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Latitude & Longitude (WGS84):
33° 19' 26'' North , 116° 45' 56'' West
Latitude & Longitude (decimal):
Type:
Mine - last checked 2023
Nearest Settlements:
PlacePopulationDistance
Aguanga1,128 (2011)16.1km
Anza3,014 (2011)27.1km
Valley Center9,277 (2011)27.6km
San Pasqual2,041 (2018)31.2km
Julian1,502 (2011)31.2km
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
ClubLocationDistance
Borrego Rock and Gem ClubBorrego Springs, California37km
Palomar Gem & Mineral ClubEscondido, California37km
Fallbrook Gem and Mineral Society, Inc.Fallbrook, California45km
Vista Gem & Mineral SocietyVista, California46km
Mindat Locality ID:
91432
Long-form identifier:
mindat:1:2:91432:6
GUID (UUID V4):
0


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 Elements

Mineral List


11 valid minerals.

Detailed Mineral List:

Albite
Formula: Na(AlSi3O8)
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'
'Tourmaline var. Rubellite'

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 4 - Oxides and Hydroxides
Quartz4.DA.05SiO2
Opal
var. Opal-AN
4.DA.10SiO2 · nH2O
4.DA.10SiO2 · nH2O
Group 8 - Phosphates, Arsenates and Vanadates
Fluorapatite8.BN.05Ca5(PO4)3F
Group 9 - Silicates
Spessartine9.AD.25Mn2+3Al2(SiO4)3
Topaz9.AF.35Al2(SiO4)(F,OH)2
Elbaite9.CK.05Na(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)
Schorl9.CK.05NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH)
Muscovite9.EC.15KAl2(AlSi3O10)(OH)2
Microcline9.FA.30K(AlSi3O8)
Orthoclase9.FA.30K(AlSi3O8)
Albite9.FA.35Na(AlSi3O8)
var. Cleavelandite9.FA.35Na(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

HHydrogen
H ElbaiteNa(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)
H Opal var. Opal-ANSiO2 · nH2O
H MuscoviteKAl2(AlSi3O10)(OH)2
H OpalSiO2 · nH2O
H SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
H TopazAl2(SiO4)(F,OH)2
LiLithium
Li ElbaiteNa(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)
BBoron
B ElbaiteNa(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)
B Tourmaline var. Indicolite
B Tourmaline var. Rubellite
B SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
B TourmalineAD3G6(T6O18)(BO3)3X3Z
OOxygen
O AlbiteNa(AlSi3O8)
O ElbaiteNa(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)
O FluorapatiteCa5(PO4)3F
O Opal var. Opal-ANSiO2 · nH2O
O Tourmaline var. Indicolite
O MicroclineK(AlSi3O8)
O MuscoviteKAl2(AlSi3O10)(OH)2
O OpalSiO2 · nH2O
O OrthoclaseK(AlSi3O8)
O QuartzSiO2
O Tourmaline var. Rubellite
O SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
O SpessartineMn32+Al2(SiO4)3
O TopazAl2(SiO4)(F,OH)2
O TourmalineAD3G6(T6O18)(BO3)3X3Z
O Albite var. CleavelanditeNa(AlSi3O8)
O Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
O Garnet GroupX3Z2(SiO4)3
FFluorine
F FluorapatiteCa5(PO4)3F
F TopazAl2(SiO4)(F,OH)2
NaSodium
Na AlbiteNa(AlSi3O8)
Na ElbaiteNa(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)
Na SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Na Albite var. CleavelanditeNa(AlSi3O8)
Na Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
AlAluminium
Al AlbiteNa(AlSi3O8)
Al ElbaiteNa(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)
Al MicroclineK(AlSi3O8)
Al MuscoviteKAl2(AlSi3O10)(OH)2
Al OrthoclaseK(AlSi3O8)
Al SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Al SpessartineMn32+Al2(SiO4)3
Al TopazAl2(SiO4)(F,OH)2
Al Albite var. CleavelanditeNa(AlSi3O8)
Al Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
SiSilicon
Si AlbiteNa(AlSi3O8)
Si ElbaiteNa(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)
Si Opal var. Opal-ANSiO2 · nH2O
Si MicroclineK(AlSi3O8)
Si MuscoviteKAl2(AlSi3O10)(OH)2
Si OpalSiO2 · nH2O
Si OrthoclaseK(AlSi3O8)
Si QuartzSiO2
Si SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Si SpessartineMn32+Al2(SiO4)3
Si TopazAl2(SiO4)(F,OH)2
Si Albite var. CleavelanditeNa(AlSi3O8)
Si Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Si Garnet GroupX3Z2(SiO4)3
PPhosphorus
P FluorapatiteCa5(PO4)3F
KPotassium
K MicroclineK(AlSi3O8)
K MuscoviteKAl2(AlSi3O10)(OH)2
K OrthoclaseK(AlSi3O8)
CaCalcium
Ca FluorapatiteCa5(PO4)3F
Ca Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
MnManganese
Mn SpessartineMn32+Al2(SiO4)3
FeIron
Fe SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)

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