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Episoder
- S1 E1 - Geology's Impact on History20. desember 202331minIf you could view Earth's history at high speed, you'd see continents whiz about, ocean basins grow and shrink, and mountain ranges rise and erode away. This lecture sets the stage for investigating our dynamic planet.Gratis prøveversjon av The Great Courses Signature Collection eller kjøp
- S1 E2 - Geologic History—Dating the Earth20. desember 202332minDiscovering Earth's exact age took centuries of detective work. Rock strata provide relative ages, but only with the discovery of radioactivity was it possible to determine the absolute geologic timescale.Gratis prøveversjon av The Great Courses Signature Collection eller kjøp
- S1 E3 - Earth's Structure-Journey to Earth's Center20. desember 202332minAnalysis of seismic waves from earthquakes allows scientists to map the structure inside Earth. Using this technique, we take a modern-day journey to the center of the Earth in the style of Jules Verne.Gratis prøveversjon av The Great Courses Signature Collection eller kjøp
- S1 E4 - Earth's Heat-Conduction and Convection20. desember 202331minWe reverse the direction of the previous lecture to see how heat flows from the center of Earth toward the surface, exploring the phenomena of heat radiation, conduction, and convection.Gratis prøveversjon av The Great Courses Signature Collection eller kjøp
- S1 E5 - The Basics of Plate Tectonics20. desember 202332minThe theory of plate tectonics accounts for the existence of continents, oceans, mountains, earthquakes, volcanoes, mineral resource distribution, climate changes, and many other aspects of our planet.Gratis prøveversjon av The Great Courses Signature Collection eller kjøp
- S1 E6 - Making Matter-The Big Bang and Big Bangs20. desember 202330minWe investigate the big bang and the early evolution of the universe to learn the origin of atoms, stars, and planets. The supernovae of dying stars played a key role in forging heavy elements.Gratis prøveversjon av The Great Courses Signature Collection eller kjøp
- S1 E7 - Creating Earth-Recipe for a Planet20. desember 202332minThe solar system formed 4.6 billion years ago when a cloud of gas, dust, and ice began to collapse and rotate, with Earth accreting in the inner region of the disk. An enormous collision with the proto-Earth produced the Moon.Gratis prøveversjon av The Great Courses Signature Collection eller kjøp
- S1 E8 - The Rock Cycle—Matter in Motion20. desember 202332minThough rocks may seem eternal, they are part of a continuous cycle of changing forms called the rock cycle, which begins with igneous rocks and can involve sedimentary and metamorphic phases.Gratis prøveversjon av The Great Courses Signature Collection eller kjøp
- S1 E9 - Minerals—The Building Blocks of Rocks20. desember 202331minRocks are made of minerals, which in turn are composed of different elements. Silicon and oxygen are the two most abundant elements in Earth's mantle and crust, and most rocks contain them.Gratis prøveversjon av The Great Courses Signature Collection eller kjøp
- S1 E10 - Magma—The Building Mush of Rocks20. desember 202332minMost magma is generated beneath mid-ocean ridges, where plates move apart and rock moves toward the surface to fill the gaps. Magma forms in these places due to a process called pressure release.Gratis prøveversjon av The Great Courses Signature Collection eller kjøp
- S1 E11 - Crystallization—The Rock Cycle Starts20. desember 202331minWhen magma cools below certain temperatures, solid mineral crystals begin to grow. With continued cooling the entire magma will eventually crystallize, and the result is an igneous rock.Gratis prøveversjon av The Great Courses Signature Collection eller kjøp
- S1 E12 - Volcanoes—Lava and Ash20. desember 202332minVolcanoes form where magma reaches the surface and erupts—at which point the magma becomes lava. The different kinds of volcanoes are related to the tectonic settings in which they occur.Gratis prøveversjon av The Great Courses Signature Collection eller kjøp
- S1 E13 - Folding—Bending Blocks, Flowing Rocks20. desember 202332minMost rock of the crust and mantle is solid. And yet, over long timescales, the crust and mantle are in motion, bending and flowing. This lecture shows how rocks deform in an elastic, plastic, or brittle manner.Gratis prøveversjon av The Great Courses Signature Collection eller kjøp
- S1 E14 - Earthquakes—Examining Earth's Faults20. desember 202331minMore than 200,000 earthquakes are recorded each year. We examine the types of faults along which they occur and the aftermath, which in some cases can leave the Earth ringing like a gong for months.Gratis prøveversjon av The Great Courses Signature Collection eller kjøp
- S1 E15 - Plate Tectonics—Why Continents Move20. desember 202331minContinents move because they are the surface expression of mantle convection. Two main forces are directly responsible for plate motions: slab pull and ridge push.Gratis prøveversjon av The Great Courses Signature Collection eller kjøp
- S1 E16 - The Ocean Seafloor—Unseen Lands20. desember 202331minThe seafloor shows a tremendous diversity of features that are related to plate tectonics and the process of mantle convection.Gratis prøveversjon av The Great Courses Signature Collection eller kjøp
- S1 E17 - Rifts and Ridges—The Creation of Plates20. desember 202332minOceans undergo reincarnation: they repeatedly die and are reborn. The Atlantic Ocean is only 180 million years old and will eventually close up again. The Red Sea appears to be a new ocean in the making.Gratis prøveversjon av The Great Courses Signature Collection eller kjøp
- S1 E18 - Transform Faults—Tears of a Crust20. desember 202330minThe San Andreas is a transform fault that separates the North American and Pacific plates. Transform faults are actually rare on land, but mid-ocean ridges are intersected by countless such features.Gratis prøveversjon av The Great Courses Signature Collection eller kjøp
- S1 E19 - Subduction Zones—Recycling Oceans20. desember 202331minSubduction zones are the most geologically exciting places on Earth. Here the most destructive earthquakes and volcanoes occur, and forces are generated that may rip supercontinents apart.Gratis prøveversjon av The Great Courses Signature Collection eller kjøp
- S1 E20 - Continents Collide and Mountains Are Made20. desember 202332minWhen plate motions bring continents in contact with each other, the result is the formation of mountains. A notable example is the Himalayas, produced by the continental collision of India with China.Gratis prøveversjon av The Great Courses Signature Collection eller kjøp
- S1 E21 - Intraplate Volcanoes—Finding the Hot Spots20. desember 202331minFor years intraplate volcanoes such as those that produced the Hawaiian Islands were lumped together under the catch-all name of "hot spots," but recent work is showing that Earth has many different ways of making a volcano.Gratis prøveversjon av The Great Courses Signature Collection eller kjøp
- S1 E22 - Destruction from Volcanoes and Earthquakes20. desember 202331minThe largest earthquakes and volcanic eruptions release as much energy as the simultaneous explosion of tens of thousands of nuclear weapons. We look at the human consequences of these events.Gratis prøveversjon av The Great Courses Signature Collection eller kjøp
- S1 E23 - Predicting Natural Disasters20. desember 202331minVolcanoes can be easily monitored, and they reveal many clues to an impending eruption as the magma slowly forces its way toward the surface. Earthquakes, by contrast, are not yet predictable.Gratis prøveversjon av The Great Courses Signature Collection eller kjøp
- S1 E24 - Anatomy of a Volcano—Mount St. Helens20. desember 202331minWe examine the eruption of Mount St. Helens on May 18, 1980, triggered when an earthquake caused a gigantic avalanche that released pent-up magma and gases, leveling trees for over 600 square kilometers.Gratis prøveversjon av The Great Courses Signature Collection eller kjøp
- S1 E25 - Anatomy of an Earthquake—Sumatra20. desember 202330minThe 2004 Sumatra earthquake produced a massive tsunami that killed more than 200,000 people around the Indian Ocean. We look at the complex tectonic forces behind this cataclysm.Gratis prøveversjon av The Great Courses Signature Collection eller kjøp
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