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This Is My World. Earth Sciences and the Exploration of Our Planet: A Journey Through Time, from Its Origins to the Future

 
Time
18:00 - 24:00 o'clock
Organizer
Friedrich-Schiller-Universität Jena and Institut für Geowissenschaften
Place
Campus
Adresse
Carl-Zeiss-Straße 3

What holds the world together at its very core? To use ores, water, and energy resources sustainably over the long term, we need to understand exactly that. What is the Earth made of, and how was it formed? What processes take place within and on its surface? How do we know this?

This is all about the world—and even beyond, to other planets and meteorites. You can:

· Experience the fascination of the solar system’s primordial matter as we examine meteorites under a microscope together. Meteorites originate from the solar system’s primordial bodies—the asteroids—and are the oldest rocks. They provide unique insights into the formation and early development of the solar system and Earth. They also reveal long-past processes, such as the condensation and agglomeration of the first solid matter in what is known as the solar nebula. The oldest meteorites—the carbonaceous chondrites—contain not only silicates but also organic matter, which may have arrived on Earth through impacts as potential building blocks of life. These are also the targets of current space missions in which the University of Jena is participating.

· Take a look at the Mineralogical Collection: Discover fluorescence in mineralogy. In 1801, Johann W. Ritter discovered ultraviolet (UV) light in Jena. The term “fluorescence” was not introduced until about 50 years later by G. Stokes, although the natural fluorescence of fluorspar (fluorite) in sunlight had been known for some time. We’ll demonstrate and explain fluorescence using various minerals. UV light has many applications in modern earth sciences—from gemstone appraisal to the prospecting of industrial minerals, the range is vast. Let us surprise you, and if you have a piece of ruby jewelry, feel free to bring it along—we’ll take a look at it together…under UV light, of course! 

· Learn how we use geophysics to explore the Earth’s interior —without digging at all: Using methods such as geoelectrics, magnetics, and gravimetry, we can peer into the subsurface without breaking ground. To do this, we utilize electrical currents, the Earth’s magnetic field, and its gravitational field. These provide information, for example, about the stratigraphic relationships of rock layers. But they can also be used to detect groundwater, geological structures such as faults, salt domes, ore deposits, and other hidden objects—like archaeological finds—or underground cavities. There’s a lot to discover right beneath our feet. We’ll show you how it’s done. 

· Experience a “bouncy castle” with a twist: Instead of earthquakes, seismic measurements detect and visualize our guests’ jumps. We explain how these measurements work and how we operate within the Thuringian Seismological Network to monitor seismic activity in Thuringia and the surrounding area.

· Understanding plants as the link between the underground and above-ground worlds: Plants and photosynthesis have played a fundamental role in making our planet largely habitable—the ozone layer, a pleasant climate, and air to breathe. They are a geological force. Plants fluoresce, and through small experiments, we make the vital process of photosynthesis visible. We demonstrate its connection to carbon sequestration and the greenhouse effect, as well as how water scarcity affects it.

 
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Links: Kosmonautin Christina Koch schaut während Artemis II zurück zur Erde, Mitte oben: Calcit aus China im UV-Licht, unten: Chondrit im Lichtmikroskop zwischen gekreuzten Polarisatoren, Rechts: Geolektrische Messung im Feld.
Links: Kosmonautin Christina Koch schaut während Artemis II zurück zur Erde, Mitte oben: Calcit aus China im UV-Licht, unten: Chondrit im Lichtmikroskop zwischen gekreuzten Polarisatoren, Rechts: Geolektrische Messung im Feld.
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