midnight on December 31, 1983. Another provision in the Act ( Section 5 b.) directed the Department of Agriculture ( United States Forest Service ) to provide free and unrestricted access going to and coming from any and all existing claims and patents ( filed prior to December 31, 1983 ) along customary, established routes. In conclusion, the survey was intended to determine precisely where the prospecting, mining and exploration was being carried out within the SMWA, what type and quantity of minerals were present, and what the approximate value of those mineralized areas are, that when the December 31, 1983 deadline expired, the Department of the Interior and the US Forest Service would be appraised of the mining activity they would have to contend with within the Superstition Mountain Wilderness Area. The SMWA geological mineral survey began in 1973 with that goal in mind, however, by 1975-1976, the focus on that goal had changed dramatically.

What changed that original mineral survey plan and it’s focus ?

It is not hard to follow the course of events that transpired and come to a conclusion. In the beginning the plan was to allow the continuation of prospecting and mining after the Wilderness deadline on claims that could be proven to have a verified minable resource present. Two Federal agencies were tasked at appraising the minable mineral deposits and the later oversight of the mines and mining. Those agencies were the Bureau of Mines and the Department of Agriculture (US Forest Service). In 1973 the Bureau of Mines began its survey and strictly held to its goal and original plan. But by the fall of 1976, that agencies plan took a sharp turn. The method of sampling, the records kept and even the areas being sampled changed. Where in 1973, the entire Superstition range was being sampled, by 1976, the entire northern half of the Superstition Mountains were withdrawn from the survey and only the southern half was being sampled. This does not mean the northern half did not fall under the scope of the survey because it did, it simply was ignored and the field work that had already been accomplished there, never saw the light of day.

The early field work done by the geologists from the US Bureau of Mines, building upon Dr. Martin Stouts field work, was a thorough and meticulous analysis of the geology and mineralization of the mountains, much of that work done in the northern half of the range. The northern half of the range could be described approximately as everything north of an imaginary line running down the east west alignment of LaBarge canyon. It seems incredible that such a large portion of the SMWA would be ignored and is a question that has never been answered. The assumption is the final report concluded there was no mineralization in the northern half yet the field notes and records of the early geologists paint an altogether different picture. In fact, it shows a pattern of mineralization that would certainly at the least, require further excavation and exploration to understand the size and scope of the resources that were found by the sampling. The survey instead, from 1976 on, focused on a small area surrounding Weavers Needle and mines and prospects lying outside the proposed SMWA boundaries. Along with this zeroing in of the Weavers Needle area, much of the findings were purposely laced with the tales and legend of the Lost Dutchman mine. For what purpose one can only speculate, most likely in an attempt to minimize the survey and sensationalize the legends, making the case that mining in the Superstitions was all a big useless treasure hunt with no possibility of mineral discovery.

The stage was now set. By 1976 the mineral survey had degraded into a small area surrounding one legendary landmark and many areas not even within the Superstition Mountain Wilderness Area boundary. All other areas were ignored and not even considered. The final survey predictably showed there was no mineralization whatsoever within the SMWA boundaries. The only thing left now was for the Bureau of Mines and the Department of Agriculture to catalog the mining claims filed prior to the December 31, 1983 deadline and eliminate them. This was to be accomplished by conducting a survey on each claim and disproving the mineralization, thereby effectively invalidating the claim and the land returned to the SMWA. It would come to pass that the individual claim surveys would also degrade into an exercise where the claims were withdrawn without any actual survey being conducted. Numerous protests were lodged by individual claim holders who petitioned for a survey of their claims and were either ignored, or in closed hearings, were denied or over ruled. In most cases, claim holders received a notice in the mail stating their claim had been invalidated without any field survey or former notification. By 1985, every mining claim filed within the SMWA that was current, had been denied and invalidated.

The focus of the 1973 mineral survey had indeed changed. Where once the stated plan was for the Bureau of Mines and Agriculture Department to work with and manage mines and prospects within the SMWA boundary, the plan became the elimination of all prospecting and mining within the Superstition Mountains. This plan was carried out with efficiency, forcefulness and in the end, ruthlessness.

 

 

                                                                         In Part II, the real survey, and gold in the Superstitions.

                                                                                                       Part I by Fred Williams

 

 

(Superstition Mountain, Arizona)

 

The Geologic History of Superstition Mountain 1970

 

 

Michael Sheridan

Martin Stout

 

 

The Superstition Mountains lie in a narrow zone that separates the Colorado Plateau to the north from the Basin and Range Province to the south. The Colorado Plateau is an area of geologic stability since the start of the Paleozoic era (600 million years ago). No great episodes of folding, faulting, or intrusion are recorded during this time. The Basin and Range province (Superstition Mountains), on the other hand, has undergone a great deal of geologic activity in the not too distant geologic past, including faulting, intrusions, volcanism, and one major ore emplacement. Much of this activity was during the period of 20 to 30 million years ago when the rocks of the Superstition Mountains were forming. Hence this area is an important key to interpreting the geology of a broader region.

During the middle part of the Cenozoic era (30 million years ago) the region near the present Superstition Mountains had a relatively flat-lying topography. The low hills were composed of Precambrian granite with minor amounts of Precambrian and Paleozoic sedimentary rocks exposed to the east. Sometime in the range of about 25-30 million years ago a vast region of the southwest experienced tensional stresses in an east-west direction. Minor faulting occurred and the valleys were quickly filled with coarse conglomerates, breccias, and sandstones eroded from the uplifted areas. These sediments formed the red bedded deposits now exposed in Papago Park in Phoenix and the west end of Camelback Mountain. These red bedded deposits have been given the formational name, the White Tail Conglomerates.

The pace of geologic activity then quickened. The ground around the present Superstition Mountain swelled and a ring of dacite volcanoes issued forth, forming a series of mountain masses 2000 to 3000 feet high. The major part of this eruptive event occurred about 29 million years ago.

The most violent phase of the volcanic cycle then began. Tremendous explosions produced deposits of at least 2000 feet of ash and fractured rock that spread out laterally as a thick red-hot dust cloud moving along the ground. The cloud traveled scores of miles in all directions and the resulting ash completely covered the former dacite volcanoes. The hot volcanic glass compressed to form a dense rock called welded tuff. The explosion left an area of some 15 kilometers in diameter that formed a colossal pit containing jumbled blocks of steeply dipping rocks. Outside this caldera the tuffs remained nearly horizontal in the position of their deposition. The welded tuff formed by eruption is here called the Superstition Formation.

But the cycle was not yet complete. Renewed energy brought another portion of the magma near the surface. As the magma pushed upward the central part of the collapsed caldera was domed-up to form the present Superstition Mountain mass. The gasses in this second magma exploded producing another ash deposit. However, this time the deposits were cooler and did not weld into a dense compact rock. Ash from this series of eruptions covered the Goldfield Mountains to the west and spread northward toward Four Peaks. This ash, which is pale yellow in color, and interbedded with glassy lavas is called the Geronimo Head Formation. Other areas then collapsed forming the Goldfield Cauldron and Tortilla Cauldron. Glassy dikes intruded along the caldera faults and a final outburst 15 million years ago produced the welded tuff that now occurs along the south side of Canyon Lake. A quiet period then followed.

At about 18 to 15 million years ago, after this violent phase, slow outpourings of black basalt lavas occurred within the caldera. At Black Mesa at least three such basalt lavas are seen along the Second Water trail. Water washed the loose ash into the low areas forming bedded deposits like those north of First Water Ranch and Canyon Lake. Late rhyolite gravels that washed onto the caldera depressions now make up the cliffs north of Canyon Lake and the terraced deposits between Tortilla Flat and Fish Creek Canyon. This rock unit is called the Mesquite Flat breccia for the good exposures between Tortilla Flat and Horse Mesa dam.

The rocks that formed the Superstition wilderness are placed in stratigraphic sequence.

This short period of violent activity from 29 to 15 million years formed the spectacular rocks of the Superstition Mountains today. It remained for 15 million years of normal erosion and some gentle tilting, faulting and intrusions to further modify the landforms created during this episode.

Geologic dictionary of terms :

Caldera: A large basin shaped volcanic depression which is more or less circular in form. Calderas range in size from one to 20 miles in diameter.

Caldron: A large irregular shaped volcanic depression, usually formed by collapse due to eruption of a large volume of ash.

Cenozoic: The latest of the four eras into which geologic time is divided. This era extends from about 70 million years ago until the present.

Dacite: A generally light colored volcanic rock having plagioclase feldspar and quartz as essential minerals.

Dike: A tabular body of igneous rock that cuts across existing rocks. Dikes result from the intrusion of magma toward the surface.

Fault: A fracture in the earth along which there has been displacement of the sides relative to one another.

Glass: The rapidly chilled liquid portion of magma that does not have crystalline structure. Volcanic glass (Obsidian) are generally of rhyolite composition.

Intrusion: A body of igneous rock that invades and pushes into or through older rock.

Magma: Mobile, partly-molten rock material generated within the earth.

Quartz: The whitish clear mineral with the formula SiO2. Silicone and Oxygen,

Rhyolite: A volcanic rock composed of quartz, sanidine, and biotite generally with a glassy groundmass.

Tuff: A rock composed of volcanic particles ejected through the air.

Volcanic breccias: A rock composed of large angular fragments of older volcanic rock surrounded by an ash matrix.

End

 

 

 

 

Typical Goldfield Epithermal Quartz Deposit

The Superstition Mining District

by Matthew Roberts

(copyright 1985)

 

The Superstition Mining District of Arizona was founded in 1893 following the discovery of gold in rich gold and silver bearing veins along the Piedmont Basin which is the general area of todays Weekes Wash. The Mammoth, Bull Dog, and Black Queen mines were the major producers in the 1893 - 1898 time period, which was known as the glory years for the Superstition Mining District. The booming community of Goldfield sprang up along the road from Mesa to Government well and at one time boasted almost 5,000 residents. An estimated $1,000.000 in gold was taken from the mines in these glory years, represented by almost 50,000 ounces, and that was when gold was $20.67 per ounce. The silver taken from those mines in the same time period was estimated at $350,000 when silver averaged about 65 cents per ounce.

The Superstition Mining District is but a memory. Today, the District has been renamed the "Goldfield Mining District". The district boasted 12 major gold, silver and copper producers in its "golden years". Several other claims were filed where some gold was removed but either accurate records were never kept, or the mines produced less than a few ounces / pounds of gold and silver.

The producing mines of the district were :

The Mammoth                     The Treasure Vault                       The Gold Bond

The Bull Dog                       The Copper Crown                       The Gold Strike

The Black Queen                The Tom Thumb                            The Lazy Doc

The Old Wasp                    The Fair Stake

The Bluebird                        The High Flyer

The Golden Hillside             The Buckhorn-Boulder ( Palmer )

 

Mining still goes on in the district today. Most of the mines best producers are flooded by groundwater. Unable to pump out the ground water, the gold left in these mines is safe under a watery grave, at least for the time being. The Old wasp is still being mined at this writing and other prospects along the 9 major faults that criss-cross the Piedmont Basin are being worked.

Dr. Michael Sheridan, geology professor at ASU in Tempe, completed a study on the geology of the Superstition Mountains and the ore deposits of the Goldfield District. Sheridan found the gold and silver fell into the class of epithermal veins, lodes and ore bodies. The epithermal veins have a northerly trend along faults and are usually associated with intrusive dikes. Sheridan identified nine separate faults along which the gold deposits were located.

Epithermal gold deposits form when superheated water percolates through pre existing fractures and porous areas of rock near the surface. Quartz forms in these cracks and fissures and the gold and metallic elements precipitate and migrate forming the ore and quartz matrix. The goldfield mines are all located along the outer edge of what is known as the Superstition Caldera. This outer edge is a highly fractured zone with faults running in a generally north south direction. This fracture zone is highly conducive to the formation of metallic ore deposits.

It was late 1891 when four prospectors, Orin and Orlando Merrill, C.R. Hakes and James Morse, discovered the workings of what they believed to be a placer deposit in a long wash known today as Weekes Wash. The dump of the placer digging was played out and no further placer ore could be located at the site so they moved on. In November of the following year (1892) following a terrific rain, James Morse was again in that same wash when he noticed the recent flood had washed the alluvial gravel in the wash down to the bedrock in several places. Upon checking these exposed places, he discovered a rich vein of gold embedded in quartz along the floor of the wash. He and his partners filed on the deposit and a gold rush to the area quickly ensued. The town of Goldfield sprang up on the site and by 1898 almost $1,500,000 worth of gold and silver had been taken out of Weekes wash.

The rich mines became worked out for the most part save for the Black Queen, Bull Dog, Mammoth and Old Wasp which suffered the fate of being flooded with ground water. In 1949, at the idle site of the Mammoth Mine, a mining engineer (Alfred Strong Lewis) was working for the mines owner, the Shumway brothers of Phoenix, when he discovered an enormous boulder covering a shaft and tunnel which had previously been overlooked in the mining activity. No record of this old shaft and tunnel could be found in the Mammoth Mine records which were some of the most exacting and detailed ever documented in Arizona. The boulder was placed there to conceal the entrance to the down shaft. The shaft and tunnel were of Spanish or Mexican origin, very small in comparison to the Mammoth excavations and was timbered with crudely cut iron wood logs which Lewis had analyzed, along with some other artifacts taken from the tunnel. The shaft went down about 50 feet and a tunnel of about 80 feet drifted with a rich vein of gold in quartz. Lewis formed a partnership with some friends after securing ownership of the mine from the Shumways. The partners took out about $50,000 worth of gold when they broke into an old tunnel of the Mammoth Mine dug in 1895 by the then owner, Charles Hall. Thus ended Lewiss brief but lucrative mining boom.

The Superstition / Goldfield District mines are among some of the richest and most interesting mines in Arizonas mining history. The Superstition Mountain Caldera that is responsible for these rich mines, continues on in a circle all the way around Superstition Mountain proper, deep into the interior of the mountains. Geologists believe rich gold deposits can be found all along the outer fracture rings of the Superstition Caldera. The goldfield Mines were discovered because they were situated where erosion and floods periodically exposed the veins to prospectors. The same deposits may be lying deep in the interior of the mountains, covered over by between 20-500 feet of overburden rock.

The End

 

 

 

 


Hydrothermal  Gold  Deposit
Undisclosed  Location. 

Superstition Mountains Gold

by  Anderson  Wilde

Gold is the most sought after element by treasure seekers in and around the Superstition Mountains of central Arizona. Rich gold mines are located around the outside of the vast mountain range and while no commercially workable mine has ever been operated within the range, some placer and lode deposits have been reported and numerous prospectors have found color and over 1,000 mining claims were filed within the range prior to the Wilderness Act.

The rich gold mines located at the fringe of the Superstition range, the Mammoth, Bull Dog, Wasp, Black Queen and Palmer mines were all Hydrothermal gold deposits. All these mines produced thousands of ounces of rich gold and millions of dollars in revenue for their owners before the mines played out or were flooded by underground rivers.

This article briefly explains the hydrothermal gold deposit, how and why it forms and where it can be found within the Superstition Mountain range.

A hydrothermal deposit is a deposit precipitated from a high temperature solution. As hot water and minerals in solution rise toward the earths surface, the lower temperature and pressure near the surface causes the minerals to precipitate out of the solution. Molten rock and magma below the surface supplies the hot fluids which travel upwards along the pressure gradient (cracks and fissures in the earths crust). Molten magma is three to eight percent water by weight and lava contains five percent water.

Several processes must affect the rock in order to make it more receptive for mineralization. The rock must become more permeable and brittle. Rocks are hardened by silica, then shattered by faulting which increases permeability. Broken silica causes clean fractures so that fluids can move easily through the rock toward the surface.

Faults are fractures along the surface where displacement of the surface rock has occurred. The greater the fault (displacement) the greater the formation of clay zones which fill the openings and block the hydrothermal activity. Therefore, small faults, with slight displacement are the most favorable for hydrothermal ore deposits to form.

As hot fluids are discharged from the magma, they circulate through huge volumes of shattered (displaced) rock, dissolving a variety of minerals. After taking minerals in solution at high temperatures and pressures, the fluids move toward the surface along channels known as fracture zones. When the temperature and pressure drops sufficiently, minerals will begin to precipitate along the walls of the fractures forming ore (gold) deposits. Think of the gold being suspended in a liquid solution and as the solution cools the gold migrates to one side of the crack in the earths crust where it collects and hardens.

Rich lode gold deposits formed by hydrothermal solutions precipitate such minerals as quartz, barite, carbonate materials, fluorite, gold, gold tellurides and silver. These deposits tend to be found on the surface of the earth or at a shallow depth down to 1000 feet and may contain fabulously rich pockets of gold. Hydrothermal gold lodes have been referred to as bonanzas, because they tend to be much richer than other types of gold lodes. Ore grades of Hydrothermal deposits commonly range from one to twenty ounces of gold per ton of rock with pockets of 5000 ounces per ton having been discovered.

Some of the keys to prospecting for hydrothermal deposits are, of course, anywhere there is a hot spring. There are several hot springs located in and around the Superstition Mountains.

Volcanic rock covers most of the entire Superstition mountain range. For millions of years, the volcanic layers of rock and gas and ash built up on top of one another. Then, as in the end of the Jurassic period of the Mesozoic era and again during the Tertiary period of the Cenozoic Era, magma from deep in the earth forced its way toward the surface under great pressures from deep within the earths center. The Superstition mountains have remained unchanged for the past 27 million years except for faulting and erosion. It is the faults and fissures in the volcanic rock that one must look for when searching for possible gold deposits within the Superstition mountains. Float gold (gold which has broken off a deposit and has been washed downhill into canyon bottoms) is a good way to look for the deposit. Often this float can be traced back uphill to its original source.

The Superstition mountains are still a place of great mystery, and searchers still comb the twisting canyons and mountainsides for that elusive deposit that has yet to be found.

 

When Silver Was King
By Jack San Felice


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