Maple Lode Mine (Maple claim), Aguanga Mountain, Oak Grove, Aguanga Mountain Mining District (Smith Mountain Mining District), San Diego County, California, USAi
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Latitude & Longitude (WGS84):
33° 19' 26'' North , 116° 45' 56'' West
Latitude & Longitude (decimal):
Type:
Mine - last checked 2023
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Aguanga | 1,128 (2011) | 16.1km |
| Anza | 3,014 (2011) | 27.1km |
| Valley Center | 9,277 (2011) | 27.6km |
| San Pasqual | 2,041 (2018) | 31.2km |
| Julian | 1,502 (2011) | 31.2km |
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 |
|---|---|---|
| Borrego Rock and Gem Club | Borrego Springs, California | 37km |
| Palomar Gem & Mineral Club | Escondido, California | 37km |
| Fallbrook Gem and Mineral Society, Inc. | Fallbrook, California | 45km |
| Vista Gem & Mineral Society | Vista, California | 46km |
Setting:
A gemstone mine located in the S½NW¼ Sec. 13, T9S, R3E, SBM, situated southwest of the crest of Aguanga Mountain. The property consists of a single unpatented lode mining claim aggregating 20 acres, more or less.
History:
The Maple Lode is a gem-bearing pegmatite deposit first discovered by Bert Simmons around 1902, and later claimed by Bill Dyche. The deposit was worked by Dyche and his men for gem-quality blue tourmaline and blue topaz. The main working face consisted of a shallow adit which extended nearly 27 feet into the ledge following a series of pockets.
The deposit was claimed again in 1915 by Fred Rynerson who briefly worked the ledge with Henry Stenbock. Rynerson discovered one exceptionally fine blue topaz crystal which measured 1 inch tall by one half inch wide, associated with blue tourmaline, about 10 feet back along the east wall of the underground workings.
The mine was later claimed as the Maple Lode, and worked for several years by Mr. MacMillan of Sunshine Summit. MacMillan was said to have developed a second adit about 8 feet above the original underground workings, producing a small quantity of gem material. This new adit was described as an irregular, partially gophered working which extended back nearly 20 feet from the surface, and was connected to the lower main adit by a short raise. The main adit was also extended an additional 23 feet underground, although these workings were said to have partially caved afterward. MacMillan sold his claim to Del Flatz of San Diego in 1959.
In the late 1970's and early 1980's, Roland Reed and several partners worked the deposit using heavy equipment to strip overburden and develop a large bench cut along the pegmatite exposure, removing most of the old underground workings during the process. A claim to the deposit was located by Roland Reed and John E. Gregory of Alpine on November 2, 1985. Work by Reed and others produced several topaz crystals ranging in color from medium blue to pale green, and a few small matrix specimens of topaz on lepidolite and albite were also recovered. Additionally, numerous blue and blue-pink bicolor elbaite crystals were discovered, usually occurring as slender gem pencils up to 5cm long, some of them being a bright sky-blue color. A few pinkish-red colored apatite crystals were also found, up to 7.5cm in size and displaying a tabular habit. Reed later transferred his interest in the claim to Gregory on July 28, 2000. Gregory transferred his interest to Cal Graeber and Jeffrey Kent in 2009.
On September 01, 2021 the unpatented Maple Lode claim became invalid due to the Graeber & Kent's failure to file annual papers and fees on the claim required by BLM under the federal mining laws. The Maple Lode was subsequently relocated by Christopher Wentzell on September 23, 2021 and registered as BLM Serial #CA105275076. Wentzell sold the claim to Corey Bauch in April/May 2025.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsDetailed Mineral List:
| ⓘ Albite Formula: Na(AlSi3O8) References: Troy Schmidt CollectionIdentification: Visual Identification, Dealer/Collection Label |
| ⓘ Albite var. Cleavelandite Formula: Na(AlSi3O8) References: Troy Schmidt CollectionIdentification: Visual Identification, Dealer/Collection Label |
| ⓘ Elbaite Formula: Na(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH) |
| ⓘ Fluorapatite Formula: Ca5(PO4)3F |
| ⓘ 'Garnet Group' Formula: X3Z2(SiO4)3 |
| ⓘ 'Lepidolite' |
| ⓘ Microcline Formula: K(AlSi3O8) |
| ⓘ Muscovite Formula: KAl2(AlSi3O10)(OH)2 Description: A significant constituent of dikes. |
| ⓘ Opal Formula: SiO2 · nH2O Description: Hyalite was observed to be coating quartz and feldspar crystals on the walls of a small vug discovered in the early 1990's by D. Bernstein of Century City. |
| ⓘ Opal var. Opal-AN Formula: SiO2 · nH2O Description: Hyalite was observed to be coating quartz and feldspar crystals on the walls of a small vug discovered in the early 1990's by D. Bernstein of Century City. |
| ⓘ Orthoclase Formula: K(AlSi3O8) |
| ⓘ 'Plagioclase' Formula: (Na,Ca)[(Si,Al)AlSi2]O8 |
| ⓘ Quartz Formula: SiO2 |
| ⓘ Schorl Formula: NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH) |
| ⓘ Spessartine Formula: Mn2+3Al2(SiO4)3 |
| ⓘ Topaz Formula: Al2(SiO4)(F,OH)2 |
| ⓘ 'Tourmaline' Formula: AD3G6(T6O18)(BO3)3X3Z |
| ⓘ 'Tourmaline var. Indicolite' References: |
| ⓘ 'Tourmaline var. Rubellite' |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 4 - Oxides and Hydroxides | |||
|---|---|---|---|
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| ⓘ | Opal var. Opal-AN | 4.DA.10 | SiO2 · nH2O |
| ⓘ | 4.DA.10 | SiO2 · nH2O | |
| Group 8 - Phosphates, Arsenates and Vanadates | |||
| ⓘ | Fluorapatite | 8.BN.05 | Ca5(PO4)3F |
| Group 9 - Silicates | |||
| ⓘ | Spessartine | 9.AD.25 | Mn2+3Al2(SiO4)3 |
| ⓘ | Topaz | 9.AF.35 | Al2(SiO4)(F,OH)2 |
| ⓘ | Elbaite | 9.CK.05 | Na(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH) |
| ⓘ | Schorl | 9.CK.05 | NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH) |
| ⓘ | Muscovite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| ⓘ | Microcline | 9.FA.30 | K(AlSi3O8) |
| ⓘ | Orthoclase | 9.FA.30 | K(AlSi3O8) |
| ⓘ | Albite | 9.FA.35 | Na(AlSi3O8) |
| ⓘ | var. Cleavelandite | 9.FA.35 | Na(AlSi3O8) |
| Unclassified | |||
| ⓘ | 'Tourmaline var. Indicolite' | - | AD3G6(T6O18)(BO3)3X3Z |
| ⓘ | 'Lepidolite' | - | |
| ⓘ | 'Tourmaline var. Rubellite' | - | AD3G6(T6O18)(BO3)3X3Z |
| ⓘ | '' | - | AD3G6(T6O18)(BO3)3X3Z |
| ⓘ | 'Plagioclase' | - | (Na,Ca)[(Si,Al)AlSi2]O8 |
| ⓘ | 'Garnet Group' | - | X3Z2(SiO4)3 |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Elbaite | Na(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH) |
| H | ⓘ Opal var. Opal-AN | SiO2 · nH2O |
| H | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| H | ⓘ Opal | SiO2 · nH2O |
| H | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
| H | ⓘ Topaz | Al2(SiO4)(F,OH)2 |
| Li | Lithium | |
| Li | ⓘ Elbaite | Na(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH) |
| B | Boron | |
| B | ⓘ Elbaite | Na(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH) |
| B | ⓘ Tourmaline var. Indicolite | |
| B | ⓘ Tourmaline var. Rubellite | |
| B | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
| B | ⓘ Tourmaline | AD3G6(T6O18)(BO3)3X3Z |
| O | Oxygen | |
| O | ⓘ Albite | Na(AlSi3O8) |
| O | ⓘ Elbaite | Na(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH) |
| O | ⓘ Fluorapatite | Ca5(PO4)3F |
| O | ⓘ Opal var. Opal-AN | SiO2 · nH2O |
| O | ⓘ Tourmaline var. Indicolite | |
| O | ⓘ Microcline | K(AlSi3O8) |
| O | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Opal | SiO2 · nH2O |
| O | ⓘ Orthoclase | K(AlSi3O8) |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Tourmaline var. Rubellite | |
| O | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
| O | ⓘ Spessartine | Mn32+Al2(SiO4)3 |
| O | ⓘ Topaz | Al2(SiO4)(F,OH)2 |
| O | ⓘ Tourmaline | AD3G6(T6O18)(BO3)3X3Z |
| O | ⓘ Albite var. Cleavelandite | Na(AlSi3O8) |
| O | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| O | ⓘ Garnet Group | X3Z2(SiO4)3 |
| F | Fluorine | |
| F | ⓘ Fluorapatite | Ca5(PO4)3F |
| F | ⓘ Topaz | Al2(SiO4)(F,OH)2 |
| Na | Sodium | |
| Na | ⓘ Albite | Na(AlSi3O8) |
| Na | ⓘ Elbaite | Na(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH) |
| Na | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
| Na | ⓘ Albite var. Cleavelandite | Na(AlSi3O8) |
| Na | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Al | Aluminium | |
| Al | ⓘ Albite | Na(AlSi3O8) |
| Al | ⓘ Elbaite | Na(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH) |
| Al | ⓘ Microcline | K(AlSi3O8) |
| Al | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Al | ⓘ Orthoclase | K(AlSi3O8) |
| Al | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
| Al | ⓘ Spessartine | Mn32+Al2(SiO4)3 |
| Al | ⓘ Topaz | Al2(SiO4)(F,OH)2 |
| Al | ⓘ Albite var. Cleavelandite | Na(AlSi3O8) |
| Al | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Si | Silicon | |
| Si | ⓘ Albite | Na(AlSi3O8) |
| Si | ⓘ Elbaite | Na(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH) |
| Si | ⓘ Opal var. Opal-AN | SiO2 · nH2O |
| Si | ⓘ Microcline | K(AlSi3O8) |
| Si | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Opal | SiO2 · nH2O |
| Si | ⓘ Orthoclase | K(AlSi3O8) |
| Si | ⓘ Quartz | SiO2 |
| Si | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
| Si | ⓘ Spessartine | Mn32+Al2(SiO4)3 |
| Si | ⓘ Topaz | Al2(SiO4)(F,OH)2 |
| Si | ⓘ Albite var. Cleavelandite | Na(AlSi3O8) |
| Si | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Si | ⓘ Garnet Group | X3Z2(SiO4)3 |
| P | Phosphorus | |
| P | ⓘ Fluorapatite | Ca5(PO4)3F |
| K | Potassium | |
| K | ⓘ Microcline | K(AlSi3O8) |
| K | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| K | ⓘ Orthoclase | K(AlSi3O8) |
| Ca | Calcium | |
| Ca | ⓘ Fluorapatite | Ca5(PO4)3F |
| Ca | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Mn | Manganese | |
| Mn | ⓘ Spessartine | Mn32+Al2(SiO4)3 |
| Fe | Iron | |
| Fe | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
Other Regions, Features and Areas containing this locality
North AmericaContinent
North America Plate
- Franciscan DomainDomain
- Peninsular Ranges BatholithVolcanic Arc
- Southern California Borderland BasinsBasin
Pacific PlateTectonic Plate
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Maple Lode Mine, Aguanga Mountain, Oak Grove, Aguanga Mountain Mining District, San Diego County, California, USA