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- Hot rocks, big rivers and the world’s tallest mountain face
- Lovely Ladakhi landslides
- Building models about building mountains
- Geological pilgrimage – Assynt, Scotland
- Where on Google Earth #343 – updated
- Sources of open access scientific papers
- Crème brûlée or jelly sandwich?
- Accretionary Wedge #44 – “most important teacher”
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- On Hot rocks, big rivers and the world’s tallest mountain face :
- Bryan O'Sullivan: This essay was simply excellent, describing an exciting corner of geoscience research that I... (5 hours 33 minutes ago)
- Brian Romans: Awesome. I love this stuff. I find the coupling and feedbacks of the crust and its surface... (13 hours 8 minutes ago)
- Felix Bossert: WoGE#344 is ready to dive in at http://woge-felix.blogspot.de/ 2012/05/where-on-google-ear... (9 days 13 hours ago)
- Metageologist: Spot on as always Felix. I’ve nothing more to add to your description. I picked it as a... (9 days 15 hours ago)
- Felix Bossert: 31.6194°, 79.7060° Zanda Basin, Tibet, a late Cenozoic graben between the Himalayan mountain... (9 days 16 hours ago)
- Bill: The European Geophysical Union has a series of peer-reviewed open-access journals.... (10 days 3 hours ago)
- cush copeland: In the early ’70s, the University of Illinois (Urbana) ran a summer geology field course... (13 days 18 hours ago)
- Suvrat: terrific post! just a terminological observation: Talking about the Himalayas once more, there is a... (14 days 4 hours ago)
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Author Archives: Metageologist
Hot rocks, big rivers and the world’s tallest mountain face
In areas of active mountain-building the middle crust can get hot and weak, like a soft jam/jelly filling in a sandwich. These squishy rocks are hidden from us by the cold rigid upper crust, so we wouldn’t expect to see … Continue reading
Categories: mountains, open access, tectonics
Lovely Ladakhi landslides
Time for a post with an emphasis on photos. There’s more context here, but let’s get on with admiring the view. That’s me, standing in front of chorten (Tibetan Buddhist religious structure). The rather pretty cliffs are Tethyan sediments, now … Continue reading
Categories: mountains
Building models about building mountains
How do mountains form? It’s just thrusts, right? Compression causes thrust faulting which piles up layers and layers of rock. This causes Barrovian metamorphism and makes mountains. Simple, no? No. Thrusting is important, of course, but as always real rocks are … Continue reading
Geological pilgrimage – Assynt, Scotland
In Accretionary Wege #45 Denise Tang asked for “Geological Pilgrimage – the sacred geological place that you must visit at least once in your lifetime “. For me, and dare I say it for any British educated hard-rock geologist the … Continue reading
Categories: Accretionary Wedge
