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Sumiko Tsukamoto

@sumikotsuka.bsky.social
36 followers 27 following 4 posts
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Reposted by Sumiko Tsukamoto
Luca Malatesta @geoluca.bsky.social · 14/11/2025
On Noto Peninsula where coseismic uplift was ~2m. Sequence pre-earthquake, EQ +3 months, EQ +23 months. I thought we would be able to monitor this nice flat surface for weathering efficiency over the years…
Noto coast in Nov. 2023. 
Waves come all the way up to a concrete embankment protecting a cliffNoto Coast after 2 m coseismic uplift.
100 m wide rock platform is now emergedA road is now built on the bedrock platform, protected by a new sea wall
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Reposted by Sumiko Tsukamoto
Norbert Marwan @pucicu.de · 06/12/2024
Too old, too dirty, to unradiogenic? Can’t use your #speleothem? Don’t despair! ITL dating is here to help you out! www.sciencedirect.com/science/arti... @speleoseb.bsky.social @sumikotsuka.bsky.social
sciencedirect.com
Isothermal thermoluminescence dating of speleothem growth – A case study from Bleßberg cave 2, Germany
Speleothems are a key archive of past climatic and environmental changes. 230Th/U dating is the most commonly used method to determine speleothem ages…
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Reposted by Sumiko Tsukamoto
Luca Malatesta @geoluca.bsky.social · 05/12/2024
Our work on surface deformation by the Noto Earthquake is finally out! Fukushima Yo led a team to create and ground-truth a full 3D deformation field from InSAR on the entire Peninsula. We show that repetition of similar quakes explains the 1st-order landscape features. 1/5 doi.org/10.1126/scia...
doi.org
Landscape changes caused by the 2024 Noto Peninsula earthquake in Japan
Deformation due to the Noto Peninsula earthquake showed that its repetition shaped the Peninsula’s modern landscapes.
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Reposted by Sumiko Tsukamoto
Luca Malatesta @geoluca.bsky.social · 14/11/2024
A recurring question for us: Where do beach cobbles come from? Here a cool answer on a ~340ka terrace that shows strath & sed cover: (Salt?) weathering of volcaniclastics frees clasts when it was a coastal (intertidal?) platform. Strongest survive & make up sediment. Or so we think.
A pine tree on a cliff overlooking the coast that extends in the distance. Some km away, a terrace is highlighted by yellow pencilA vegetated road cut in a flat surface (supposed MIS9 terrace). On the road cut yellow dots highlight the terrace surface. A red dashed line follows the estimated position of the bedrock strath. A pink rectangle outlines a scraped of segment of the road cut surfacePicture of the scraped off surface from the previous image. The upper part is made of soil and scattered cobbles. The lower part is made of pebbles and cobbles in a cemented matrix. Clasts have varying lithologies. They are generally poorly sorted but layers of finer grained material exist.Same image as previous with pencil annotations highlighting lithologies of clays existing both in bedrock and sediment cover as well as clasts of weak tuff only existing in the bedrock
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Reposted by Sumiko Tsukamoto
Luca Malatesta @geoluca.bsky.social · 01/11/2024
Some context for the 🇯🇵 pictures I am posting. @sumikotsuka.bsky.social & I are working on Sado Island and Noto Peninsula since '23 for the DFG project TEMARI. Both sites face 🌊 on 1 side, are tectonically active (Noto EQ), & have many many marine terraces *What controls the creation of terraces?
Map of Noto Peninsula and Sado Island, arrows show direction of waves, pink lines represent distribution of terraces, red lines mark main (active) faults. The figure shows that Noto and Sado face the same wave condition but Noto has terraces on its shielded side, while they are on the wave-exposed side of Sado.Oblique view from Google Earth of marine terraces covered by rice paddies along the NW coast of Sado Island.
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Reposted by Sumiko Tsukamoto
Norbert Marwan @pucicu.de · 01/10/2024
We have shown that thermoluminescence dating can provide reliable age estimates for particularly old speleothems: (open access) www.sciencedirect.com/science/arti... short summary at bbh.pik-potsdam.de/en/thermolum...
sciencedirect.com
Isothermal thermoluminescence dating of speleothem growth – A case study from Bleßberg cave 2, Germany
Speleothems are a key archive of past climatic and environmental changes. 230Th/U dating is the most commonly used method to determine speleothem ages…
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Reposted by Sumiko Tsukamoto
Seb Breitenbach @speleoseb.bsky.social · 29/09/2024
If you have dirty and seemingly ’undatable‘ speleothem samples in your lab - look no further! Isothermal Thermoluminescence (ITL) dating can help you ! Look at our latest study led by Junjie Zhang & Sumiko Tsukamoto of #LIAG and #TuebingenUni : eur02.safelinks.protection.outlook.com?url=https%3A...
eur02.safelinks.protection.outlook.com
Redirecting
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Reposted by Sumiko Tsukamoto
Luca Malatesta @geoluca.bsky.social · 04/03/2024
We were able to reach the same spot on the north coast of Noto Peninsula where I took pictures last November. That was before the earthquake and the ~1.7m of uplift it caused at this location. Before/after below
North coast of Noto last November, the water reaches the cliff.North coast of Noto after the earthquake, the water is 50-100 m away from the cliff.North coast of Noto last November, the water reaches the cliff.North coast of Noto after the earthquake, the water is 50-100 m away from the cliff.
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Reposted by Sumiko Tsukamoto
Luca Malatesta @geoluca.bsky.social · 03/03/2024
As a result of liquefaction, we see manholes shooting up across the pavement. At first I thought it was the land sinking around fixed water pipes, but it seems that they do actually move up. Is it a matter of buoyancy? They're mostly empty after all. Does someone here know?
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Reposted by Sumiko Tsukamoto
Luca Malatesta @geoluca.bsky.social · 02/03/2024
Back in Noto Peninsula 🇯🇵 for a post earthquake survey. Here you see a bay near Monzenmachi, we measured 4.4m of coseismic uplift. The white rocks are covered by organisms that lived in the sea, now perennially emerged. Note the now dry harbor on the right.
A steep coast with a large swath of white rocks that separate a settlement and harbor from the coastline a couple hundred metres further.
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