Katerina Mine (Ashley mine; Caterina mine; Catherin mine; Catherina mine; Katrina mine), Hiriart Mountain (Hariat Mtn; Harriot Mtn; Heriart Mtn; Heriot Mtn; Hiriat Hill), Pala, Pala Mining District, San Diego County, California, USAi
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Latitude & Longitude (WGS84):
33° 22' 23'' North , 117° 2' 33'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
Place | Population | Distance |
---|---|---|
Rainbow | 1,832 (2011) | 10.6km |
Temecula | 112,011 (2017) | 16.6km |
Valley Center | 9,277 (2011) | 17.2km |
Hidden Meadows | 3,485 (2011) | 17.7km |
Aguanga | 1,128 (2011) | 18.2km |
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
Local clubs are the best way to get access to collecting localities
Club | Location | Distance |
---|---|---|
Fallbrook Gem and Mineral Society, Inc. | Fallbrook, California | 19km |
Vista Gem & Mineral Society | Vista, California | 27km |
Palomar Gem & Mineral Club | Escondido, California | 29km |
Mindat Locality ID:
9684
Long-form identifier:
mindat:1:2:9684:6
GUID (UUID V4):
f07d1c52-104d-4ba5-893b-62f859999524
"Katerina"
—Italian, meaning "pure".
Setting:
Located in the center of the S2SW4 Sec. 24 T9S R2W SBM, the mine is low on the southwest slope of Hiriart Mountain, aggregating 20.66 acres, more or less. Over 2,056 tons of material had been excavated from open pit operations at the Katerina mine, principally during the period from 1902 to 1940. Approximately 2,019 tons of rock and ore had been removed from 13 underground workings between 1902 and 1992.
The Katerina mine is located approximately 2.5 miles east of the town of Pala, in San Diego County. Access is 1.3 miles north from state highway 76, on Magee road. The west boundary (endline) of the lode mining claim is 321 feet east of Magee road. Access to the property is by a two-track dirt road, ending 992 feet from the intersection with Magee road. Slopes on the claim are steep, measured by Brunton compass at approximately 24 degrees. The claim is positioned on the south slope of Hiriart Mountain at an elevation varying from 820 feet at the southwest corner to 1,240 feet above sea level at the northeast corner. A steep, narrow, south-flowing drainage dissects the claim across the center of the property.
History:
The deposit was discovered by Bernardo Hiriart and first located under the general mining laws by Marion M. Sickler on March 15th of 1902. Sickler reported that later that year, he and his son Frederick, discovered nodular to blade-like crystal fragments of a clear, colorless to straw-yellow and pale-lilac mineral. Several unsuccessful efforts were made to identify the mineral, until December of 1902, when they sent specimens to George Frederick Kunz, a gem expert for Tiffany and Company of New York. This newfound gem variety of lilac-colored spodumene was subsequently named in honor of Dr. Kunz and was popularly known as "California's own gem"[1].
Not long after the date of the Katerina location, the surrounding vacant public lands were temporarily withdrawn and removed from mineral entry under the United States land and mineral laws pursuant to Secretarial Order dated January 24, 1903. This order was a temporary withdrawal pending acquisition of all private inholdings, including valid existing rights, for the benefit of the Pala Tribe, under Indian tract allotment pursuant to the Act of January 12, 1891.
In 1905, Kunz described the Katerina mine as a cut 40 feet in length and 30 feet in width, which exposed a ledge of lepidolite 2.5 feet thick, producing about 6 tons of lepidolite. Also from this cut was reported some kunzite and spodumene production, the greater part of which was considered float. Other gems found included pink beryl and a few tourmalines.
In 1906, Kunz described the main Katerina development as a large open cut which cut the "pay streak", or central part gem-bearing part of the ledge, which varied from 2 to 4 feet in thickness, and consisted of quartz, albite, and lepidolite. Several pockets were reported to be found, primarily containing quartz crystals and violet-colored kunzite. Another cut some one hundred yards to the east was said to reveal similar pockets, with pink kunzite and some indicolite, together with quartz crystals, often clear and fine. One pocket from here was said to yield nearly a ton of crystallized quartz, with some individual crystals weighing up to 40 pounds.
Between 1907 and 1938, Marion Sickler reported a total approximately 538 days of work extending tunnels and open pit at the Katerina mine. On August 27th, 1938, Marion M. Sickler deeded the mine to his son Fred for 1 dollar and 'love and affection'. Between 1939 and 1946, Fred reported a total of approximately 150 days of work prospecting the ledges.
On July 28, 1947, Fred M. Sickler and his wife Florence A. Sickler sold the mine to George A. Ashley of Pala. In 1948 Ashley reported running over 68 feet of tunnels. Between 1949 and 1956, a small amount of work was accomplished, and Ashley continued filing his affidavit of annual assessment work.
Ashley sold the claim to Karl V. Morin Jr. of Vista and Jean P. Oddous on January 4th of 1957. Work began improving the road, and renewed tunneling and drifting at the Katerina throughout 1959. In 1960, a well was drilled on the property, and other sections of pegmatite were prospected for gem minerals. Again in 1964 tunneling and drifting operations at the Katerina throughout 1965. Between 1972 and 1984, additional tunneling and some open pit work were accomplished by Morin and mineral collector Al Ordway of Hesperia.
On November 1, 1990, Morin leased the Katerina mine for 5 years to Otto Komarek and Byron Weege, both of Pala. In December of 1990, Weege discovered a large pocket while working underground which contained several cathedral-style quartz crystals, many with tiny indicolite inclusions, giving the quartz a pale bluish cast. Over 125 feet of underground drift was constructed by Komarek and Weege, utilizing a small diesel wheeled loader to load and haul waste rock to the surface for dumping, combined with hand tool work while working the pocket zone. On December 21st of 1992, Morin quitclaimed an undivided 2/3rds interest in the Katerina lode mining claim to Komarek and Weege.
On December 9, 1992, the Bureau of Land Management (BLM), initiated an investigation and verification of rights under the United States mining laws in order for the claimants to proceed with planned mining activities. Field examinations of the Katerina mine were conducted beginning with a preliminary examination on January 7th, 1993. In March and April of 1994, the BLM conducted surveys of the mining claim boundaries. Investigations continued in January of 1996, with detailed field examinations of the Katerina lode claim conducted by mineral examiners Robert M. Waiwood and Walter R. Todd between March and April. These examinations detailed the mineralization of the claim and included survey and mapping of all improvements and access to them.
On March 20, 1996, two pockets were discovered underground by Karl Morin, Otto Komarek, and Byron Weege, and over 1,200 grams of kunzite and over 2,000 grams of morganite specimens were removed from the pockets. On October 30, 1996, a mineral report was completed and serialized, completing the validity examination of the Katerina Lode, which concluded that the claimants had fulfilled all obligations under the mining laws, and had a right to proceed with mineral operations, and a right of access guaranteed under the General Mining Law of May 10, 1872 (30 USC 22 et seq.).
In November of 1998, a small find of kunzite was made in the area of the dike worked by Ashley during the early 1950s. The mine area was consumed by a wildfire which started near the southern claim boundary in July of 2001.
On May 5, 2003, Otto Komarek quitclaimed his one half of one-third portion of the Katerina mining claim to Byron C. Weege.
On April 5, 2005, Karl Morin quitclaimed his two-thirds portion of the Katerina mine claim to Byron C. Weege, giving Byron Weege ownership of the entire Katerina mining claim.
In 2007 - 2010 Byron Weege with the help of friends Stephen and Lisa Koonce and Joe Johnson minor prospecting and exploration of the Katerina mine claim was conducted with the purpose of beginning operations at the mine in the near future. During this period a few small pockets were encountered in the upper tunnels yielding both Kunzite and Morganite crystals.
In July of 2010, Byron C. Weege passed away and transferred the Katerina mining claim to his brother.
On October 1, 2012, Greg Weege quitclaimed the entire Katerina mining claim over to Joe Johnson. With the intent to once again get the Katerina mine in working condition as Byron wanted.
Currently, the Katerina mining claim is again being prospected and a plan of operations has been made for beginning operations at the Katerina mine in early 2013. Joe Johnson, Stephen and Lisa Koonce and several other experienced Pala area miners are working hard to once again bring the Katerina mine back into active operation.
Footnotes:
1. Kunz received spodumene samples from Frederick M. Sickler, but no locality information was given at that time. There is, however, ample supporting evidence that the samples sent to New York were from the discovery workings of the Katerina mine.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
Mineral list contains entries from the region specified including sub-localities24 valid minerals.
Detailed Mineral List:
ⓘ Albite Formula: Na(AlSi3O8) Localities: Katerina Mine (Ashley mine; Caterina mine; Catherin mine; Catherina mine; Katrina mine), Hiriart Mountain (Hariat Mtn; Harriot Mtn; Heriart Mtn; Heriot Mtn; Hiriat Hill), Pala, Pala Mining District, San Diego County, California, USA Vanderberg-Katerina pegmatites (Vanderburg-Katerina dikes; Vanderburg-Katerina pegmatites), Katerina Mine (Ashley mine; Caterina mine; Catherin mine; Catherina mine; Katrina mine), Hiriart Mountain (Hariat Mtn; Harriot Mtn; Heriart Mtn; Heriot Mtn; Hiriat Hill), Pala, Pala Mining District, San Diego County, California, USA References: |
ⓘ Albite var. Cleavelandite Formula: Na(AlSi3O8) Localities: Katerina Mine (Ashley mine; Caterina mine; Catherin mine; Catherina mine; Katrina mine), Hiriart Mountain (Hariat Mtn; Harriot Mtn; Heriart Mtn; Heriot Mtn; Hiriat Hill), Pala, Pala Mining District, San Diego County, California, USA Vanderberg-Katerina pegmatites (Vanderburg-Katerina dikes; Vanderburg-Katerina pegmatites), Katerina Mine (Ashley mine; Caterina mine; Catherin mine; Catherina mine; Katrina mine), Hiriart Mountain (Hariat Mtn; Harriot Mtn; Heriart Mtn; Heriot Mtn; Hiriat Hill), Pala, Pala Mining District, San Diego County, California, USA References: |
ⓘ Amblygonite Formula: LiAl(PO4)F References: |
ⓘ Bertrandite Formula: Be4(Si2O7)(OH)2 Description: Three tiny crystals of bertrandite were in a small cavity in one phenakite-cleavelandite specimen from the main workings of the Katerina mine. |
ⓘ Beryl Formula: Be3Al2(Si6O18) References: |
ⓘ Beryl var. Goshenite Formula: Be3Al2(Si6O18) |
ⓘ Beryl var. Morganite Formula: Be3Al2(Si6O18) |
ⓘ Columbite-(Fe) Formula: Fe2+Nb2O6 Colour: Dull black on crystals faces; bright submetallic luster on freshly broken surfaces. Description: Ferrocolumbite forms tabular crystals, generally no more than 1/4 inch thick and 1 inch by 1 inch in plan. The principal faces of most of the crystals are flat, but some very thin and broad crystals are markedly curved. Many of these platy individuals are 1/16 inch or less in thickness and as much as 4 inches in maximum dimension. They occur in radiating groups. A few crystals are more equant, and appear as subhedral to euhedral "chunks" 1/2 inch to 6 inches in diameter, with an average of about an inch. |
ⓘ 'Columbite-Tantalite' |
ⓘ Cookeite Formula: (LiAl4◻)[AlSi3O10](OH)8 Colour: White, buff-colored and very pale pink. Description: Cookeite is a rather widespread pocket species, and ordinarily forms a coating on crystals and crystal aggregates of quartz, lepidolite, spodumene, albite, and orthoclase. It forms white, buff-colored and very pale pink aggregates of small plates and flakes. |
ⓘ 'Feldspar Group' References: |
ⓘ 'Feldspar Group var. Perthite' References: |
ⓘ Fluorapatite Formula: Ca5(PO4)3F References: |
ⓘ Foitite ? Formula: ◻(Fe2+2Al)Al6(Si6O18)(BO3)3(OH)3(OH) References: |
ⓘ Helvine Formula: Be3Mn2+4(SiO4)3S Habit: Tetrahedra Colour: Honey-colored Description: An exceedingly rare constituent of the pegmatite in the Katerina mine. It forms small honey-colored tetrahedral crystals that are less than 1 millimeter in diameter. They occur on the surfaces of cleavelandite and spodumene crystals, and in general are typical of the pocket-bearing parts of the dike. |
ⓘ 'Indicolite' Formula: A(D3)G6(T6O18)(BO3)3X3Z |
ⓘ 'Lepidolite' References: |
ⓘ Lithiophilite Formula: LiMn2+PO4 Description: Moore (2000) analyzed lithiophilite from this locality and found the Mn/Mn + Fe ratio was 0.76 |
ⓘ Microcline Formula: K(AlSi3O8) References: |
ⓘ Muscovite Formula: KAl2(AlSi3O10)(OH)2 Localities: Katerina Mine (Ashley mine; Caterina mine; Catherin mine; Catherina mine; Katrina mine), Hiriart Mountain (Hariat Mtn; Harriot Mtn; Heriart Mtn; Heriot Mtn; Hiriat Hill), Pala, Pala Mining District, San Diego County, California, USA Vanderberg-Katerina pegmatites (Vanderburg-Katerina dikes; Vanderburg-Katerina pegmatites), Katerina Mine (Ashley mine; Caterina mine; Catherin mine; Catherina mine; Katrina mine), Hiriart Mountain (Hariat Mtn; Harriot Mtn; Heriart Mtn; Heriot Mtn; Hiriat Hill), Pala, Pala Mining District, San Diego County, California, USA References: |
ⓘ Orthoclase Formula: K(AlSi3O8) |
ⓘ Phenakite Formula: Be2SiO4 Colour: Colorless Description: Phenakite forms both flat, colorless crystals with sharply defined faces, and subhedral masses that are distinctly milky. It is associated with very small crystals of white to pale-blue topaz, and both minerals are attached to the exposed edges of large cleavelandite aggregates in the pocket pegmatite. None of the phenakite crystals exceeds 1/2 inch (12.7mm) in dimension. |
ⓘ Pseudomalachite Formula: Cu5(PO4)2(OH)4 Habit: Irregular masses and tiny blebs which are vitreous and conchoidal. Colour: Dark green to light bluish green. Description: Pseudomalachite averaging 5mm across; hosted in greenish feldspar; associated minerals include minor purple strengite, dark brown sicklerite, and reddish brown kaolinite. |
ⓘ Pucherite Formula: Bi(VO4) Localities: Katerina Mine (Ashley mine; Caterina mine; Catherin mine; Catherina mine; Katrina mine), Hiriart Mountain (Hariat Mtn; Harriot Mtn; Heriart Mtn; Heriot Mtn; Hiriat Hill), Pala, Pala Mining District, San Diego County, California, USA Vanderberg-Katerina pegmatites (Vanderburg-Katerina dikes; Vanderburg-Katerina pegmatites), Katerina Mine (Ashley mine; Caterina mine; Catherin mine; Catherina mine; Katrina mine), Hiriart Mountain (Hariat Mtn; Harriot Mtn; Heriart Mtn; Heriot Mtn; Hiriat Hill), Pala, Pala Mining District, San Diego County, California, USA |
ⓘ Quartz Formula: SiO2 Localities: Katerina Mine (Ashley mine; Caterina mine; Catherin mine; Catherina mine; Katrina mine), Hiriart Mountain (Hariat Mtn; Harriot Mtn; Heriart Mtn; Heriot Mtn; Hiriat Hill), Pala, Pala Mining District, San Diego County, California, USA Vanderberg-Katerina pegmatites (Vanderburg-Katerina dikes; Vanderburg-Katerina pegmatites), Katerina Mine (Ashley mine; Caterina mine; Catherin mine; Catherina mine; Katrina mine), Hiriart Mountain (Hariat Mtn; Harriot Mtn; Heriart Mtn; Heriot Mtn; Hiriat Hill), Pala, Pala Mining District, San Diego County, California, USA References: |
ⓘ Quartz var. Smoky Quartz Formula: SiO2 References: |
ⓘ Schorl Formula: NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH) References: |
ⓘ Spodumene Formula: LiAlSi2O6 References: |
ⓘ Spodumene var. Kunzite Formula: LiAlSi2O6 |
ⓘ Stibiotantalite Formula: Sb(Ta,Nb)O4 Description: Two crystals of stibiotantalite were observed in the Katerina mine, where they were in close association with coarse-grained cleavelandite, quartz, orthoclase, and colorless to pinkish beryl. The crystals were near several clusters of manganotantalite tablets, which they resembled in color and luster. In contrast, however, the antimony mineral showed a perfect cleavage. |
ⓘ Tantalite-(Mn) Formula: Mn2+Ta2O6 Localities: Katerina Mine (Ashley mine; Caterina mine; Catherin mine; Catherina mine; Katrina mine), Hiriart Mountain (Hariat Mtn; Harriot Mtn; Heriart Mtn; Heriot Mtn; Hiriat Hill), Pala, Pala Mining District, San Diego County, California, USA Vanderberg-Katerina pegmatites (Vanderburg-Katerina dikes; Vanderburg-Katerina pegmatites), Katerina Mine (Ashley mine; Caterina mine; Catherin mine; Catherina mine; Katrina mine), Hiriart Mountain (Hariat Mtn; Harriot Mtn; Heriart Mtn; Heriot Mtn; Hiriat Hill), Pala, Pala Mining District, San Diego County, California, USA References: |
ⓘ Topaz Formula: Al2(SiO4)(F,OH)2 Colour: White to pale-blue Description: Very small crystals of white to pale-blue topaz are associated with colorless crystals of phenakite, and both are attached to the exposed edges of large cleavelandite aggregates in the pocket pegmatite. |
ⓘ 'Tourmaline' Formula: AD3G6 (T6O18)(BO3)3X3Z References: |
ⓘ Triplite Formula: Mn2+2(PO4)F Habit: Tabular and fracture-filling masses with rough faces; cleavage is fairly well developed. Colour: Deep-tan to dark reddish-brown on freshly broken surfaces; resinous luster. Description: Triplite occurs sparingly in the Vanderberg-Katerina pegmatites, where it is associated with lithiophilite and triphylite. It forms crystals with rough faces, measuring 1/4 inch to 5 inches in diameter, with an average of about an inch. The mineral also occurs as tabular, fracture-filling masses within quartz, and rarely within coarse quartz-spodumene or quartz-perthite varieties of pegmatite. Most crystals are heavily stained with manganese oxides, and many are coated with a blue-gray film of very finely crystalline vivianite. The vivianite appears to have been derived from the triplite crystals. |
ⓘ Vivianite Formula: Fe2+Fe2+2(PO4)2 · 8H2O Habit: Very finely crystalline Colour: Blue-gray Description: A blue-gray film of very finely crystalline vivianite coats many triplite crystals. The vivianite appears to have been derived from the triplite crystals. |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 4 - Oxides and Hydroxides | |||
---|---|---|---|
ⓘ | Quartz var. Smoky Quartz | 4.DA.05 | SiO2 |
ⓘ | 4.DA.05 | SiO2 | |
ⓘ | Columbite-(Fe) | 4.DB.35 | Fe2+Nb2O6 |
ⓘ | Tantalite-(Mn) | 4.DB.35 | Mn2+Ta2O6 |
ⓘ | Stibiotantalite | 4.DE.30 | Sb(Ta,Nb)O4 |
Group 8 - Phosphates, Arsenates and Vanadates | |||
ⓘ | Lithiophilite | 8.AB.10 | LiMn2+PO4 |
ⓘ | Pucherite | 8.AD.40 | Bi(VO4) |
ⓘ | Amblygonite | 8.BB.05 | LiAl(PO4)F |
ⓘ | Triplite | 8.BB.10 | Mn2+2(PO4)F |
ⓘ | Pseudomalachite | 8.BD.05 | Cu5(PO4)2(OH)4 |
ⓘ | Fluorapatite | 8.BN.05 | Ca5(PO4)3F |
ⓘ | Vivianite | 8.CE.40 | Fe2+Fe2+2(PO4)2 · 8H2O |
Group 9 - Silicates | |||
ⓘ | Phenakite | 9.AA.05 | Be2SiO4 |
ⓘ | Topaz | 9.AF.35 | Al2(SiO4)(F,OH)2 |
ⓘ | Bertrandite | 9.BD.05 | Be4(Si2O7)(OH)2 |
ⓘ | Beryl | 9.CJ.05 | Be3Al2(Si6O18) |
ⓘ | var. Morganite | 9.CJ.05 | Be3Al2(Si6O18) |
ⓘ | var. Goshenite | 9.CJ.05 | Be3Al2(Si6O18) |
ⓘ | Foitite ? | 9.CK.05 | ◻(Fe2+2Al)Al6(Si6O18)(BO3)3(OH)3(OH) |
ⓘ | Schorl | 9.CK.05 | NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH) |
ⓘ | Spodumene var. Kunzite | 9.DA.30 | LiAlSi2O6 |
ⓘ | 9.DA.30 | LiAlSi2O6 | |
ⓘ | Muscovite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
ⓘ | Cookeite | 9.EC.55 | (LiAl4◻)[AlSi3O10](OH)8 |
ⓘ | Orthoclase | 9.FA.30 | K(AlSi3O8) |
ⓘ | Microcline | 9.FA.30 | K(AlSi3O8) |
ⓘ | Albite var. Cleavelandite | 9.FA.35 | Na(AlSi3O8) |
ⓘ | 9.FA.35 | Na(AlSi3O8) | |
ⓘ | Helvine | 9.FB.10 | Be3Mn2+4(SiO4)3S |
Unclassified | |||
ⓘ | 'Tourmaline' | - | AD3G6 (T6O18)(BO3)3X3Z |
ⓘ | 'Lepidolite' | - | |
ⓘ | 'Indicolite' | - | A(D3)G6(T6O18)(BO3)3X3Z |
ⓘ | 'Feldspar Group var. Perthite' | - | |
ⓘ | '' | - | |
ⓘ | 'Columbite-Tantalite' | - |
List of minerals for each chemical element
H | Hydrogen | |
---|---|---|
H | ⓘ Bertrandite | Be4(Si2O7)(OH)2 |
H | ⓘ Cookeite | (LiAl4◻)[AlSi3O10](OH)8 |
H | ⓘ Foitite | ◻(Fe22+Al)Al6(Si6O18)(BO3)3(OH)3(OH) |
H | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
H | ⓘ Pseudomalachite | Cu5(PO4)2(OH)4 |
H | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
H | ⓘ Topaz | Al2(SiO4)(F,OH)2 |
H | ⓘ Vivianite | Fe2+Fe22+(PO4)2 · 8H2O |
Li | Lithium | |
Li | ⓘ Amblygonite | LiAl(PO4)F |
Li | ⓘ Cookeite | (LiAl4◻)[AlSi3O10](OH)8 |
Li | ⓘ Spodumene var. Kunzite | LiAlSi2O6 |
Li | ⓘ Lithiophilite | LiMn2+PO4 |
Li | ⓘ Spodumene | LiAlSi2O6 |
Be | Beryllium | |
Be | ⓘ Bertrandite | Be4(Si2O7)(OH)2 |
Be | ⓘ Beryl | Be3Al2(Si6O18) |
Be | ⓘ Helvine | Be3Mn42+(SiO4)3S |
Be | ⓘ Beryl var. Morganite | Be3Al2(Si6O18) |
Be | ⓘ Phenakite | Be2SiO4 |
Be | ⓘ Beryl var. Goshenite | Be3Al2(Si6O18) |
B | Boron | |
B | ⓘ Foitite | ◻(Fe22+Al)Al6(Si6O18)(BO3)3(OH)3(OH) |
B | ⓘ Indicolite | A(D3)G6(T6O18)(BO3)3X3Z |
B | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
B | ⓘ Tourmaline | AD3G6 (T6O18)(BO3)3X3Z |
O | Oxygen | |
O | ⓘ Albite | Na(AlSi3O8) |
O | ⓘ Amblygonite | LiAl(PO4)F |
O | ⓘ Bertrandite | Be4(Si2O7)(OH)2 |
O | ⓘ Beryl | Be3Al2(Si6O18) |
O | ⓘ Cookeite | (LiAl4◻)[AlSi3O10](OH)8 |
O | ⓘ Columbite-(Fe) | Fe2+Nb2O6 |
O | ⓘ Fluorapatite | Ca5(PO4)3F |
O | ⓘ Foitite | ◻(Fe22+Al)Al6(Si6O18)(BO3)3(OH)3(OH) |
O | ⓘ Helvine | Be3Mn42+(SiO4)3S |
O | ⓘ Indicolite | A(D3)G6(T6O18)(BO3)3X3Z |
O | ⓘ Spodumene var. Kunzite | LiAlSi2O6 |
O | ⓘ Lithiophilite | LiMn2+PO4 |
O | ⓘ Tantalite-(Mn) | Mn2+Ta2O6 |
O | ⓘ Microcline | K(AlSi3O8) |
O | ⓘ Beryl var. Morganite | Be3Al2(Si6O18) |
O | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
O | ⓘ Orthoclase | K(AlSi3O8) |
O | ⓘ Phenakite | Be2SiO4 |
O | ⓘ Pseudomalachite | Cu5(PO4)2(OH)4 |
O | ⓘ Pucherite | Bi(VO4) |
O | ⓘ Quartz | SiO2 |
O | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
O | ⓘ Quartz var. Smoky Quartz | SiO2 |
O | ⓘ Spodumene | LiAlSi2O6 |
O | ⓘ Stibiotantalite | Sb(Ta,Nb)O4 |
O | ⓘ Topaz | Al2(SiO4)(F,OH)2 |
O | ⓘ Tourmaline | AD3G6 (T6O18)(BO3)3X3Z |
O | ⓘ Triplite | Mn22+(PO4)F |
O | ⓘ Vivianite | Fe2+Fe22+(PO4)2 · 8H2O |
O | ⓘ Beryl var. Goshenite | Be3Al2(Si6O18) |
O | ⓘ Albite var. Cleavelandite | Na(AlSi3O8) |
F | Fluorine | |
F | ⓘ Amblygonite | LiAl(PO4)F |
F | ⓘ Fluorapatite | Ca5(PO4)3F |
F | ⓘ Topaz | Al2(SiO4)(F,OH)2 |
F | ⓘ Triplite | Mn22+(PO4)F |
Na | Sodium | |
Na | ⓘ Albite | Na(AlSi3O8) |
Na | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
Na | ⓘ Albite var. Cleavelandite | Na(AlSi3O8) |
Al | Aluminium | |
Al | ⓘ Albite | Na(AlSi3O8) |
Al | ⓘ Amblygonite | LiAl(PO4)F |
Al | ⓘ Beryl | Be3Al2(Si6O18) |
Al | ⓘ Cookeite | (LiAl4◻)[AlSi3O10](OH)8 |
Al | ⓘ Foitite | ◻(Fe22+Al)Al6(Si6O18)(BO3)3(OH)3(OH) |
Al | ⓘ Spodumene var. Kunzite | LiAlSi2O6 |
Al | ⓘ Microcline | K(AlSi3O8) |
Al | ⓘ Beryl var. Morganite | Be3Al2(Si6O18) |
Al | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
Al | ⓘ Orthoclase | K(AlSi3O8) |
Al | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
Al | ⓘ Spodumene | LiAlSi2O6 |
Al | ⓘ Topaz | Al2(SiO4)(F,OH)2 |
Al | ⓘ Beryl var. Goshenite | Be3Al2(Si6O18) |
Al | ⓘ Albite var. Cleavelandite | Na(AlSi3O8) |
Si | Silicon | |
Si | ⓘ Albite | Na(AlSi3O8) |
Si | ⓘ Bertrandite | Be4(Si2O7)(OH)2 |
Si | ⓘ Beryl | Be3Al2(Si6O18) |
Si | ⓘ Cookeite | (LiAl4◻)[AlSi3O10](OH)8 |
Si | ⓘ Foitite | ◻(Fe22+Al)Al6(Si6O18)(BO3)3(OH)3(OH) |
Si | ⓘ Helvine | Be3Mn42+(SiO4)3S |
Si | ⓘ Spodumene var. Kunzite | LiAlSi2O6 |
Si | ⓘ Microcline | K(AlSi3O8) |
Si | ⓘ Beryl var. Morganite | Be3Al2(Si6O18) |
Si | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
Si | ⓘ Orthoclase | K(AlSi3O8) |
Si | ⓘ Phenakite | Be2SiO4 |
Si | ⓘ Quartz | SiO2 |
Si | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
Si | ⓘ Quartz var. Smoky Quartz | SiO2 |
Si | ⓘ Spodumene | LiAlSi2O6 |
Si | ⓘ Topaz | Al2(SiO4)(F,OH)2 |
Si | ⓘ Beryl var. Goshenite | Be3Al2(Si6O18) |
Si | ⓘ Albite var. Cleavelandite | Na(AlSi3O8) |
P | Phosphorus | |
P | ⓘ Amblygonite | LiAl(PO4)F |
P | ⓘ Fluorapatite | Ca5(PO4)3F |
P | ⓘ Lithiophilite | LiMn2+PO4 |
P | ⓘ Pseudomalachite | Cu5(PO4)2(OH)4 |
P | ⓘ Triplite | Mn22+(PO4)F |
P | ⓘ Vivianite | Fe2+Fe22+(PO4)2 · 8H2O |
S | Sulfur | |
S | ⓘ Helvine | Be3Mn42+(SiO4)3S |
K | Potassium | |
K | ⓘ Microcline | K(AlSi3O8) |
K | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
K | ⓘ Orthoclase | K(AlSi3O8) |
Ca | Calcium | |
Ca | ⓘ Fluorapatite | Ca5(PO4)3F |
V | Vanadium | |
V | ⓘ Pucherite | Bi(VO4) |
Mn | Manganese | |
Mn | ⓘ Helvine | Be3Mn42+(SiO4)3S |
Mn | ⓘ Lithiophilite | LiMn2+PO4 |
Mn | ⓘ Tantalite-(Mn) | Mn2+Ta2O6 |
Mn | ⓘ Triplite | Mn22+(PO4)F |
Fe | Iron | |
Fe | ⓘ Columbite-(Fe) | Fe2+Nb2O6 |
Fe | ⓘ Foitite | ◻(Fe22+Al)Al6(Si6O18)(BO3)3(OH)3(OH) |
Fe | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
Fe | ⓘ Vivianite | Fe2+Fe22+(PO4)2 · 8H2O |
Cu | Copper | |
Cu | ⓘ Pseudomalachite | Cu5(PO4)2(OH)4 |
Nb | Niobium | |
Nb | ⓘ Columbite-(Fe) | Fe2+Nb2O6 |
Nb | ⓘ Stibiotantalite | Sb(Ta,Nb)O4 |
Sb | Antimony | |
Sb | ⓘ Stibiotantalite | Sb(Ta,Nb)O4 |
Ta | Tantalum | |
Ta | ⓘ Tantalite-(Mn) | Mn2+Ta2O6 |
Ta | ⓘ Stibiotantalite | Sb(Ta,Nb)O4 |
Bi | Bismuth | |
Bi | ⓘ Pucherite | Bi(VO4) |
Localities in this Region
- California
- San Diego County
- Pala Mining District
- Pala
- Hiriart Mountain (Hariat Mtn; Harriot Mtn; Heriart Mtn; Heriot Mtn; Hiriat Hill)
- Katerina Mine (Ashley mine; Caterina mine; Catherin mine; Catherina mine; Katrina mine)
- Hiriart Mountain (Hariat Mtn; Harriot Mtn; Heriart Mtn; Heriot Mtn; Hiriat Hill)
- Pala
- Pala Mining District
- San Diego County
Other Regions, Features and Areas containing this locality
North America Plate
Pacific PlateTectonic Plate
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Katerina Mine, Hiriart Mountain, Pala, Pala Mining District, San Diego County, California, USA