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URL: https://www.mindat.org/loc-399346.html

⇱ Mc Gregor Quarry, Highway 26, Clatsop County, Oregon, USA


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Mc Gregor Quarry, Highway 26, Clatsop County, Oregon, USAi
Regional Level Types
Mc Gregor QuarryQuarry (Active)
Highway 26Road
Clatsop CountyCounty
OregonState
USACountry

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Latitude & Longitude (WGS84):
45° 48' 28'' North , 123° 25' 49'' West
Latitude & Longitude (decimal):
Type:
Quarry (Active) - last checked 2020
Deposit first discovered:
2019
Nearest Settlements:
PlacePopulationDistance
Vernonia2,143 (2017)19.2km
Banks1,934 (2017)32.3km
Westport321 (2011)36.3km
Clatskanie1,759 (2017)36.9km
Nehalem278 (2017)37.3km
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
ClubLocationDistance
Tualatin Valley Gem ClubForest Grove, Oregon41km
North American Research GroupHillsboro, Oregon47km
Mindat Locality ID:
399346
Long-form identifier:
mindat:1:2:399346:3
GUID (UUID V4):
0


Originally shared with me by Michael Feehan, who knows the Oregon Coast Range better than just about anyone I've met. He found the locality looking for free gold, and shared it with me last year via a digital conversation, mentioning some unknown zeolites were present. Considering he now lives out of state, I had to investigate for both our sakes, and found a well hidden very large Quarry, with 5 major terraces/benches dug out, all around 700-900ft combined top to bottom. A combination of numerous rock types of similar chemistry are found around the quarry, with the same material being found on just about every level. The main rock type is Basalt, but there are basalt flows separated by marine sedimentary rocks, as well as lahar like tuff layers that have all experienced Zeolite facies metamorphism, as well as other types of hydrothermal alteration in addition. This is an active quarry, with equipment brought in every few months to break rocks down to make new logging roads, and for that reason, travel on the roads, as well as digging at the quarry requires good discretion and attention to safety for all. Workers have been kind enough to let me work safely away from them in the past, but I don't think anyone should push their luck...

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


11 valid minerals.

Detailed Mineral List:

Amicite ?
Formula: K2Na2Al4Si4O16 · 5H2O
References:
Baryte
Formula: BaSO4
References:
Calcite
Formula: CaCO3
References:
Celadonite
Formula: K(MgFe3+◻)(Si4O10)(OH)2
References:
'Chlorite Group'
References:
Harmotome
Formula: Ba2(Si12Al4)O32 · 12H2O
References:
'Heulandite Subgroup'
Formula: (Na/Ca/K)5-6[Al8-9 Si27-28 O72] · nH2O
References:
Laumontite
Formula: CaAl2Si4O12 · 4H2O
References:
Marcasite
Formula: FeS2
References:
Mordenite
Formula: (Na2,Ca,K2)4(Al8Si40)O96 · 28H2O
References:
Natrolite
Formula: Na2Al2Si3O10 · 2H2O
References:
Pyrite
Formula: FeS2
References:
Quartz
Formula: SiO2
References:
'Smectite Group'
Formula: A0.3D2-3[T4O10]Z2 · nH2O
References:
'Stilbite Subgroup'
Formula: M6-7[Al8-9Si27-28O72] · nH2O
References:

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
Pyrite2.EB.05aFeS2
Marcasite2.EB.10aFeS2
Group 4 - Oxides and Hydroxides
Quartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
Calcite5.AB.05CaCO3
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
Baryte7.AD.35BaSO4
Group 9 - Silicates
Celadonite9.EC.15K(MgFe3+◻)(Si4O10)(OH)2
Natrolite9.GA.05Na2Al2Si3O10 · 2H2O
Laumontite9.GB.10CaAl2Si4O12 · 4H2O
Amicite ?9.GC.05K2Na2Al4Si4O16 · 5H2O
Harmotome9.GC.10Ba2(Si12Al4)O32 · 12H2O
Mordenite9.GD.35(Na2,Ca,K2)4(Al8Si40)O96 · 28H2O
Unclassified
'Chlorite Group'-
'Heulandite Subgroup'-(Na/Ca/K)5-6[Al8-9 Si27-28 O72] · nH2O
'Stilbite Subgroup'-M6-7[Al8-9Si27-28O72] · nH2O
'Smectite Group'-A0.3D2-3[T4O10]Z2 · nH2O

List of minerals for each chemical element

HHydrogen
H AmiciteK2Na2Al4Si4O16 · 5H2O
H CeladoniteK(MgFe3+◻)(Si4O10)(OH)2
H HarmotomeBa2(Si12Al4)O32 · 12H2O
H Heulandite Subgroup(Na/Ca/K)5-6[Al8-9 Si27-28 O72] · nH2O
H LaumontiteCaAl2Si4O12 · 4H2O
H Mordenite(Na2,Ca,K2)4(Al8Si40)O96 · 28H2O
H NatroliteNa2Al2Si3O10 · 2H2O
H Stilbite SubgroupM6-7[Al8-9Si27-28O72] · nH2O
H Smectite GroupA0.3D2-3[T4O10]Z2 · nH2O
CCarbon
C CalciteCaCO3
OOxygen
O AmiciteK2Na2Al4Si4O16 · 5H2O
O BaryteBaSO4
O CalciteCaCO3
O CeladoniteK(MgFe3+◻)(Si4O10)(OH)2
O HarmotomeBa2(Si12Al4)O32 · 12H2O
O Heulandite Subgroup(Na/Ca/K)5-6[Al8-9 Si27-28 O72] · nH2O
O LaumontiteCaAl2Si4O12 · 4H2O
O Mordenite(Na2,Ca,K2)4(Al8Si40)O96 · 28H2O
O NatroliteNa2Al2Si3O10 · 2H2O
O QuartzSiO2
O Stilbite SubgroupM6-7[Al8-9Si27-28O72] · nH2O
O Smectite GroupA0.3D2-3[T4O10]Z2 · nH2O
NaSodium
Na AmiciteK2Na2Al4Si4O16 · 5H2O
Na Heulandite Subgroup(Na/Ca/K)5-6[Al8-9 Si27-28 O72] · nH2O
Na Mordenite(Na2,Ca,K2)4(Al8Si40)O96 · 28H2O
Na NatroliteNa2Al2Si3O10 · 2H2O
MgMagnesium
Mg CeladoniteK(MgFe3+◻)(Si4O10)(OH)2
AlAluminium
Al AmiciteK2Na2Al4Si4O16 · 5H2O
Al HarmotomeBa2(Si12Al4)O32 · 12H2O
Al Heulandite Subgroup(Na/Ca/K)5-6[Al8-9 Si27-28 O72] · nH2O
Al LaumontiteCaAl2Si4O12 · 4H2O
Al Mordenite(Na2,Ca,K2)4(Al8Si40)O96 · 28H2O
Al NatroliteNa2Al2Si3O10 · 2H2O
Al Stilbite SubgroupM6-7[Al8-9Si27-28O72] · nH2O
SiSilicon
Si AmiciteK2Na2Al4Si4O16 · 5H2O
Si CeladoniteK(MgFe3+◻)(Si4O10)(OH)2
Si HarmotomeBa2(Si12Al4)O32 · 12H2O
Si Heulandite Subgroup(Na/Ca/K)5-6[Al8-9 Si27-28 O72] · nH2O
Si LaumontiteCaAl2Si4O12 · 4H2O
Si Mordenite(Na2,Ca,K2)4(Al8Si40)O96 · 28H2O
Si NatroliteNa2Al2Si3O10 · 2H2O
Si QuartzSiO2
Si Stilbite SubgroupM6-7[Al8-9Si27-28O72] · nH2O
SSulfur
S BaryteBaSO4
S MarcasiteFeS2
S PyriteFeS2
KPotassium
K AmiciteK2Na2Al4Si4O16 · 5H2O
K CeladoniteK(MgFe3+◻)(Si4O10)(OH)2
K Heulandite Subgroup(Na/Ca/K)5-6[Al8-9 Si27-28 O72] · nH2O
K Mordenite(Na2,Ca,K2)4(Al8Si40)O96 · 28H2O
CaCalcium
Ca CalciteCaCO3
Ca Heulandite Subgroup(Na/Ca/K)5-6[Al8-9 Si27-28 O72] · nH2O
Ca LaumontiteCaAl2Si4O12 · 4H2O
Ca Mordenite(Na2,Ca,K2)4(Al8Si40)O96 · 28H2O
FeIron
Fe CeladoniteK(MgFe3+◻)(Si4O10)(OH)2
Fe MarcasiteFeS2
Fe PyriteFeS2
BaBarium
Ba BaryteBaSO4
Ba HarmotomeBa2(Si12Al4)O32 · 12H2O

Other Regions, Features and Areas containing this locality


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