Rare Earth Elements Gemology Gold Deposits Diamonds Sedimentary Rocks Mineral Deposits Mineral Exploration Iron Oxides Meteorite Composition Sulfur Compounds Igneous Rocks Meteorites Critical Minerals Clay Minerals Ore Deposits Carbonate Minerals Olivine Chemical Composition Chemical Reactions Hydrated Minerals Sulfate Minerals Lunar Minerals Carbonates Zircon Crystals Silicate Minerals Volcanic Rocks Mineral Composition Rock Formation Natural Resources Stalagmites Diamond Formation Mineral Analysis Uranium Mineral Resources Hydrothermal Alteration Amber Quartz Salt Minerals Chondrites Chemical Processes Rock Analysis Material Analysis Martian Minerals Meteorite Analysis Crystallography Gemstones Crystalline Minerals Oxidation Processes Minerals Salt Deposits Elemental Sulfur Silicon Compounds Rock Composition Sulfur Crystals Lithium Zircon Fossils Polymetallic Deposits Geochemistry Evaporites Evaporite Minerals Pyroxene Rare Earth Metals Ferrihydrite Radioactive Elements Critical Minerals Research Zeolites Calcium Carbonate Concretions Carbon-Rich Worlds Organic Compounds Uranium Deposits Precious Metals Resource Assessment Sulphate Minerals Siderite Phosphates Hydroxyl Groups Carbonatite Systems Shock-Altered Minerals Gold Systems Isotope Geochemistry Gold Silicon Oxide Jadarite Resource Management Cosmic Minerals Rare Minerals Mineral Formation Iron Minerals Djerfisherit Exploration Techniques Manganese Mineral Identification Martian Rocks Rare Earth Minerals Resource Identification Mining Engineering Lithium Resources Chemical Analysis
Peer-reviewed shock evidence in quartz confirms a meteorite strike.