Magnesiopascoite

A variety of Minerals

Magnesiopascoite specimen

What is Magnesiopascoite?

Magnesiopascoite is a member of the pascoite group and is the magnesium analogue of pascoite. It is transparent and bright orange in color, occurring as intergrown, parallel stackings of crystals up to several millimeters in the largest dimension. The crystals vary from tabular to equant to prismatic. The mineral dissolves slowly in water and quickly in cold, dilute hydrochloric acid. It decomposes rapidly when mildly heated, likely as a result of dehydration.

Market Value Factors

Pricing varies for every rock and mineral, so use these universal factors to gauge Magnesiopascoite before comparing listings or appraisals.

Size & Weight

Larger, intact specimens usually command higher prices.

Rarity & Demand

Scarce material or popular varieties sell at a premium.

Condition & Finish

Chips, repairs, and heavy wear lower value; clean prep helps.

Treatment & Provenance

Untreated specimens with documented locality are prized.

Applies to all rocks & minerals.

Magnesiopascoite Localities Map

See where Magnesiopascoite is found with a localities map, collecting zones, and geology context. Generate a sample map preview below.

Map preview
North ZoneCentral RidgeSouth Basin

Interactive map layers and collecting notes are available in the app.

Key Characteristics

Formation of Magnesiopascoite

In the area of the type locality, the reducing environment caused by carbonaceous material in the Salt Wash and Brushy Basin members of the Morrison Formation precipitated uranium and vanadium minerals from solution. After mining, subsequent leaching and oxidation by groundwater created magnesiopascoite. The mineral has been found in association with gypsum, martyite, montroseite, pyrite and rossite.

Quick Facts

Chemical Properties

Chemical Formula
Ca2Mg(V10O28) · 16H2O
Elements
Ca, H, Mg, O, V
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Magnesiopascoite FAQs

What is the formation of magnesiopascoite of Magnesiopascoite?

In the area of the type locality, the reducing environment caused by carbonaceous material in the Salt Wash and Brushy Basin members of the Morrison Formation precipitated uranium and vanadium minerals from solution. After mining, subsequent leaching and oxidation by groundwater created magnesiopascoite. The mineral has been found in association with gypsum, martyite, montroseite, pyrite and rossite.

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