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Yahoo
7 days ago
- Science
- Yahoo
Ghana has a rare treasure, a crater made when a meteor hit Earth: why it needs to be protected
Impact craters are formed when an object from space such as a meteoroid, asteroid or comet strikes the Earth at a very high velocity. This leaves an excavated circular hole on the Earth's surface. It is a basic geological process that has shaped the planets from their formation to today. It creates landscapes and surface materials across our solar system. The moon is covered with them, as are planets like Mercury, Mars and Venus. On Earth, impacts have influenced the evolution of life and even provided valuable mineral and energy resources. However, very few of the impact craters on Earth are visible because of various processes that obscure or erase them. Most of the recognised impact craters on Earth are buried under sediments or have been deeply eroded. That means they no longer preserve their initial forms. The Bosumtwi impact crater in Ghana is different, however. It is well preserved (not deeply eroded or buried under sediments). Its well-defined, near-circular basin, filled by a lake, is surrounded by a prominent crater rim that rises above the surface of the lake and an outer circular plateau. This makes it a target for several research questions. As an Earth scientist, I joined a research team from 2019 to better understand the morphology of the crater. We carried out a morphological analysis of the crater (a study of its form, structure and geological features). This study concluded that the activities of illegal miners are a threat to the sustainability of the crater. We also discovered that the features of the Bosumtwi impact crater can be considered as a terrestrial representation for a special type of impact crater known as rampart craters. These are common on the planets Mars and Venus and are found on icy bodies of the outer solar system (like Ganymede, Europa, Dione, Tethys and Charon). For future studies, the Bosumtwi impact crater can be used to help understand how rampart craters form on Mars and Venus. So the Bosumtwi impact crater should be protected and preserved. Read more: The crater The Bosumtwi impact crater is in Ghana's mineral-rich Ashanti gold belt. It is the location of the only natural inland lake in Ghana. As one of the world's best-preserved young meteorite impact craters it is designated as an International Union of Geological Sciences geoheritage site. It is one of only 190 confirmed impact crater sites worldwide, one of only 20 on the African continent. Its lake is one of six meteoritic lakes in the world, recognised for their outstanding scientific value. At almost 1.07 million years old, the crater offers unparalleled opportunities for studying impact processes, climate history and planetary evolution. It's an irreplaceable natural laboratory for researchers and educators. Beyond its scientific importance, the crater holds cultural significance for the Ashanti people of Ghana. The lake at its centre serves as a sacred site and spiritual landmark. The crater's breathtaking landscape also supports eco-tourism and local livelihoods, contributing to Ghana's economic development while maintaining exceptional aesthetic value. The research As part of further research work on the 2019 study, in 2025 we have discovered through field work and satellite data analysis that illegal artisanal mining is prevalent in the area and threatening the crater. This refers to informal, labour-intensive extraction of minerals, primarily gold. It is conducted by individuals or small groups using basic tools and rudimentary machinery. The use of toxic chemicals such as mercury and cyanide, and practices such as river dredging, cause severe environmental harm. Illegal miners are encroaching on and around the crater rim, posing severe threats to its environment and sustainability. Their activities have become more prevalent over the course of less than 10 years, indicating a growing problem. If unchecked, it could lead to irreversible damage to the crater. These mining operations risk contaminating the lake with toxic heavy metals. The consequences of these are grave. They include destroying critical geological evidence, accelerating deforestation, and degrading the land. All this damages the crater's scientific, cultural and economic value. The International Union of Geological Sciences geoheritage designation of the crater underscores the urgent need for protection measures. The loss of this rare geological wonder would represent not just a national tragedy for Ghana, but a blow to global scientific heritage. Immediate action is required. This includes enhanced satellite monitoring (tracking illegal mining, deforestation and environmental changes) using optical imagery (such as Sentinel-2, Landsat, PlanetScope). These tools can detect forest loss, identify mining pits and sediment runoff, and analyse changes over time. Stricter enforcement of mining bans, and community engagement programmes, will help preserve the Bosumtwi impact crater's unique attributes for future generations of scientists, students, tourists and local communities who depend on its resources. This article is republished from The Conversation, a nonprofit, independent news organization bringing you facts and trustworthy analysis to help you make sense of our complex world. It was written by: Marian Selorm Sapah, University of Ghana Read more: How are Australians adapting to climate change? Here are 729 ways The US Environmental Protection Agency's retreat from science endangers the health of people and the planet EU efforts to measure companies' environmental impacts have global effects. Here's how to make them more just Marian Selorm Sapah does not work for, consult, own shares in or receive funding from any company or organisation that would benefit from this article, and has disclosed no relevant affiliations beyond their academic appointment. Solve the daily Crossword
Scoop
08-05-2025
- Science
- Scoop
Archeologists Join Geologists In The Quest To Define The Age Of Humans
The evolution of the human mind has allowed us to transcend our modern understandings of time and expand into the realm of 'deep time thinking.' One example of this is the Geologic Time Scale (GTS), a human construct that traces the astrophysical events that have affected the composition and structure of the Earth since it was formed some 4.6 billion years ago. Scientists have assembled bits and pieces of this huge temporal scale into periods of relative climatic and biotic stability based on geological and fossil data. By ordering these events sequentially in time, they have been able to reconstruct when, how, and under what conditions life emerged on the planet. Under the aegis of the International Union of Geological Sciences (IUGS), the International Commission on Stratigraphy (ICS) is charged with defining geological epochs based on fundamental changes registered in the Earth's geological formations. The GTS is often depicted with spiraling concentric branches divided into segments representing distinct geological epochs defined by periods of relative geobiological stability. These epochs are named, dated, and ordered, and the length of each segment is proportional to its duration relative to the other phases. As we progress toward the outer rings of the spiral, we notice that the time segments gradually become smaller, especially around 500 million years ago after the unprecedented proliferation of complex life forms that appeared during the Cambrian explosion, which accelerated the pace of global ecological changes registered in the Earth's layers. The emergence of the first humanoid species has been traced back to only around 7 million years ago and is placed at the extreme tip of the last branch of the spiral, underscoring how little time has passed, relatively, since our ancestors appeared on the planet. Based on global climatic data, the evolutionary story of the genus Homo has taken place throughout the Quaternary Period that began around 2.58 million years ago during the Pleistocene Epoch. This period roughly overlaps with the invention of the first breakthrough human technologies made from stone. A global warming event that began 11,650 years ago around the same time as the emergence of early sedentary civilisations in the Fertile Crescent signals the start of the Holocene Epoch, in which we currently live. The Anthropocene (The Age of Humans) has been proposed as a new geological epoch after or within the Holocene, and, if formalised, would be the first to be introduced based on geologically observable effects of human activity on the planet. This compelling proposal spurred the establishment of the Anthropocene Working Group (AWG), which is tasked to evaluate whether the geophysical signature of human behavior is sufficient to justify placing this new epoch at the apex of the spiraling branches of the GTS. While many scientists agree on the idea in principle, a major point of contention is when exactly the Anthropocene began. Not surprisingly, pinpointing a precise threshold when human activity caused recognisable global geological alteration has proven to be a very difficult task that geologists and archeologists are working together to resolve. Some archeologists consider the Anthropocene as an incremental process, whose genesis can be identified diachronically in the Earth's strata as early as tens of thousands of years ago, when modern humans consolidated planetary dominance, appropriating and transforming landscapes and biotic resources in archeologically detectable ways. Anthropogenic signals, such as changes in ecosystems brought on by human overhunting of ice age megafauna, can be traced back to this period. By 10,000 years ago, plant and animal domestication boosted human ecosystem engineering as populations grew steadily through time. By around 5,000 years ago, the first urban dwellings drew swelling numbers of individuals into restricted areas, and technological innovation surged after the invention of metallurgy. Growing populations and intensified farming consumed and modified land, and animal husbandry led to increases in methane emissions traceable in the Earth's sedimentary record. The human imprint on the planet becomes significantly more conspicuous after the industrial age was launched in the Western world around 200 years ago, with an upsurge in carbon emissions from burning coal to feed technological development and increasing concentration of greenhouse gases driving global warming. While viable arguments support each of these signposts along our evolutionary highway, the AWG concluded that the most suitable time to begin the Anthropocene would be in the 1950s, when the Great Acceleration sharply augmented the signs of human activity in the global geological record. This made the signs even more clearly distinguishable thanks to a wide range of indicators synchronously chronicling their symptoms, like climate deregulation, atmospheric, terrestrial, and water pollution, loss of biodiversity, excessive resource consumption, and massive land transformations. In March 2024, the IUGS decided not to formally integrate the Anthropocene into the GTS; a verdict that has hardly quelled disagreements surrounding this matter. And there are other problems related to this issue. For example, while the existing chronostratigraphic divisions of the GTS register periods of stability lasting millions of years, the Anthropocene would be the first geological epoch to occur within only a human lifetime. Even if we situate its beginning thousands of years before the industrial revolution, the Anthropocene sedimentary archive is currently still under formation. No matter the outcome of this fascinating planet-wide debate, the Anthropocene has indelibly entered into scientific and social discourse as the world faces many challenges posed by the unprecedented expansion of advanced human populations with unique techno-social behaviors that are now clearly linked to cataclysmic climatic events and biological genocide. It has become evident that the implications of the Anthropocene now exceed the question of its validity as a geochronological division in the Earth's evolutionary history. While geologists examine the end results of long-term paleoecological scenarios, archeologists center on more recent layers that record the origins and evolution of human life (the archeosphere). Fascinating interpretations are coming out of the collaboration between geologists and archeologists on the issue of the Anthropocene. Among these, the concept of the physical technosphere is particularly interesting since it addresses questions about how the entire mass of materials manufactured and modified by humans is becoming assimilated into the Earth system. In 2016, Jan Zalasiewicz and colleagues estimated the total mass of the physical technosphere to be a staggering 30 trillion tons, and it continues to grow, far surpassing both the volume and the diversity of the domesticated biosphere (plants and animals). 'We define the physical technosphere as consisting of technological materials within which a human component can be distinguished, with part in active use and part being a material residue. The human signature may be recognised by characteristics including form, function and composition that result from deliberate design, manufacture and processing. This includes extraction, processing and refining raw geological materials into novel forms and combinations of elements, compounds and products,' stated the article by Zalasiewicz and colleagues published in the Anthropocene Review, United Kingdom. The study further added, 'The active technosphere is made up of buildings, roads, energy supply structures, all tools, machines, and consumer goods that are currently in use or usable, together with farmlands and managed forests on land, the trawler scours and other excavations of the seafloor in the oceans, and so on. It is highly diverse in structure, with novel inanimate components including new minerals and materials… and a living part that includes crop plants and domesticated animals. Humans both produce and are sustained by (and now are dependent on) the rest of the physical technosphere.' Although it was formed culturally because of anthropogenic agency, the technosphere combined with natural forces, has become an integral part of the functioning Earth system. It operates above and below the ground, in the seas, and even in outer space, with components interacting constantly and dynamically with the lithosphere, the biosphere, the hydrosphere, and the atmosphere. While these other spheres have evolved over millions, or even billions of years, the technosphere—like the Anthropocene—has existed for a comparatively minute period of time. Continuously growing in pace with human demography and technological advances, the technosphere now generates so much excess waste that it cannot all be recycled back into the system, creating an imbalance in the structural relationships guiding the planet's equilibrium and generating traceable Anthropocene deposits. Beyond its physical aspects, the technosphere also encompasses the human social structures that enable it to function and in which all individuals play a part. Much like the synapses within the human brain or molecular systems forming the parts of a larger whole, humans constitute the individual components of the technosphere, cooperating to enable it to function while also creating the need for its existence. 'The technosphere is also manifest in the wide distribution of myriad artefacts such as needles, motors, and medicines, and by technological or technologically assisted processes like pumping and harvesting, as well as by nominally human activities that are closely tied to technological processes, such as watching television or filling out tax forms. Most such localised systems, processes and artefacts derive from, or are connected either directly or indirectly to, the globe-spanning networks of the technosphere,' stated the 2014 article by P. K. Haff, published in the Geological Society, London. Following geological precepts and using methodologies classically applied in archeological sciences, the imprint of human activity on the planet is gradually being defined, quantified, mapped, and categorised, while novel subjects like technospheric taxonomy are being developed to complement traditional geological and stratigraphic practices. Just like the remnants of prehistoric material culture—like stone tools or pottery sherds—the objects we produce, use, and throw away in our daily lives are transforming into technofossils that will become markers in the chronocultural framework of human evolution, providing fodder for future archeologists. At the generational scale, residues from polluting gases, sewage, toxic chemicals, and microplastics are melding into sedimentary layers, and artificial ground transformed by landfills, war rubble, mining, and urban settings is converted into novel anthropic geological settings with the passage of time. There is no doubt that scarring and modification of land and sea resulting from wars, agriculture, urbanisation, mining, and other human activities are being incorporated into the Earth's geological layers. The evolution of human technologies has led our species to embark on an ongoing process that began incrementally and snowballed exponentially over the millennia, converting into the emblem of modern human heritage. The global distribution of all human waste will be chronicled in relation to its position in sub-actual sedimentary formations that—in the not so distant future—will serve to define and classify the sequential cultural contexts of the Anthropocene. Author Bio: Deborah Barsky is a writing fellow for the Human Bridges, a researcher at the Catalan Institute of Human Paleoecology and Social Evolution, and an associate professor at the Rovira i Virgili University in Tarragona, Spain, with the Open University of Catalonia (UOC). She is the author of Human Prehistory: Exploring the Past to Understand the Future (Cambridge University Press, 2022). Credit Line:
Japan Times
01-04-2025
- General
- Japan Times
Tsukuba massif granite, one of the world's few heritage stones
In 2024, the Tsukuba massif granite of the Mt. Tsukuba Area Geopark was certified by the International Union of Geological Sciences as one of the first 55 IUGS Heritage Stones, which have been 'used in significant architecture and monuments' and 'recognized as integral aspects of human culture.' In a recent interview with The Japan Times, Mt. Tsukuba Area Geopark Promotion Council specialist Kaoru Sugihara, a geologist and former professor, spoke about the characteristics of the region's granite and the positive effects that the certification has brought. The geopark covers a large area in central Ibaraki Prefecture west of Lake Kasumigaura, Japan's second-largest lake. With Mount Tsukuba at its center and many other smaller mountains, the area is home to three main types of granite, formed at different times and named after the areas where they are found: Tsukuba granite, Kabasan granite and Inada granite. 'They can be further divided into smaller groups based on their characteristics,' Sugihara said. 'But it is not only the geological diversity and scientific value that the IUGS recognizes, but also the cultural and historical value of the stones based on how local people have used the resources.' He explained that the council had decided to apply for certification for a number of reasons. 'By having our important regional resource certified by a global organization, we will be able to promote not only the stones, but also the geopark itself. This will help increase the international presence of Japan's geopark network and contribute to the broader global geopark community,' he said. Another purpose was to promote and support the local stone industry: 'We need to preserve the special techniques of mining and stone working while securing human resources. This certification was a perfect opportunity for people in the industry to think about how to preserve the mining culture in a sustainable way while preserving the geological heritage itself.' The certification was also an opportunity to reassess the local history and culture. Sugihara noted that in ancient times, mountain worship flourished in this area, and huge stones and rocks found in the mountains were the object of worship and places for ascetic practices. In the Kamakura Period, the value of these stones as building materials was further recognized, and stone-carving technology developed in the area. An artisan works on a Makabe stone lantern made from Kabasan granite. | MT. TSUKUBA AREA GEOPARK PROMOTION COUNCIL 'With the introduction of Western culture to Japan during the Meiji Era, Western-style stone architecture flourished in the Kanto region, leading to the extensive use of granite from the Tsukuba mountains in buildings that are now recognized as National Treasures and important cultural assets,' said Sugihara. He pointed out that a major outcome of the IUGS Heritage Stone certification has been an increased interest in the geopark among those involved in the stone industry, and a heightened sense of confidence and pride in the history and techniques of the local stone industry. 'There has also been an increased awareness of the need for sustainable practices within the stone industry. I believe it is possible to find ways to improve the sustainability of stone quarrying and processing while preserving the rich history and culture of the region, which is rooted in the use of stone as a resource,' he said. He also noted that efforts are being made to improve technology to increase the proportion of commercially viable stone, which has been less than 30% of the total extracted from the mountains. 'The development of new products using stone waste, including toys and craft items, is also underway,' he said. The council is also planning tours to Tokyo this year to visit places and buildings where Ibaraki granite is used. 'For example, the granite mined in the Inada region, in the northern part of the geopark, is used in the walls of the Supreme Court of Japan,' Sugihara said. He noted that various parts of the Diet building and Tokyo Station are also made of granite from Ibaraki. 'We hope to bring people from Tokyo and other parts of Japan to Ibaraki to see the quarries and how the stone is processed,' he said. The Tsukuba Geo Museum features exhibits, educational installations and video materials that help people learn how stone is formed, mined, processed and made into building materials and traditional crafts such as stone lanterns. 'Through various efforts, we aim to arouse interest in the industry among younger generations in order to preserve the regional culture,' Sugihara said. Tsukuba is a member of the Sustainable Japan Network, a group of companies that cooperate with this newspaper to spread information about sustainability in Japan. You can also be part of the network; visit for more details.
