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Conversations on a century of geoscience in Europe: Part 1

Conversations on a century of geoscience in Europe: Part 1

When you think about the last century of geoscience, what comes to mind? Perhaps Alfred Wegener’s theory of continental drift? Or Inge Lehmann’s discovery of Earth’s solid inner core?

Over the last 100 years, geoscientists have made incredible contributions to our understanding of the Earth, the solar system, and beyond. The science community has explored uncharted territory, challenged previously held conceptions, provided vital information to policymakers, worked to address societal challenges, and put forth paths for sustainability. Through the years, researchers have also worked to promote diversity, inclusion, transparency, and accessibility in the geosciences. Many Europe-based scientists have been at the forefront of these advances.

Inspired by the centennials of the American Geophysical Union (AGU) and the International Union of Geodesy and Geophysics (IUGG), which were both founded in 1919, we would like to highlight Europe’s role in shaping the geosciences and the great achievements of European geoscientists within the last century.

In this series of interviews, scientists across different disciplines and scientific fields reflect on the last 100 years of Earth, space and planetary sciences in Europe and share their perspectives on the future:


Anne-Marie Treguier: Research Director at the French National Centre for Scientific Research and the European Institute for Marine Studies in the Ocean Physics Laboratory

The responsibility of geoscientists is huge. We must frame our scientific questions in the context of a wide range of future scenarios..

Read interview →

 

John Burrows: Professor of the Physics of the Ocean and Atmosphere and a Director of the Institutes of Environmental Physics and Remote Sensing at the University of Bremen

The history of discoveries in the geosciences is a fascinating story, involving unexpected and perplexing observations..

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Günter Blöschl: Head of the Institute of Hydraulic Engineering and Water Resources Management and Director of the Centre for Water Resource Systems of the Vienna University of Technology

As Heraclitus said, there is nothing permanent except change. Innovation needs to be permanent. We are in for an exciting future..

 

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Antje Boetius: Director of the Alfred Wegener Institute (AWI) Helmholtz Center for Polar and Marine Research and Professor of Geomicrobiology at the University of Bremen

When one reads the original reports and letters, we can learn how relevant expeditions and fieldwork were – and still are – for the international, collaborative spirit of the geosciences worldwide. The amazing thing is, in many ways we have remained explorers of our own planet Earth even today..

 

 

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Bernhard Diekmann, Head of the Research Unit Potsdam of the Alfred Wegener Institute (AWI) Helmholtz Center for Polar and Marine Research and Professor of Quaternary Geology at Potsdam University

During the last 100 years, the focus in geological research was understanding of processes in Earth’s interior and skin…The geosciences should no longer be seen as an individual field of research, but must be integrated into a holistic view of natural and social sciences..

 

Read interview →

Interviews by Olivia Trani, EGU Communications Officer

Imaggeo on Mondays: The salt mine carving into the Carpathians

Imaggeo on Mondays: The salt mine carving into the Carpathians

The image gives us a glimpse into the Slănic Salt Mine in central Romania, about 100 kilometres north of the capital city Bucharest. The region was actively mined for almost 30 years, from 1943 to 1970.

The Slănic Salt Mine is the largest salt mine in Europe, and the facility consists of 14 large chambers, each more than 50 metres high. The cavities of the mine, more than 200 metres deep, carve into the Southern Carpathian Mountains, offering a unique large-scale view into how the layers of rock beneath the Earth’s surface bend and fold. The structures featured in this image were stretched out over time as the Earth’s tectonic plates shifted, highlighting just how fluid our planet can be.

Compared to other rocks, the rock salts in this mine can change form and flow without much pressure and at relatively shallow depths. “This flow is however very slow, so that man-made cavities in salt mines deform very slowly and remain open for decades,” notes Janos Urai, a professor of structural geology, tectonics and geomechanics at RWTH Aachen University in Germany who snapped this image while visiting the mine in 2017. “We study this slow flow of salt in nature, to be able to improve predictions of the long-term evolution of nuclear waste repositories and abandoned salt caverns.

The mine is no longer used for resource extraction, but is now an active tourist destination (there are even playgrounds, pool tables and other recreational features).

By Olivia Trani, EGU Communications Officer

You can learn more about salt tectonics on the Tectonics and Structural Geology blog here:  Minds over Methods: Reconstruction of salt tectonic features

Imaggeo is the EGU’s online open access geosciences image repository. All geoscientists (and others) can submit their photographs and videos to this repository and, since it is open access, these images can be used for free by scientists for their presentations or publications, by educators and the general public, and some images can even be used freely for commercial purposes. Photographers also retain full rights of use, as Imaggeo images are licensed and distributed by the EGU under a Creative Commons licence. Submit your photos at http://imaggeo.egu.eu/upload/.

July GeoRoundUp: the best of the Earth sciences from around the web

July GeoRoundUp: the best of the Earth sciences from around the web

Drawing inspiration from popular stories on our social media channels, major geoscience headlines, as well as unique and quirky research, this monthly column aims to bring you the latest Earth and planetary science news from around the web.

Major story

The world soaks up the sun

This summer our planet experienced the hottest June in recorded history, with the average global temperature reaching 16.4 °C, and July is on track to becoming the hottest month ever measured on Earth. And if you either live in or have been visiting Europe over the last few weeks, it sure feels like record-breaking heat.

In both June and July, several regions in Europe reached all-time temperature highs as warm air from northern Africa made its way through the continent. A rapid analysis done by researchers affiliated with the World Weather Attribution Network shows that human-caused climate change made the June heatwave at least five times more likely to happen. Furthermore, the scientists say in their report that “every heat wave occurring in Europe today is made more likely and more intense by human-induced climate change.”

Heatwaves this intense can put human health at risk and even be deadly in severe cases. A death toll reported that extreme heat Europe in the summer of 2003 led to more than 70,000 deaths throughout the continent.

The heatwave is now advancing towards Greenland, scientists report, and increased heat in the Arctic will likely lead to “another major peak in melt area,” said Twila Moon, a research scientist with the National Snow and Ice Data Center (NSIDC) in Colorado, US, to Live Science.

Simultaneous to the heatwave, a new study has reported that Earth’s current global warming is the only worldwide climate event to have happened in the last 2,000 years. While there have been notable climate events within the last few centuries, such as dramatic temperature changes from volcanic eruptions, the impact of these events were more regional rather than universal. In contrast, the study finds that modern climate change has affected 98 percent of the world.  “Absolutely nothing resembling modern-day global warming has happened on Earth for at least the past 2,000 years,” said the Atlantic.

50 years since one small step

20 July 2019 also marked the 50th anniversary of the first human steps on the Moon. In 1969, NASA astronauts Neil Armstrong and Buzz Aldrin landed on the Moon’s surface as part of the Apollo 11 Mission, revolutionising our understanding of our closest cosmic neighbor. For the 21 hours and 36 minutes on the lunar landscape, Armstrong and Aldrin reported field observations, installed instruments for multiple experiments, and gathered more than 20 kilograms of rock and dust samples.

Since then, scientists have made several discoveries from the data collected during the Apollo 11 Mission. For example, the rocks brought back from the Moon were determined to be about 4.5 billion years old, not much older than the Earth. Geoscientists also found that rocks from the Moon were very similar chemically to those on Earth, suggesting that the two bodies could have evolved in tandem from a large impact event, a leading theory also known as the giant-impact hypothesis.

Lunar Module pilot Buzz Aldrin photographed during the Apollo 11 extravehicular activity on the moon. Aldrin had just deployed the Early Apollo Scientific Experiments Package. In the foreground is the Passive Seismic Experiment Package; beyond it is the Laser Ranging Retro-Reflector (LR-3). Credit: NASA

While operational, the lunar seismometers installed by Armstrong and Aldrin detected ‘moonquakes’ and revealed that the Moon has a relatively small solid core and a thicker crust compared to the Earths’ interior.

Armstrong and Aldrin also set up a Laser Ranging Retroreflector to precisely measure how close the Moon is to the Earth. The retroreflector is still operational to this day, and the data obtained from the experiment shows that the Moon is almost literally inching away from the Earth at 3.8 centimetres (1.5 inches) each year on average.

These examples are just some of the discoveries made following this mission, and scientists are still studying the samples and data obtained 50 years ago to learn more about the Moon, the Earth and the solar system.

“One of the biggest misconceptions is that the Apollo samples aren’t being studied anymore, and that the Apollo samples only tell us about the moon,” says Ryan Zeigler, Apollo sample curator at the Johnson Space Center, in Science News.

What you might have missed

A new study published in July reported that tidewater glaciers, ones that flow from land to sea, could be melting much faster than previously thought. By analysing detailed measurements collected through radar, sonar and time-lapse photography, a team of researchers found that one Alaskan tidewater glacier is releasing a surprising meltwater from below the surface of the ocean.

“The melt rates that we measured were about 10 to 100 times larger than what theory predicted,” says lead study author David A. Sutherland, an oceanographer at the University of Oregon, in Scientific American.

The new findings could help scientists better understand how glaciers respond to global warming and how such glacial melt contributes to sea level rise and impacts local ecosystems.

Researchers studying LeConte Glacier in Alaska have found that its melt rate was 10 to 100 times larger than expected. Credit: US Forest Service, Carey Case

Other noteworthy stories

The EGU story

In July we are advertised another vacancy at the EGU Executive Office in Munich, Germany: EGU Communications Officer. The successful candidate will manage the EGU blogs and social media channels and be the office contact point for early career scientists.

Additionally, we are providing an EGU member with the opportunity to visit Brussels and work alongside a Member of the European Parliament (MEP) for a day. The pairing scheme will enable the selected EGU member to experience the daily work of an MEP, learn more about the role of science in policymaking, and potentially provide expertise on a science-policy issue. Interested EGU members should apply by 6 September.

Also in July, we have opened the call for candidates for EGU Union President, General Secretary and Division Presidents: if you’d like to nominate yourself or propose a candidate, you can do so by 15 September.

Finally, if you’d like to apply for financial support from the EGU to organise a meeting, make sure to submit an application by 15 August. This is also the deadline to submit proposals for Union Symposia and Great Debates at the EGU General Assembly 2020. The deadline for scientific sessions and short courses is 5 September.

Imaggeo on Mondays: Loch Coruisk – home of the wild Kelpie

Imaggeo on Mondays: Loch Coruisk – home of the wild Kelpie

On the south-western coast of the Isle of Skye, Scotland, lies Loch Coruisk, supposedly home of a water horse. At the southern end of this freshwater Loch, the Scavaig River discharges into a sea Loch, Loch na Cuilce. Loch Coruisk snuggles close to the center of the Cuillin Hills complex, younger than both the northern and southern formations of the Isle. At present, the neighbouring hills are dominated by Paleogene intrusive bytownite gabbros that are responsible for the jagged outline of the topography. Cuillin Hills forms the remains of an eroded magmatic chamber.

Description by Cedric Gillmann, as it first appeared on imaggeo.egu.eu.

Imaggeo is the EGU’s online open access geosciences image repository. All geoscientists (and others) can submit their photographs and videos to this repository and, since it is open access, these images can be used for free by scientists for their presentations or publications, by educators and the general public, and some images can even be used freely for commercial purposes. Photographers also retain full rights of use, as Imaggeo images are licensed and distributed by the EGU under a Creative Commons licence. Submit your photos at http://imaggeo.egu.eu/upload/.