Difficulty: Easy
Correct Answer: Pitchblende (uraninite)
Explanation:
Introduction / Context:
Identifying uranium-rich minerals is important in mining, fuel-cycle planning, and general science GK. Different ores vary widely in uranium concentration and in the presence of other actinides or rare-earth elements.
Given Data / Assumptions:
Concept / Approach:
Pitchblende (also known as uraninite) is essentially uranium dioxide-rich mineral and is historically the most uranium-dense ore, often the primary source in high-grade deposits. Carnotite is a potassium–uranium–vanadium mineral with lower U content. Monazite sands are largely rare-earth phosphates with thorium and only modest uranium traces. Thorite is primarily a thorium mineral. “Rescolite” is not a standard uranium ore name in typical mining catalogs and may represent a distractor or misnomer.
Step-by-Step Solution:
Recall mineral compositions: uraninite (UO2±x) is highly uranium-rich.Compare with carnotite and monazite: uranium present but at lower percentages.Exclude thorium-dominant minerals (thorite) and nonstandard names.Select pitchblende/uraninite as the richest uranium ore.
Verification / Alternative check:
Historical mining records and geochemical references consistently cite high-grade uraninite/pitchblende veins as the most uranium-concentrated mineralized material used in extraction.
Why Other Options Are Wrong:
Carnotite: Uranium present but diluted by K and V components.Thorite: Predominantly thorium; not a high-U mineral.Rescolite: Not a recognized primary uranium ore.Monazite: Rare-earth phosphate with thorium; uranium is minor.
Common Pitfalls:
Assuming any actinide-bearing sand (monazite) is uranium-rich; many are thorium-dominant. Always match mineral identity with its primary actinide content.
Final Answer:
Pitchblende (uraninite)
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