WEEK 8 - Metals Flashcards
What are Native Metals?
Metals found in their pure, elemental form in nature
Native Metals Historical Value
Their value in ancient times was partly due to their rarity
Examples of Native Metals
- Native Copper
- Native Gold
- Native Silver
What are metal compounds?
- Metal compounds are minerals where metals are combined with other elements like sulphur or oxygen.
Examples:
- Galena – lead sulphide
- Sphalerite – zinc sulphide
- Magnetite – iron oxide
Why were metal compounds important historically?
- The increased use of metals led to the development of smelting techniques to extract metals from these impure compounds.
- Smelting separated the metal from the sulphur or oxygen in the compounds, making metals like lead, zinc, and iron more accessible for use in tools, construction, and industry.
What are the general properties of metals?
- High electrical conductivity
- Luster (shiny appearance)
- Malleability (can be shaped without breaking)
- Ability to lose electrons and form positive ions (cations)
What are “fusible metals”?
- Metals of moderate hardness.
- They can be melted and combined with other metals to form alloys (mixtures of metals).
How are fusible metals classified?
- Precious metals
- Base metals
What are precious metals?
- Precious metals are metals that are rare and have high value (e.g., gold, silver, platinum).
- Often used for jewelry or coins
- They are desirable for electrical components due to their resistance to corrosion and oxidation.
What are base metals?
- Base metals are more common metals, often used in industry (e.g.,Iron, Lead, Copper, Zinc, Inc)
- Have low intrinsic value compared to precious metals.
- Most base metals oxidize (tarnish) in air.
- The term comes from the practice of alchemists trying to make gold from less valuable metals.
What makes up most of Earth’s crust?
98.5% of Earth’s crust (by weight) is made up of 8 elements:
- Oxygen (O) - 46.6%
- Silicon (Si) - 27.7%
- Aluminum (Al) - 8.1%
- Iron (Fe) - 5.0%
- Calcium (Ca) - 3.6%
- Sodium (Na) - 2.8%
- Potassium (K) - 2.6%
- Magnesium (Mg) - 2.1%
Other element’s in earth’s crust?
- 1.5% of Earth’s crust is made up of all other elements
- Most metals used in society (besides iron and aluminum) don’t appear on the list of the 8 most abundant elements.
What is the abundance of base metals in the earth’s crust?
Base metals (other than iron, aluminum, and titanium) in the continental crust:
- Copper: 0.0055%
- Nickel: 0.0075%
- Zinc: 0.0070%
- Lead: 0.00125%
- Tin: 0.00020%
What is the abundance of precious metals in the earth’s crust?
Precious metals in the continental crust:
- Silver: 0.000007%
- Gold: 0.0000004%
- Platinum: 0.0000005%
What does “Enrichment” of metals mean?
- Metals don’t occur in uniform abundance throughout the Earth’s crust.
- Certain geological circumstances cause metals to occur in higher concentrations (enrichment).
Why is understanding enrichment important for Geologists?
- Geologists study the processes and environments that lead to metal enrichment.
- This knowledge helps discover metal-rich deposits, which is essential for metal mining and use.
How does geology impact daily life?
Geologists help find valuable metal deposits, influencing the availability of materials used in technology, infrastructure, and more.
What is magmatic cooling in the context of metal enrichment?
- Some metals, like iron and chromium, can be concentrated by the cooling of magma.
- Heavy minerals like magnetite (Fe3O4) and chromite (FeCr2O4) form during cooling and sink to the bottom of the magma chamber.
How does gravitational settling contribute to metal enrichment?
- Heavy minerals (like magnetite and chromite) sink to the bottom of the magma chamber due to gravity during cooling.
- This results in layers with high concentrations of these metals.
What do the dark and light bands in magma cooling represent?
- Dark bands: Concentrated heavy minerals like magnetite, chromite, and platinum.
- Light bands: Silicates, which are lighter minerals.
What are the igneous processes that lead to metal enrichment?
- Magmatic Cooling
- Immiscibility
- Hydrothermal Processes
What is immiscibility in the context of metal enrichment?
- Immiscibility refers to the separation of metal-rich liquid from silicate-rich liquid.
- It occurs when a metal-rich liquid (like nickel) separates from a silicate liquid, similar to how oil separates from water.
What role did the Sudbury structure play in metal enrichment?
- The Sudbury structure is believed to be a meteorite impact crater, which was later compressed into an oval shape by tectonic forces.
- The impact event caused heat that melted rock far below the surface, allowing metal-rich liquid to separate from the silicate liquid.
How did the Sudbury Basin form?
- After the meteorite impact, molten material rose to the surface.
- Metal-rich liquid separated from silicate liquid and was concentrated in cracks around the impact crater.
- The crater basin was later filled with sediment.