Midterm Flashcards
(150 cards)
What does the world geology mean? Why is it important?
Geo = earth
Ology = the study of
Therefore geology is the study of the earth.
It is important for energy and natural resources, solving environmental problems, building cities and highways, and predicting and preventing natural disasters.
What is the fundamental principle of the concept of uniformitarianism, and what does it mean? What is the timescale of the earth measured in?
The present is the key to the past. This means that the processes that we see shaping th earth today are the same as the processes that shaped the earth millions of years ago. Geological time is meausred in billions of years.
When when did the Big Bang occur?
~14 billion years ago
What theory is generally excepted as correctly explaining the formation of the solar system? Describe it.
The Nebular theory - 5 billion years ago. A nebular made up of hot gasses - mainly hydrogen and helium. The nebular cloud contracted under gravity and began rotating. The rotating instigating central pedal force, which caused elements to concentrate in the centre. Gravitational energy converted to thermal energy. This became the sun. The other, heavier elements began to fuse together into planets and moons, which continued to rotate around the sun.
Explain how the earth was formed, and what layers formed.
Formed by rock collisions. The heavier elements (Fe, Mg) migrated inwards and became the core. The lighter elements (oxygen rich elements) migrated outwards and formed a very thin crust. The middle area between the crust and the core is called the mantle. In the process, gasses escaped and formed the atmosphere.
Describe the names and the layers of the world.
- Lithosphere (“sphere of rock”)
- the crust AND the upper most mantle - split into plates that move over top of the asthenosphere - Asthenosphere (“weak sphere”)
- liquid - due to unequal heat distribution in the earth convection currents occur here, the lithosphere rides on top of them, in CONTINENTAL DRIFT - Core
- very dense and under extreme heat, intense pressure keeps the core a solid - Ni, Fe
What causes more geological activity, convergent or divergent boundaries?
Convergent boundaries
What is a divergent boundary?
Occurs when plates move apart due to tensional stress. This allows for upwellling of material in the mantle, forming ridges and rifts. It is the cause of SEA-FLOOR SPREADING.
What is a convergent boundary?
The primary cause of geological activity. Occurs when denser, oceanic plate descends below lighter, continental plate. This is known as SUBDUCTION, and it forms a trench. The denser, oceanic plate reaches far enough into the asthenosphere that it begins to melt. Sometimes, this allows for melted magma to protrude and form a volcano, which eventually erodes into sediment. It is at convergent boundaries that earthquakes and volcanoes often form.
What is subduction?
The descent of the denser oceanic lithosphere beneath the lighter, continental lithosphere.
What does Pangaea mean? What evidence is there to support it?
Pan = all, Gaea = earth
- Fit of the continents
- South America and Africa fit together at a depth of 900 meters (at the continental shelf) - Fossil evidence
- Fossils match across continents (ex. Mesosaurus fossils found in East S.A. and South Africa) - Rocks and Structures
- ex. Appalachian mountains and Scandinavian mountains form a continuous chain - Paleoclimatic Similarities
- ex. finding coal in ancient tropical swamps in places that are now glaciated; finding striations from glaciers in tropical areas today
What are the 4 spheres of the earth? How do they interact?
Earth is a dynamic system of interacting spheres.
- Geosphere - the earth and rock sphere
- Hydrosphere - the sphere of water
- Biosphere - the sphere of life, ranging from the hydrosphere, slightly into the atmosphere
4, Atomsphere - thin and tenuous sphere of gases, producing weather and climate
Where are new rock types mainly produced at?
Converging boundaries
Explain the rock cycle, beginning at magma.
Magma crystallizes to form igneous rock, igneous rock is weathered, transported, and deposited to form sediment, which is cemented to form sedimentary rock, sedimentary rock undergoes metamorphisis to form metamorphic rock. Metamorphic rock melts to form magma. Metamorphic rock can become sediment by weathering, as can sedimentary rock. Igneous rock can also undergo metamorphisis under heat and pressure to form metamorphic rock.
What are minerals? How many are there? How many are common in the earth’s crust? How are they produced?
Minerals are inorganic substances formed by nature that combine together to form rocks. Their elemental composition, chemical structure, and bonding determine the properties that the mineral will have. There are 4700 known minerals, but only about 20 are predominant in the earth’s crust.
What type of mineral is the most abundant?
Silicates
What are silicates? What is their structure, and elemental composition?
Silicates are composed of Silicon and Oxygen, covalently bonded to each other to form tetrahedrons (SiO4)4-. Because oxygen is an anion, and therefore negatively charged, metal cations such as Fe2+ and Mg2+ can ionically bond. This ionic bonding is weaker than the overall covalent bonding, which usually results in a spot of weakness along the mineral, which becomes the cleavage point.
What is the composition of a dark silicate?
Ferromagnesian - therefore with Fe and Mg within the silicate tetrahedra.
What are the four ferromagnesian silicates? Describe their bonding, and cleavage?
- Olivine
- single tetrahedra, covalently bonded, with Fe2+ and Mg2+, no cleavage - Pyroxene
- single chains of tetrahedra, with metals between them, cleavage is 2 at 90 degrees - Amphibole
- double chains of tetrahedra, with metals between them, cleavage is 2 not at 90 degrees (60 and 120) - Biotite (black mica)
- sheets of tetrahedra with metals between them, cleavage is basal/platy
What are the four non-magnesian silicates? Describe them.
- Muscovite (white mica)
- perfect basal cleavage, often used for muscovy window glass - Feldspar
- strongly bonded 3D network of silica tetrahedra
a. Orthoclase (K feldspar) with potassium, cleavage is 2 at 90 degrees.
b. Plagioclase (Ca/Na feldspar) with calcium in mafic rocks and sodium in felsic rocks, cleavage is 2 at 90 degrees. - Quartz
- very strong, purely covalent silica tetrahedra, has a hardness of 7, can form crystals with sufficient space in nature. (SiO2)
Name the two types of non-silicate minerals, and describe them.
- Carbonates (CO3)2-
a. Calcite (CaCO3) - used in cement and limestone
b. Dolomite (MgCaCO3) - Evaporites
a. Halite (NaCl) - table salt
b. Gypsum - plaster and drywall
Name the metallic, non-silicate type of mineral.
Ores of metals
- Hematite/Magnetite (Fe)
- Sphalerite (Zn)
- Pyrite/Chalcopyrite (Cu)
- Galena (Pb)
Where are igneous rocks? Where does the name come from? Which types of minerals are in igneous rocks?
Igneous = fire
Igneous rock crystallizes from molten SILICATE magma, which is formed deep in the earth under high temperatures and pressures.
What are the two options for magma at the site of a volcano? What type of rock does each location of formation form? Typically what are the textures of this rock?
- Intrusive - forms plutonic rock - texture tends to be PHANERITIC
- Extrusive - forms volcanic rock - texture tends to be either PYROCLASTIC, APHANITIC, OR GLASSY, due to quick cooling, or quenching by air or water.