Tectonics, Earthquakes & Volcanoes Flashcards
1816, year without summer
average global temperatures decreased by 0.4 - 0.7 °C
resulted in major food shortages across the Northern Hemisphere
caused by the massive 1815 Mount Tambora (Dutch East Indies) eruption (world’s largest eruption since Hatepe eruption in 180 AD)
the eruption cloud spread across the entire globe and allowed less sun through leading to the huge drop in temperatures
high levels of tephra in the atmosphere led to unusually spectacular sunsets (evident in several painters’ (such as J. M. W. Turner) work at that time)
Crop failures led to massive famine
Acid/dome volcano
Lava quickly solidifies on exposure to the air. A steep-sided convex cone is produced, as in most cases lava solidifies quickly near the crater. In one extreme case, the lava solidified on Mt. Pelee in Martinique to form a spine.
(for a volcano) active, dormant, extinct
An active volcano is a volcano that is showing signs seismic or thermal activity such as smoke or an eruption. (Mt. Stromboli)
A dormant volcano is an active volcano that is not erupting, but supposed to erupt again. (Mt. Kilimanjaro))
An extinct volcano is a volcano which is not expected to erupt again. (Mt. Kenya)
Aleutian islands
A chain of more than 150 mostly volcanic islands forming an island arc that separates the Bering Sea in the north from the main portion of the Pacific Ocean. Lies on the destructive Pacific and North American plate boundary.
Alfred Wegener (1880-1930)
Alfred Wegener was a geophysicist and meteorologist who proposed the theory of continental drift – the idea that Earth’s continents move. Despite publishing a large body of compelling fossil and rock evidence for his theory between 1912 and 1929, it was rejected by most other scientists. It was only in the 1960s that continental drift finally became part of mainstream science.
ash
Fragments of pulverized rock, minerals and volcanic glass, created during volcanic eruptions. Once in the air, ash is transported by wind up to thousands of kilometers away. Can form into an ash cloud which can block some of the sun’s rays leading to a temperature drop
Benioff zone
comes after the subduction zone, where the crust is going down into the mantle.
Caldera (acid lava)
Large bowl-shaped crater that forms by the collapse of a volcanic cone after an eruption. The gases which build up become so extreme that a huge explosion removes much of the former summit. Sometimes the eruptions are so violent on islands that the crater becomes flooded by the sea. (e.g. Santorini & Krakatoa)
Cinder cone volcano (acid lava)
Built of ejected lava fragments. Usually small ( < 1000 ft high), have steep slopes and often form near bigger volcanoes. (e.g. Paricutin (Mexico))
Coal in Greenland
On an expedition in Greenland, Wegener discovered coal. This was a curious discovery as coal is only found in places where there has been a jungle (coal is made out of residue of trees and plants from millions of years ago through combined effects of pressure and heat; it is mainly composed of carbon, oxygen and hydrogen) and since jungles are found around and close to the Equator, (and Greenland is very far from the Equator) is was very strange to find coal in Greenland). So, Greenland must have been close the equator at some point - this was evidence for Wegener’s idea of Pangea.
Collision margin
Continental crust colliding with continental crust, the land is folded creating huge fold mountains. earthquakes are common at this boundary but there are no volcanoes as subduction is limited and there is usually too much material for extrusive features to form. (e.g. Himalayas & European Alps)
Composite cone volcano
This is the classic shape of a volcano and is the result of alternating eruptions of lava (usually acid) and ash. (e.g. Mt. Etna, Mt. St. Helens, Mt. Fujiyama, Mt. Stromboli)
Conservative/ Passive margin
2 plate slide side by side (opposite directions or in the same direction at different speeds). Crust is neither created nor destroyed. Faults and earthquakes are found at these boundaries. (e.g. San Andreas fault ( Pacific & North American plate)
Constructive plate margin
Magma rises within the mantle due to convection currents. The heat weakens and cracks the crust. Magma forces its way through the crack and solidifies. A combination of the new crust and the convection currents slowly ‘pushes’ the two plates apart. New crust is constructed (hence the name ‘constructive plate boundaries) (e.g. Mid Atlantic Ridge, East Pacific Rise)
Continental drift
Set forth in 1912 by Alfred Wegener, continental drift was a theory that explained how continents shift position on Earth’s surface. It also explained why look-alike animal and plant fossils, and similar rock formations, are found on different continents.
Convection currents
Convection currents in the magma drive plate tectonics. Large convection currents in the mantle transfer heat to the surface, where plumes of less dense magma break apart the plates at the constructive margins, creating divergent plate boundaries. As the plates move away from the constructive margins, they cool, and the higher density basalt rocks that make up ocean crust get consumed at the ocean trenches/subduction zones. The crust is recycled back into the mantle.
Crater lake
A crater lake is a depression created by a volcanic crater or caldera that is filled with water. When a volcano is no longer active, the crater or caldera may fill with water from rainfall and melting snow that may also feed the lake. A caldera is created by the collapse of a volcanic crater and the land around it. (e.g. Crater Lake, Oregon - formed by the now-collapsed volcano, Mount Mazama)
Crust
The outermost solid shell of a planet
Deep ocean trench
Any long, narrow, steep-sided depression in the ocean bottom. Typically form in locations where one tectonic plate subducts under another. Deepest: Mariana Trench (Pacific plate under Philippine plate)
Destructive plate margin
Two plates (oceanic and continental or oceanic and oceanic) collide. One (the weaker one) falls beneath the other plate (this is the subduction zone), creating a deep trench, whilst the other will form fold mountains from stone folding and buckling as the plates collided. When the weaker plate meets the upper mantle, it will melt and mix with the magma. Since it is now a mixture of substances from both the crust and mantle, it is lighter and will rise in the form of plutons under the fold mountains, creating volcanoes. This is why it is extremely common to find volcanoes along a destructive boundary. However, most of the rising magma will actually never make it to the surface, sometimes forming batholiths (e.g. Sugar Loaf in Rio de Janeiro). As the weaker plate moves down, it also pulls down the edge of the other plate causing earthquakes since rock does not move along rock smoothly. This will also lead to an increase in tension until it is released when the stronger plate flicks back up usually causing a tsunami.
Disease
Disease can spread very easily after an earthquake due to a lack of clean water and medical facilities
Drop, cover, hold
If one is indoors during an earthquakes, these are appropriate actions to reduce risk of injury and death.
epicentre
The point on the Earth’s surface that is directly above the earthquake focus (the point where an earthquake or underground explosion originates).
fissure volcano
Liquid flows (usually) from elongated fractures or cracks on the slope of a volcano. Common where plates move apart (constructive boundary). The basalt (solidifies lava) may form large plateaus (new crust). Basic lava. Common in Iceland (e.g. Eyjafjallajökull) and the Giants Causeway in Ireland.
Focus
The point inside the crust where pressure is released causing an earthquake.
fold mountains
a range of high mountains formed by two plates moving together at a collision or destructive margin
hot spot
An area in the Earth’s mantle where a column of magma rises and melts through the crust leading to volcanic activity. As new magma continues to rise and solidify, islands can be made. It is common to find a chain of islands (e.g. Hawaii) with the biggest ones closer to the hotspot and the smaller ones further from it. This is due to the movement of the plate; so if the hotspot forms an island and the plate moves, it will start forming a new one next to the old one. The older islands get eroded by the ocean, making them smaller.
island arc
a curving line of islands formed by volcanic activity at a destructive plate boundary (e.g. Aleutian islands)
lava
molten rock (magma) ejected onto the Earth’s surface by volcanic activity. Two types: basaltic/basic - fluid, pure magma, not mixed with anything else (e.g. Hawaii); and andesitic/acid - viscous, comes from subduction zone (e.g. Andes)
mantle
the part of the Earth’s structure between the crust and the core