- Видео 16
- Просмотров 11 795
Department of Geosciences, University of Oslo
Норвегия
Добавлен 7 ноя 2017
Velkommen til Institutt for geofag, UiO sin offisielle RUclips-kanal. Institutt for geofag ved Universitetet i Oslo dekker de fleste av disiplinene i geofag, og har bredest orientering innen forskning og studier i geofag i Norge. Fra tid til annen publiserer vi videoer her fra aktiviteter og forskning. Følg oss gjerne ...
Institutt for geofag, UiO på WWW, besøk URL: www.mn.uio.no/geo/
Welcome to the The Department of Geosciences, University of Oslo's official RUclips-channel. Our department covering the most of the disciplines in geosciences, and has the broadest orientation in research and studies in geosciences in Norway. From time to time we publish videos from activities and research. Please follow us ...
Department of Geosciences, University of Oslo, Norway on WWW, visit URL: www.mn.uio.no/geo/english/
Institutt for geofag, UiO på WWW, besøk URL: www.mn.uio.no/geo/
Welcome to the The Department of Geosciences, University of Oslo's official RUclips-channel. Our department covering the most of the disciplines in geosciences, and has the broadest orientation in research and studies in geosciences in Norway. From time to time we publish videos from activities and research. Please follow us ...
Department of Geosciences, University of Oslo, Norway on WWW, visit URL: www.mn.uio.no/geo/english/
Opening of the VISTA Centre VICCO, December 6 2024, Dept of Geosciences, University of Oslo
The official opening of the new VISTA Centre VICCO - VISTA Centre for CO2 Storage in Volcanic-Sedimentary Systems at University of Oslo (UiO) was December 6th 2024 at the Department of Geosciences, University of Oslo, Norway. The opening event was streamed online, and this is the recorded film of the opening event.
The research centre VICCO aims to explore the potential for large-scale permanent CO2 storage on the Norwegian Continental Self through carbonate mineral-forming reactions. Such carbonatization may enhance seal integrity and reduce reservoir leakage risks in mixed volcanic-sedimentary systems. The centre is led by Henrik Hovland Svensen, Professor of Geology at Department of Ge...
The research centre VICCO aims to explore the potential for large-scale permanent CO2 storage on the Norwegian Continental Self through carbonate mineral-forming reactions. Such carbonatization may enhance seal integrity and reduce reservoir leakage risks in mixed volcanic-sedimentary systems. The centre is led by Henrik Hovland Svensen, Professor of Geology at Department of Ge...
Просмотров: 354
Видео
Søk geofagstudier ved UiO - Geologi og geografi (bachelor)
Просмотров 492 месяца назад
Er du interessert i en karriere og arbeid innen realfag og geofag? Søker du geofag ved Universitetet i Oslo får du ved Institutt for geofag stor bredde i studiene, og undervisningen er spennende og variert med alt fra forelesninger og arbeid i grupper, til ekskursjoner og arbeid i felt. Naturen er ofte det fineste og mest spennende klasserommet for læring innenfor geofag. Institutt for geofag t...
Studer geofag ved UiO - Geofysikk og klima (bachelor)
Просмотров 672 месяца назад
Er du interessert i en karriere og arbeid innen realfag og geofag? Studiene ved Institutt for geofag ved Universitetet i Oslo har stor bredde, og undervisningen er spennende og variert med alt fra forelesninger og arbeid i gruppe, til ekskursjoner og arbeid i felt. Naturen er ofte det fineste og mest spennende klasserommet for læring innenfor geofag. Institutt for geofag tilbyr to bachelorprogr...
Velg studier i geofag ved Universitetet i Oslo
Просмотров 3392 года назад
Viss du velger å studere ved Institutt for geofag ved Universitetet i Oslo så får du stor bredde i fagene som undervises, og undervisningen er variert med alt fra forelesninger og arbeid i grupper, til ekskursjoner og feltarbeid. Naturen er ofte det fineste og mest spennende klasserommet for læring innenfor geofag, noe som denne kortfilmen viser. I studiene i geofag ved Universitetet i Oslo møt...
Hvorfor det er spennende å studere geofag!
Просмотров 4603 года назад
Guro er student på bachelorprogrammet Geologi og geografi ved Institutt for geofag, Universitetet i Oslo. I denne kortfilmen forteller hun om hvorfor det er spennende å være student i geofag. Nysgjerrighet er et stikkord. Kortfilmen ble første gang vist på Åpen dag 2021 ved Universitetet i Oslo. Filmen er laget av: Guro Lilledal Andersen / ©
Opplev studentmiljøet ved UNIS på Svalbard med UiO
Просмотров 1325 лет назад
Flere studenter ved Institutt for geofag velger å dra på studieutveksling et semester i løpet av studiene sine. Mange velger å dra til UNIS på Svalbard, som er en norsk øygruppe i Arktis. I tillegg til at du kan ta flere faglig interessante emner innen arktisk geologi, geofysikk og glasiologi mm, kan et opphold på Svalbard og Universitetssenteret gi deg nye venner og større nettverk, nye opplev...
Geologi og geografi, 3. årig bachelorstudium på UiO (kortfilm)
Просмотров 3886 лет назад
Bli inspirert! - Se denne kortfilmen om Geologi og geografi studiet ved Institutt for geofag, Universitetet i Oslo (UiO). Lær om jordens historie og oppbygning, naturressurser og energi, miljø- og klima, geografi og landskapsutvikling, naturfarer, geomatikk og mye mer - Studiene i geofag ved UiO er spennende, har stor bredde og gir mange karrieremuligheter. Les mer om det 3. årige bachelorstudi...
Geofysikk og klima, 3. årig bachelorstudium på UiO (kortfilm)
Просмотров 2236 лет назад
Bli inspirert! - Kortfilm om bachelorstudiet 'Geofysikk og klima' som tilbys av Institutt for geofag, Universitetet i Oslo. På dette studiet kan du lære om jordens historie og oppbygning, jordsystemet, geofysiske prosesser: i jordens indre, på landjorda, i havet, og i atmosfæren, hydrologi og oseanografi og mye mer - Studiene i geofag ved UiO er spennende, de har stor bredde og gir mange valgmu...
Geologi og geofysikk studier og utveksling til UNIS/Svalbard
Просмотров 6856 лет назад
Som GEO-student har du mulighet til å dra på utveksling til Universitetssenteret på Svalbard (UNIS), som ligger i Longyearbyen. Dette er verdens nordligste studiested, 78° nord. Her møter du et internasjonalt studiemiljø, og du samarbeider med forskere som er eksperter på arktiske fagområder innenfor biologi, geologi, geofysikk og teknologi. Dra på utveksling til Svalbard!
Sjekker mudderet i fjordbunnen utenfor Arendal
Просмотров 986 лет назад
Mikropaleontolog og professor i miljøgeologi Elisabeth Alve ved Institutt for geofag, Universitetet i Oslo var med forskningsskipet MS Trygve Braarud på et tokt for å sjekke om det var mangel på oksygen i fjordbunnen utenfor Arendal by. I mudderet fant hun intet tegn til liv utenfor sørlandsbyen. Kortfilm fra Apollon i forbindelse med Arendalsuka august 2018.
Excursion 8 August 2018, Diabasodden, Svalbard (GEO-DEEP9500)
Просмотров 3356 лет назад
The PhD course "Arctic tectonics, volcanism and climate" was held early August in the high north. The intensive week-long course held in Longyearbyen, Svalbard, brought together 15 students and 11 lecturers from 9 universities around the world. The course was funded through the DEEP Research School and the NOR-R-AM project, and UNIS. Film by Eivind Straume.
Excellent video and terrifying information.
Taken into context with the Ring of fire that's a great overall explanation of the reason for it's existence. Thx , brief and comprehensive 👍
I have been waiting for this info for 50 m years. Finally everything is clear now, we can move on.
I'll go one better. The hot spot track is far longer and more complicated than you think because the earths crust has been doing some serious moving around. The hot spot track goes far under Kamchatka almost to the mid Atlantic rift fault in Siberia because it fractured near Kiska and then was subducted. Before the fracture it followed the bowers ridge and then comes ashore at 60 n 170 e and goes north to near Wrangel island and follows the alpha ridge to Elsmere island and Greenland. Probable age 156 million years or more. It is probable that north America rotated clock wise and then got pushed south westwards. If true it puts a whole new spin on geologic history. I am using the 8 cm per year plate movement speed stated by Dr. Mike Poland and google earth to plot the hot spot track.
Why does something bend? Because due to an obstacle. A river around a mountain. A tree growing towards light. A vine around a pole. A road bypassing a tree, house...
Nice🇳🇴🇳🇴🇳🇴🇳🇴💙🐠
Happy New Year 🎉🎉🎉🎉🎉
Been looking for this info for years. Thanks
LOL. A total comedy of errors. Thanks for the entertainment. "Subduction" lol! Go back to grade school and learn that rocks, especially deep ocean floor basalt, don't bend.
There’s much more to the “Big Bend” than the island chain; look at Google Earth renderings of the region; due West of the Emperor Chain is a very deep trench, which appears to be a [former?] subduction zone, parallel to and nearly as long as the chain. What are the origin tests of the Emperor Chain? Is it identical to the Hawaiian Chain or a volcanic arc? If it’s an arc, there is no bend and would show the HHS was birthed by a spreading ridge, like the other oceanic hot spots, including Yellowstone.
the earth crust unlock from mantal every 12000 year at same time sun corna stutdown
Wasn't it about the same time that the Indian Plate collided with Asia?
Huh??
I have post graduated in MS Resevior geology, and I want to pursue PhD , can you please share me the link from where I can apply for fully funded PhD scholarship?
The supposed collision requires more detail. The Emperor Seamounts disappear into the Aleutian Trench, where the Pacific Plate subducts. When it changed direction it headed more toward Asia, so blaming an Asian collision for the change in direction seems unlikely. More detail on this, please.
wtf my teacher told us to watch this for homework but i have already watched this video before and liked it- bruh i have no memory of this
Okay wait, what?? It wasn't due to the collision of the Indian subcontinent with Asia???
19.5 Jupiter, Neptune (north and south) Mars. You think that pattern would tell you it's more plate movement then a drifting hot spot. And why can't you date it from the speed of the motion of the plate vs. some sketchy radioactive dating methods? What, is there some kind of discrepancy you're trying to hide from us?
I don't think hotspots "move" they are "mantle plumes" and the mantle of the earth is a thick lump around the whole planet. I half think that ocean spreading is a mild linear plume near the surface, but the heat difference across the ocean bottom from 1 side of the ocean to another is not major, so if a shock to the ocean floor occurs due to some collision then the difergence can shift direction. Unlike continental crust the ocean crust is so similar in all spots there is no great density difference in any direction, so divergence and direction can randomly shift so long as the same amount of heat energy keeps being released to the surface. I could be very wrong,....
Just an addition. I don't know if hot spots move on earth, but on Neptune, it had a giant storm at 19.5 degrees in its southern hemisphere. At some point it disappeared. Later observations showed the giant storm reappeared on Neptune, however it was at 19.5 degrees in the northern hemisphere. Magnetic poles also drift gradually for some time. The storm on Neptune disappeared completely, and no observed drift occurred, it just suddenly reappeared in the northern hemisphere. This guy seems to avoid the controversy of why this plate change motion didn't affect other island changes in the south pacific by saying that basically there was a subduction zone just south of the more east west undersea Hawaiian mounts. Maybe he's saying that the pacific plate was broken there, and that allowed the plates to move separately from the south pacific, until that northern pacific plate slammed conveniently into the Eurasian plate thanks to a, who's knows how Kamchatka formed, slammed into the Eurasian plate causing the supposed, North Pacific plate, to look for an easier direction of motion by moving east west to form the east west motion of the Hawaiian chain, then finally the North Pacific plate mysterious suduction zone (plate division) recombined forming a continuous Pacific Plate. Well hot damn, how do you like those dominoes.