Press Releases

ST. PAUL, Minn., July 3 /PRNewswire-USNewswire/ -- The Minnesota chapter of the Council on American-Islamic Relations (CAIR-MN) today welcomed the decision of a fireworks retailer in Wisconsin to withdraw a product called "Run Hadji Run," which was deemed offensive by local Muslims.

["Hadji" is an honorific term for those who have completed the pilgrimage to Mecca, but it has often been used as a derogatory term by U.S. soldiers during the Iraq War.]

One side of the fireworks shows a picture of Arabs and Muslims riding camels with a bomber overhead. On the other side, there is what appears to be Uncle Sam pulling the long beard of a man in traditional Muslim attire.

SEE: Run Hadji Run

http://www.redrhinofireworks.com/itemview.aspx?ID=CD-2881

ALSO SEE: http://img.moonbuggy.org/run-hadji-run/

After being contacted by CAIR-MN, the company agreed to remove the product from its shelves.

SEE: Racist Fireworks Found Being Sold in Wis. (KSTP-TV)

http://kstp.com/news/stories/S1011199.shtml?cat=206

"We appreciate the quick response of the retailer to Muslim concerns and hope that everyone can enjoy the July 4th holiday in an inclusive environment," said CAIR-MN Communications Director Jessica Zikri.

Zikri added that the Muslim civil rights and advocacy group has contacted the distributors, Missouri-based Red Rhino Fireworks, to take similar action and withdraw the product from sales in other areas of the country.

On Saturday, July 4th, the Tampa chapter of the Council on American-Islamic Relations (CAIR-Tampa) will join with local Muslims in the 2009 Temple Terrace 4th of July Parade to honor and celebrate our nation's independence.

"Part of CAIR's mission is to build coalitions that promote justice and mutual understanding. I cannot think of a better way to express this, than to be a part of a celebration honoring our nation's independence," said CAIR-Tampa Executive Director Ramzy Kilic. "We all must value the freedom, tolerance and justice America offers to us all. This is what it means to be an American."

WHAT: Tampa-area Muslims to join parade in celebration of Independence Day

WHEN: Saturday July 4th, 10 a.m.

WHERE: 113th Avenue -- Temple Terrace, FL -- Unit Section 38 B. For more information on the 2009 Temple Terrace 4th of July Parade, please visit: http://templeterracechamber.com/

CONTACT: CAIR-Tampa Executive Director Ramzy Kilic, 813-486-2529, 813-514-1414, E-Mail: rkilic@cair.com

CAIR, America's largest Islamic civil liberties and advocacy group has 35 offices and chapters nationwide and in Canada. Its mission is to enhance the understanding of Islam, encourage dialogue, protect civil liberties, empower American Muslims, and build coalitions that promote justice and mutual understanding.

CONTACT: CAIR-MN Communications Director Jessica Zikri, 612-226-3289, E-Mail: jzikri@cair.com; CAIR-MN Civil Rights Director Taneeza Islam, Esq., 651-587-4712, E-Mail: tislam@cair.com; CAIR National Communications Director Ibrahim Hooper, 202-488-8787 or 202-744-7726, E-Mail: ihooper@cair.com

SOURCE Council on American-Islamic Relations

MILWAUKEE, Wis., July 3 /PRNewswire/ -- The law firm of Hupy & Abraham, S.C. is continuing its motorcycle safety awareness campaign with an important reminder for all motorists to share the road during the upcoming 4th of July holiday weekend.

(Photo: http://www.newscom.com/cgi-bin/prnh/20090703/CG41956)

"It is our hope that everyone enjoys a safe riding season in 2009 and that motorists share the road with motorcyclists," said Attorney Michael F. Hupy. "With even more people on the road during holidays such as the 4th of July, it is especially important for everyone on the road to be aware and take responsibility for their actions."

In connection with Hupy & Abraham, S.C.' s motorcycle awareness message for the 4th of July holiday, former Wisconsin State Senator Dave Zien will begin his latest motorcycle journey to achieve yet another riding record. Zien has broken 118 motorcycle riding records on his 1991 Harley-Davidson FXRT, most recently becoming the first person to ride one million miles on the same Harley-Davidson motorcycle. Zien will make the first major trip on his new Harley-Davidson motorcycle this weekend, riding from Key West, Florida to Proudhon Bay, Alaska and back within 11 days.

Zien will be departing from Key West at 4:00 a.m. on July 4 for his 11-day journey to Proudhon Bay and will be traveling over 1,000 miles per day. Those interested can visit the Hupy & Abraham Web site to view a live map tracking Dave Zien's progress on his latest ride. For more information, please visit www.hupy.com.

About Hupy & Abraham, S.C.

Hupy & Abraham, S.C. is a personal injury law firm offering a proven record of success with large settlements in serious cases. Hupy & Abraham, S.C. is decades old, and has office locations throughout Wisconsin and Illinois. The firm is committed to giving back to the community, supporting many worthwhile causes including America's Second Harvest of Wisconsin, the YMCA, Boy Scouts, various scholarship programs and safety programs for motorcyclists. For more information on Hupy & Abraham please visit www.hupy.com.

FOR MORE INFORMATION

Marie Maas, 414-390-5500

SOURCE Hupy & Abraham, S.C.

STANFORD, Calif.--(BUSINESS WIRE)-- The newest revolution in microbiology testing walks on four legs and says "baa."

It's the hair sheep, a less-hirsute version of the familiar woolly barnyard resident. A new study from the Stanford University School of Medicine, which is to be published July 3 in PLoS ONE, finds that not only are these ruminants low-maintenance and parasite-resistant, they're also perfect blood donors for the microbiology tests necessary to diagnose infectious disease in the developing world.

Identifying microbes from a patient's urine or sputum requires growing those microbes in culture dishes filled with gelatinous agar and a small amount of blood. The blood provides nutrients to the growing bugs and also provides clues as to the microbes' identities: Microbiologists can rule out or identify certain strains of bacteria based on how the organisms interact with the blood cells in culture.

In the developed world, microbiologists use sheep or horse blood. But in many parts of the developing world, horses are prohibitively expensive, and regular sheep, with their constant need for shearing and tendency to get infections, are difficult to keep alive. Importing animal blood isn't feasible either, as shipping is costly and often unreliable.

Many labs in the developing world use human blood, often donated by lab technicians themselves. But diagnostic tests aren't standardized for human blood, said Ellen Yeh, MD, a resident in pathology at Stanford and first author on the paper. "You don't get the same test results when you use human blood versus sheep blood," she said. In addition, the use of human donors increases technicians' risk of infection with blood-borne diseases.

Ellen Jo Baron, PhD, professor of pathology at the medical school and senior author on the paper, wanted to do better. She's a veteran of overseas microbiology, having trained lab technicians from Botswana to Cambodia for more than a decade.

"Up until the time I saw a hair sheep--which I first saw in Botswana--I had no idea there was even such a thing," said Baron, who is associate director of Stanford's clinical microbiology lab, interim director of the clinical virology lab, and associate chair of pathology for faculty development. She wasted no time in learning about the animals, finding that they resist parasites, don't need to be sheared, and do well in the tropical climes prevalent in much of the developing world.

But no one had tested whether their blood was equivalent to horse or sheep blood. So, calling in a favor from a colleague with a hobby farm near Walnut Creek, Calif., Baron and her colleagues collected blood from hair sheep--the animals are remarkably mellow about the donations, she said--and created test cultures using the blood. Then, they ran a series of common diagnostic tests.

"It worked for every single thing," Baron said.

The researchers also found that they could collect the blood in donation bags, much like those human donors might see at the Red Cross. That's a big advantage over the defibrination process the developed world uses. To defibrinate blood, technicians must shake the samples in a glass jar filled with hundreds of tiny glass beads constantly during and after the donation. That's fine in a lab with machines to do the shaking and autoclaves to sterilize all of those beads, but it's an enormous burden in labs without that equipment. Fortunately, Baron found, hair sheep blood collected in donation bags performed the same as defibrinated blood.

"It's very important," said Bruce Hanna, PhD, professor of pathology and microbiology at the New York University School of Medicine, who was not involved in the study. "This paper found an alternative that is able to be produced in Africa and provides identical results to the standardized products that are used in this country."

Michele Barry, MD, senior associate dean for global health at Stanford medical school, added: "Diagnosis of bacterial diseases and antibiotic sensitivity in low resource settings is often infeasible due to cost, access to diagnostics or manpower. Ellen Jo Baron and colleagues have uniquely decided to combine veterinary health science and human blood banking to develop a blood agar from hair sheep as medium to grow bacteria. This sheep is a low-maintenance animal adopted for hot climates. The technology, which they are modeling in Botswana, is an example of a practical 'can do' innovation in microbiology that will save lives in the tropics at low cost by quickly identifying bacteria to tailor cost-effective antibiotic use--a precious commodity overseas."

Now, said Baron and Yeh, the only hurdle is getting the sheep to the labs that need them. Two veterinary labs in Botswana already provide hair sheep blood to local labs based on Baron's initial results. Baron is now lobbying the charity Heifer International to add hair sheep to its catalogue so microbiologists can donate and send the animals to the developing world. After all, she said, the sheep can provide milk and meat--and that's on top of their role as donors of blood that, in her words, "works perfectly for every microbiology test that a laboratory would need to do."

Baron and Yeh's co-authors on the paper are Stanford pathologist Benjamin A. Pinsky, MD, PhD, and Niaz Banaei, MD, assistant professor of pathology and infectious diseases. The study was self-funded by Baron.

NOTE TO MEDIA: A photo of the sheep is available upon request.

The Stanford University School of Medicine consistently ranks among the nation's top 10 medical schools, integrating research, medical education, patient care and community service. For more news about the school, please visit http://mednews.stanford.edu. The medical school is part of Stanford Medicine, which includes Stanford Hospital & Clinics and Lucile Packard Children's Hospital. For information about all three, please visit http://stanfordmedicine.org/about/news.html.

Photos/Multimedia Gallery Available: http://www.businesswire.com/cgi-bin/mmg.cgi?eid=5999686&lang=en

    Source: Stanford University School of Medicine

SPOKANE, WASHINGTON -- (MARKET WIRE) -- 07/03/09 -- Matthew Russell, President of Azteca Gold Corp. (TSX VENTURE: AZG) (the "Company") wishes to announce recent carbonate and sulfide preliminary assay results for DDH-006 and outline the drilling plan to test, for massive sulfides, newly discovered carbonates located at depth in the Prichard formation. Our targets are the same as we found in DDH-005A: lead-zinc massive sulfides with copper, silver, and gold. Both the newly wedged-off hole DDH-006B and previously wedged-off hole DDH-005B will be deepened during July and August with the expectation of intersecting massive sulfides within and/or adjacent to what we anticipate is a significant carbonate layer or unit. A conceptual sketch of this drill plan, anticipated carbonate unit geometry, and sulfide targets is being prepared for posting on our website. The reader is cautioned that these images are only conceptual in nature and the purpose is to give investors a better understanding of the type and potential geometry of mineralization we are attempting to drill.

On June 26, 2009 the Alberta Securities Commission advised the Company that as a result of a continuous disclosure review, it was required to clarify certain technical and geological information. In addition to this release, the Company intends to provide additional disclosure next week. It cautions that any previous statements suggesting mineable nature or potential economic viability, the application of a Sullivan-type bedded massive sulfide deposit model, or any inferences about metal grades based on geological descriptions of "massive sulfide" or other mineralization types should not be relied on.

Azteca Gold is pleased to announce the intersection of both sulfide stock-work veins above previously unknown calcic carbonates composed of what may be confirmed by the Company as ankerite (limestone with iron and magnesium carbonates). "We are very excited about this new discovery," said Matt Russell. "The adjacent massive sulfide stock-work veins above this limy (calcic) carbonate unit are a good indication that the carbonate unit may have served as a trap for concentrating hydrothermal sulfide solutions. The presence of anomalous gold within the sulfides along with anomalous tungsten is particularly exciting for several reasons. Limy carbonates are known to be associated with large gold deposits such as those found in the Carlin Trend in Nevada. Also, the gold that was mined to the immediate NE of the Two Mile property near Murray, Idaho area during the first half of the twentieth century was accompanied by a tungsten (W) mineral."

Russell went on to add, "Due to the apparent strength of the stock-work veining in DDH-006 and the fact that the most prevalent ore gangue mineral of the Silver Valley is carbonates (siderite and ankerite), we believe that our massive sulfide targets may be intersected within or immediately below these carbonates."

"It may come as a surprise to re-activate wedge-off hole DDH-005B , but after discovering carbonates one kilometer away in DDH-006 and re-examining the core from DDH-005B, we have good reason to expect that these same carbonates (conceptually a carbonate layer or unit) may be intersected within 500 FT of the current 8,744 FT hole depth of DDH-005B," said Mr. Russell. "We had stopped work on hole DDH-005B in mid-March because the calcite (calcium carbonate) veining we were encountering, though encouraging because it was accompanied by light stock-work veining, did not have enough strength to predict a target depth. But now with the ability to compare strata with hole DDH-006, we believe carbonates may be intersected within a relatively short distance of approximately 500 FT in hole DDH-005B, and that it may be worthwhile to test it for massive sulfides."

DDH-006: Carbonate Assay Results 11,081.5 - 11,173 FT
From (FT)      To (FT)   Interval (FT)    Ca (%)   Fe (%)   Mg (%)   CO3 (%)

11,081.5     11,083.0             1.5      1.16     1.93     0.47      4.35

11,106.5     11,108.0             1.5      1.20     2.05     0.45      4.81

11,140.5     11,143.0             2.5      1.57     2.69     0.67      5.48

11,158.0     11,160.5             2.5      1.43     1.93     0.54      6.84
11,160.5     11,163.0             2.5      1.10     2.10     0.60      4.88
11,163.0     11,165.5             2.5      1.69     2.06     0.61      7.50
11,165.5     11,168.0             2.5      2.29     2.28     0.74      8.46
11,168.0     11,170.5             2.5      2.34     2.90     0.70      7.26
11,170.5     11,172.0             1.5      2.65     2.28     0.76     10.30
11,172.0     11,173.0             1.0      6.26     4.38     1.62     20.90

It appears that the carbonates are reasonably wide (at least approximately 90 FT) and that calcium carbonate becomes more prevalent with depth. Whether the carbonate unit discovered will become predominately calcic (calcium carbonate or limestone) can only be determined with further drilling. The width of the carbonate unit may be larger than indicated, and this may be determined as more carbonate assays are obtained for the missing intervals in the above table as well as for adjacent intervals.

CO3 is the carbonate ion and its percentage represents the amount that is carbonate ion. The reader is cautioned that Ca, Fe, and Mg may be part of minerals other than carbonate, but given the amount of CO3 in each interval, balanced chemistry suggests that the majority of the Ca, Fe are paired with CO3. It is not clear to what extent the Mg is paired with CO3.

DDH-006: Stock-work Assay Results 10,460.5 - 10,888 FT
From      To (FT) Inter-     Au     Ag   Cu    Pb   Zn    As     Sb       W
(FT)                 val   (ppb)  (ppm)  (%)   (%)  (%) (ppm)  (ppm)   (ppm)
                     (FT)

                                  less                          less   less
10,460.5 10,463.0    2.5    296 than 2    -     -    -    15  than 5 than 5

                                  less                          less   less
10,478.0 10,480.5    2.5     35 than 2 0.01  0.01 0.01    40  than 5 than 5

                           less   less
10,678.0 10,680.5    2.5 than 5 than 5 0.01  0.01 0.03    22      7      5
                           less   less
10,680.5 10,683.0    2.5 than 5 than 5 0.01  0.01 0.03    20      6      6
                           less
10,683.0 10,685.5    2.5 than 5    5.3    -  0.14 0.25    24      9     35

                                                                      less
10,860.8 10,861.8    1.0     55    6.0 0.08  0.49 2.01    24     15 than 5
                                                                      less
10,861.8 10,863.0    1.2     54    6.2 0.14  1.21 2.47    34     11 than 5
10,863.0 10,863.5    0.5     98   12.6 0.37  0.74 1.75   210     11      6
                           less   less                                less
10,863.5 10,866.0    2.5 than 5 than 2 0.01  0.02 0.08    13      8 than 5
                                                                      less
10,882.9 10,883.8    0.9     41    3.4 0.14  0.17 0.85   201     16 than 5
                           less   less                                less
10,883.8 10,886.3    2.5 than 5 than 2 0.01   .02 0.08    22      9 than 5
                           less   less                                less
10,886.3 10,888.0    1.7 than 5 than 2 0.01   .01 0.05    40      7 than 5

ppm - parts per million      ppb - parts per billion

"The ratios of zinc to lead and lead to silver in the stock-work veins above are generally similar to those found in the massive sulfides reported for hole DDH-005A in January, except that both copper and gold as they ratio to the other metals may be higher, but more data and analysis is needed to make a conclusive determination. We believe that the massive sulfide stock that may be associated with these stock-work veins may be found in or immediately below the carbonate unit," said Mr. Russell. "The gold may be associated in part with tungsten, but more study is needed to make this determination as well." Tungsten above 5 ppm is considered anomalous in samples assayed in DDH-006.

The Company wishes to stress that the above assay values represent grades of stock-work veins and disseminated mineral and not adjacent massive sulfides like those reported in DDH-005A. In a recent press release we described these stock-works as intermittent massive or semi-massive, which, if we had assayed over much smaller, intermittent intervals, it is reasonable to assume some of the above assays may be multiples of those found in the assay results.

"In our press release dated June 18th, 2009, we indicated that bornonite and polybasite and their arsenide analogs may be prevalent minerals in these stockwork veins. Although there is some anomalous antimony (Sb) and arsenic (As) as given above, we now believe that a mixture of different lead, copper, and zinc sulfides with a minority of silver sulfasalts is more likely," said Mr. Russell.

Geologic Discussion

In a press release earlier this year we stated that our massive sulfide discovery of hole DDH-005A may be a Sullivan Style bedded or strata bound type of mineralization unlike the typical vein-type mineralization mined for over 100 years in the Silver Valley of Idaho. Based on the discovery of significant carbonates in DDH-006, we are re-evaluating this mineralization concept.

DDH-006: Assays for 9,998 -- 10,142 FT

From      To (FT) Inter-     Au     Ag   Cu    Pb   Zn    As     Sb       W
(FT)                 val   (ppb)  (ppm)  (%)   (%)  (%) (ppm)  (ppm)   (ppm)
                     (FT)
AVG.                              less                                 less
9,998.0   10,008.0  10.0     19 than 2    -     -  .01    22     14  than 5
INCL.      Notable
         Intervals                less                         less    less
10,005.5  10,008.0   2.5     37 than 2    -     -  .01    47 than 5  than 5

AVG                               less
10,008.0  10,028.0  20.0     27 than 2    -     - 0.02    19      6       8
INCL.      Notable
         Intervals                less
10,008.0  10,009.5   1.5    103 than 2    -     - 0.01    33      6       7
                                  less
10,013.0  10,015.5   2.5     22 than 2    -     - 0.11    26      5      20

AVG                               less                                 less
10,028.0  10,186.0  58.0      - than 2    -     - 0.02    23     10  than 5


INCL.      Notable
         Intervals         less   less
10,137.0  10,139.5   2.5 than 5 than 2    -  0.01 0.08    36      8      15
                                  less
10,139.5  10,142.0   2.5      6 than 2    -  0.04 0.11    85     11      20

"What is most interesting about this interval (9,998-10,142 FT) of predominately fine-grained mica and other silicates (most likely chlorites) is that no significant silver was found-- even though there is anomalous antimony and arsenic, which are necessary elements in tetrahedrite and its arsenide analogs which was expected as stated in a previous news release. It is our belief that since the stock-work veining found below this mica/silicate interval had significant silver associated with it, the absence of silver within this interval may be further indication that the carbonates at depth may have acted as an effective trap for sulfides containing silver," said Mr. Russell.

It is the intention of the Company to present more details of this fine-grained mica/silicate interval as our study of the core and assay results proceeds, especially because we believe that this interval represents a distinct layer or strata which can be identified visually and/or chemically in the core of DDH-005A, DDH-005B, and DDH-006. The importance of this strata is that it may be an altered host for the massive sulfides found in DDH-005A and may be in a format that is relatively unaltered in DDH-005B and DDH-006.

Exploration Plan

A wedge has been successfully set at 9,900 FT on hole DDH-006, which is where wedge- off hole DDH-006B will begin. The target depth remains the same at 11,500 FT to test for massive sulfides in or below the newly discovered carbonates. Since we do not know the width of the carbonates, the target depth may change with drilling. Wedging off the parent hole should be complete during the week of the July 6th and it is estimated that target depth should be accomplished by mid- to end of August. Oriented core methods will be used to determine strata and mineralization dip orientation at select intervals between 9,900 and 11,500 FT.

Re-entering DDH-005B is expected to begin the week of July 13th and it is estimated that target depth of 9,500 FT may be accomplished as early as the first half of August. Oriented core methods will also be used to determine the dip of the strata and mineralization at select intervals between 8,744 and 9,500 FT.

Plans to deepen hole DDH-005A are on hold until work on DDH-005B is complete as access is from the same parent hole DDH-005.

Longer Term Exploration Plan

After testing DDH-006 and DDH-005B to depth for carbonate-hosted massive sulfides, the focus would turn, results dependent, to additional wedge-off holes immediately adjacent to each of the parent holes DDH-005 and DDH-006 w. The Company has previously described its objective of "developing resources" by step out drilling, however, the Company cautions that the definition of mineral resource depends on grades and widths of mineralization as well as a preliminary economic study of potential mine-ability of the particular mineralized geometry. The premise for our exploration is carbonate and mica hosted or replacement strata-bound massive sulfides, and not the vein type massive sulfides for which the Silver Valley of Idaho is known, nor the massive sulfides that were mined in the main zone at the Sullivan in Kimberly B.C. 50% JV partner Silver Royal Apex will undertake this preliminary mine-ability study while Azteca Gold focuses on exploration and resource definition.

Assay and Interval Qualifications

Assays are uncut. True interval widths are not determinable at this time until oriented core techniques can be employed. Some irregular and short intervals have been taken to facilitate mineral identification.

Quality Assurance and Assay Specifications

Diamond drill core samples were processed per the Company's quality assurance policy whereby chain of custody is controlled by Azteca technical personnel who transferred the samples directly to American Analytical Labs, located at Osborne, Idaho. The assay lab has provided assay results to only those within Azteca's control pursuant to the list provided to them by Matt Russell. Assay results are preliminary and will be confirmed by the Company.

Assay methods include fire assay for Ag and Au. ICP (inter-coupled plasma) was used for lead, zinc, copper, antimony, arsenic, tungsten, and carbonates anions Ca, Fe, and Mg. Carbonate (CO3) was titrated.

The information contained in this news release has been reviewed and approved by Matthew Russell, P. Eng. President and CEO, the Company's Qualified Person as defined in National Instrument 43-101.

WARNING: the Company relies upon litigation protection for "forward looking" statements. The information in this release may contain forward-looking information under applicable securities laws. This forward-looking information is subject to known and unknown risks, uncertainties and other factors that may cause actual results to differ materially from those implied by the forward-looking information. Factors that may cause actual results to vary material include, but are not limited to, inaccurate assumptions concerning the exploration for and development of mineral deposits, currency fluctuations, unanticipated operational or technical difficulties, changes in laws or regulations, the risks of obtaining necessary licenses and permits, changes in general economic conditions or conditions in the financial markets and the inability to raise additional financing. Readers are cautioned not to place undue reliance on this forward-looking information. The Company does not assume the obligation to revise or update this forward-looking information after the date of this release or to revise such information to reflect the occurrence of future unanticipated events, except as may be required under applicable securities laws.

Shares issued: 183,219,331

Neither TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release

Contacts:
Azteca Gold Corp.
Jon Slizza
VP of Finance
Cell: (509) 981-2020
Email: info@azteca-au.com

SPOKANE, WASHINGTON--(Marketwire - July 3, 2009) - Matthew Russell, President of Azteca Gold Corp. (TSX VENTURE: AZG) (the "Company") wishes to announce recent carbonate and sulfide preliminary assay results for DDH-006 and outline the drilling plan to test, for massive sulfides, newly discovered carbonates located at depth in the Prichard formation. Our targets are the same as we found in DDH-005A: lead-zinc massive sulfides with copper, silver, and gold. Both the newly wedged-off hole DDH-006B and previously wedged-off hole DDH-005B will be deepened during July and August with the expectation of intersecting massive sulfides within and/or adjacent to what we anticipate is a significant carbonate layer or unit. A conceptual sketch of this drill plan, anticipated carbonate unit geometry, and sulfide targets is being prepared for posting on our website. The reader is cautioned that these images are only conceptual in nature and the purpose is to give investors a better understanding of the type and potential geometry of mineralization we are attempting to drill.

On June 26, 2009 the Alberta Securities Commission advised the Company that as a result of a continuous disclosure review, it was required to clarify certain technical and geological information. In addition to this release, the Company intends to provide additional disclosure next week. It cautions that any previous statements suggesting mineable nature or potential economic viability, the application of a Sullivan-type bedded massive sulfide deposit model, or any inferences about metal grades based on geological descriptions of "massive sulfide" or other mineralization types should not be relied on.

Azteca Gold is pleased to announce the intersection of both sulfide stock-work veins above previously unknown calcic carbonates composed of what may be confirmed by the Company as ankerite (limestone with iron and magnesium carbonates). "We are very excited about this new discovery," said Matt Russell. "The adjacent massive sulfide stock-work veins above this limy (calcic) carbonate unit are a good indication that the carbonate unit may have served as a trap for concentrating hydrothermal sulfide solutions. The presence of anomalous gold within the sulfides along with anomalous tungsten is particularly exciting for several reasons. Limy carbonates are known to be associated with large gold deposits such as those found in the Carlin Trend in Nevada. Also, the gold that was mined to the immediate NE of the Two Mile property near Murray, Idaho area during the first half of the twentieth century was accompanied by a tungsten (W) mineral."

Russell went on to add, "Due to the apparent strength of the stock-work veining in DDH-006 and the fact that the most prevalent ore gangue mineral of the Silver Valley is carbonates (siderite and ankerite), we believe that our massive sulfide targets may be intersected within or immediately below these carbonates."

"It may come as a surprise to re-activate wedge-off hole DDH-005B , but after discovering carbonates one kilometer away in DDH-006 and re-examining the core from DDH-005B, we have good reason to expect that these same carbonates (conceptually a carbonate layer or unit) may be intersected within 500 FT of the current 8,744 FT hole depth of DDH-005B," said Mr. Russell. "We had stopped work on hole DDH-005B in mid-March because the calcite (calcium carbonate) veining we were encountering, though encouraging because it was accompanied by light stock-work veining, did not have enough strength to predict a target depth. But now with the ability to compare strata with hole DDH-006, we believe carbonates may be intersected within a relatively short distance of approximately 500 FT in hole DDH-005B, and that it may be worthwhile to test it for massive sulfides."

DDH-006: Carbonate Assay Results 11,081.5 - 11,173 FT
From (FT)      To (FT)   Interval (FT)    Ca (%)   Fe (%)   Mg (%)   CO3 (%)

11,081.5     11,083.0             1.5      1.16     1.93     0.47      4.35

11,106.5     11,108.0             1.5      1.20     2.05     0.45      4.81

11,140.5     11,143.0             2.5      1.57     2.69     0.67      5.48

11,158.0     11,160.5             2.5      1.43     1.93     0.54      6.84
11,160.5     11,163.0             2.5      1.10     2.10     0.60      4.88
11,163.0     11,165.5             2.5      1.69     2.06     0.61      7.50
11,165.5     11,168.0             2.5      2.29     2.28     0.74      8.46
11,168.0     11,170.5             2.5      2.34     2.90     0.70      7.26
11,170.5     11,172.0             1.5      2.65     2.28     0.76     10.30
11,172.0     11,173.0             1.0      6.26     4.38     1.62     20.90

It appears that the carbonates are reasonably wide (at least approximately 90 FT) and that calcium carbonate becomes more prevalent with depth. Whether the carbonate unit discovered will become predominately calcic (calcium carbonate or limestone) can only be determined with further drilling. The width of the carbonate unit may be larger than indicated, and this may be determined as more carbonate assays are obtained for the missing intervals in the above table as well as for adjacent intervals.

CO3 is the carbonate ion and its percentage represents the amount that is carbonate ion. The reader is cautioned that Ca, Fe, and Mg may be part of minerals other than carbonate, but given the amount of CO3 in each interval, balanced chemistry suggests that the majority of the Ca, Fe are paired with CO3. It is not clear to what extent the Mg is paired with CO3.

DDH-006: Stock-work Assay Results 10,460.5 - 10,888 FT
From      To (FT) Inter-     Au     Ag   Cu    Pb   Zn    As     Sb       W
(FT)                 val   (ppb)  (ppm)  (%)   (%)  (%) (ppm)  (ppm)   (ppm)
                     (FT)

                                  less                          less   less
10,460.5 10,463.0    2.5    296 than 2    -     -    -    15  than 5 than 5

                                  less                          less   less
10,478.0 10,480.5    2.5     35 than 2 0.01  0.01 0.01    40  than 5 than 5

                           less   less
10,678.0 10,680.5    2.5 than 5 than 5 0.01  0.01 0.03    22      7      5
                           less   less
10,680.5 10,683.0    2.5 than 5 than 5 0.01  0.01 0.03    20      6      6
                           less
10,683.0 10,685.5    2.5 than 5    5.3    -  0.14 0.25    24      9     35

                                                                      less
10,860.8 10,861.8    1.0     55    6.0 0.08  0.49 2.01    24     15 than 5
                                                                      less
10,861.8 10,863.0    1.2     54    6.2 0.14  1.21 2.47    34     11 than 5
10,863.0 10,863.5    0.5     98   12.6 0.37  0.74 1.75   210     11      6
                           less   less                                less
10,863.5 10,866.0    2.5 than 5 than 2 0.01  0.02 0.08    13      8 than 5
                                                                      less
10,882.9 10,883.8    0.9     41    3.4 0.14  0.17 0.85   201     16 than 5
                           less   less                                less
10,883.8 10,886.3    2.5 than 5 than 2 0.01   .02 0.08    22      9 than 5
                           less   less                                less
10,886.3 10,888.0    1.7 than 5 than 2 0.01   .01 0.05    40      7 than 5

ppm - parts per million ppb - parts per billion

"The ratios of zinc to lead and lead to silver in the stock-work veins above are generally similar to those found in the massive sulfides reported for hole DDH-005A in January, except that both copper and gold as they ratio to the other metals may be higher, but more data and analysis is needed to make a conclusive determination. We believe that the massive sulfide stock that may be associated with these stock-work veins may be found in or immediately below the carbonate unit," said Mr. Russell. "The gold may be associated in part with tungsten, but more study is needed to make this determination as well." Tungsten above 5 ppm is considered anomalous in samples assayed in DDH-006.

The Company wishes to stress that the above assay values represent grades of stock-work veins and disseminated mineral and not adjacent massive sulfides like those reported in DDH-005A. In a recent press release we described these stock-works as intermittent massive or semi-massive, which, if we had assayed over much smaller, intermittent intervals, it is reasonable to assume some of the above assays may be multiples of those found in the assay results.

"In our press release dated June 18th, 2009, we indicated that bornonite and polybasite and their arsenide analogs may be prevalent minerals in these stockwork veins. Although there is some anomalous antimony (Sb) and arsenic (As) as given above, we now believe that a mixture of different lead, copper, and zinc sulfides with a minority of silver sulfasalts is more likely," said Mr. Russell.

Geologic Discussion

In a press release earlier this year we stated that our massive sulfide discovery of hole DDH-005A may be a Sullivan Style bedded or strata bound type of mineralization unlike the typical vein-type mineralization mined for over 100 years in the Silver Valley of Idaho. Based on the discovery of significant carbonates in DDH-006, we are re-evaluating this mineralization concept.

DDH-006: Assays for 9,998 -- 10,142 FT

From      To (FT) Inter-     Au     Ag   Cu    Pb   Zn    As     Sb       W
(FT)                 val   (ppb)  (ppm)  (%)   (%)  (%) (ppm)  (ppm)   (ppm)
                     (FT)
AVG.                              less                                 less
9,998.0   10,008.0  10.0     19 than 2    -     -  .01    22     14  than 5
INCL.      Notable
         Intervals                less                         less    less
10,005.5  10,008.0   2.5     37 than 2    -     -  .01    47 than 5  than 5

AVG                               less
10,008.0  10,028.0  20.0     27 than 2    -     - 0.02    19      6       8
INCL.      Notable
         Intervals                less
10,008.0  10,009.5   1.5    103 than 2    -     - 0.01    33      6       7
                                  less
10,013.0  10,015.5   2.5     22 than 2    -     - 0.11    26      5      20

AVG                               less                                 less
10,028.0  10,186.0  58.0      - than 2    -     - 0.02    23     10  than 5


INCL.      Notable
         Intervals         less   less
10,137.0  10,139.5   2.5 than 5 than 2    -  0.01 0.08    36      8      15
                                  less
10,139.5  10,142.0   2.5      6 than 2    -  0.04 0.11    85     11      20

"What is most interesting about this interval (9,998-10,142 FT) of predominately fine-grained mica and other silicates (most likely chlorites) is that no significant silver was found-- even though there is anomalous antimony and arsenic, which are necessary elements in tetrahedrite and its arsenide analogs which was expected as stated in a previous news release. It is our belief that since the stock-work veining found below this mica/silicate interval had significant silver associated with it, the absence of silver within this interval may be further indication that the carbonates at depth may have acted as an effective trap for sulfides containing silver," said Mr. Russell.

It is the intention of the Company to present more details of this fine-grained mica/silicate interval as our study of the core and assay results proceeds, especially because we believe that this interval represents a distinct layer or strata which can be identified visually and/or chemically in the core of DDH-005A, DDH-005B, and DDH-006. The importance of this strata is that it may be an altered host for the massive sulfides found in DDH-005A and may be in a format that is relatively unaltered in DDH-005B and DDH-006.

Exploration Plan

A wedge has been successfully set at 9,900 FT on hole DDH-006, which is where wedge- off hole DDH-006B will begin. The target depth remains the same at 11,500 FT to test for massive sulfides in or below the newly discovered carbonates. Since we do not know the width of the carbonates, the target depth may change with drilling. Wedging off the parent hole should be complete during the week of the July 6th and it is estimated that target depth should be accomplished by mid- to end of August. Oriented core methods will be used to determine strata and mineralization dip orientation at select intervals between 9,900 and 11,500 FT.

Re-entering DDH-005B is expected to begin the week of July 13th and it is estimated that target depth of 9,500 FT may be accomplished as early as the first half of August. Oriented core methods will also be used to determine the dip of the strata and mineralization at select intervals between 8,744 and 9,500 FT.

Plans to deepen hole DDH-005A are on hold until work on DDH-005B is complete as access is from the same parent hole DDH-005.

Longer Term Exploration Plan

After testing DDH-006 and DDH-005B to depth for carbonate-hosted massive sulfides, the focus would turn, results dependent, to additional wedge-off holes immediately adjacent to each of the parent holes DDH-005 and DDH-006 w. The Company has previously described its objective of "developing resources" by step out drilling, however, the Company cautions that the definition of mineral resource depends on grades and widths of mineralization as well as a preliminary economic study of potential mine-ability of the particular mineralized geometry. The premise for our exploration is carbonate and mica hosted or replacement strata-bound massive sulfides, and not the vein type massive sulfides for which the Silver Valley of Idaho is known, nor the massive sulfides that were mined in the main zone at the Sullivan in Kimberly B.C. 50% JV partner Silver Royal Apex will undertake this preliminary mine-ability study while Azteca Gold focuses on exploration and resource definition.

Assay and Interval Qualifications

Assays are uncut. True interval widths are not determinable at this time until oriented core techniques can be employed. Some irregular and short intervals have been taken to facilitate mineral identification.

Quality Assurance and Assay Specifications

Diamond drill core samples were processed per the Company's quality assurance policy whereby chain of custody is controlled by Azteca technical personnel who transferred the samples directly to American Analytical Labs, located at Osborne, Idaho. The assay lab has provided assay results to only those within Azteca's control pursuant to the list provided to them by Matt Russell. Assay results are preliminary and will be confirmed by the Company.

Assay methods include fire assay for Ag and Au. ICP (inter-coupled plasma) was used for lead, zinc, copper, antimony, arsenic, tungsten, and carbonates anions Ca, Fe, and Mg. Carbonate (CO3) was titrated.

The information contained in this news release has been reviewed and approved by Matthew Russell, P. Eng. President and CEO, the Company's Qualified Person as defined in National Instrument 43-101.

WARNING: the Company relies upon litigation protection for "forward looking" statements. The information in this release may contain forward-looking information under applicable securities laws. This forward-looking information is subject to known and unknown risks, uncertainties and other factors that may cause actual results to differ materially from those implied by the forward-looking information. Factors that may cause actual results to vary material include, but are not limited to, inaccurate assumptions concerning the exploration for and development of mineral deposits, currency fluctuations, unanticipated operational or technical difficulties, changes in laws or regulations, the risks of obtaining necessary licenses and permits, changes in general economic conditions or conditions in the financial markets and the inability to raise additional financing. Readers are cautioned not to place undue reliance on this forward-looking information. The Company does not assume the obligation to revise or update this forward-looking information after the date of this release or to revise such information to reflect the occurrence of future unanticipated events, except as may be required under applicable securities laws.

Shares issued: 183,219,331

Neither TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release

FOR FURTHER INFORMATION PLEASE CONTACT:
        Azteca Gold Corp.
        Jon Slizza
        VP of Finance
        Cell: (509) 981-2020
        Email: info@azteca-au.com

Source: Azteca Gold Corp.