Showing posts with label Volcanoes. Show all posts
Showing posts with label Volcanoes. Show all posts

Tuesday, 9 June 2026

Manus Island, Papua New Guinea, inundated with pumice following eruption of Titan Ridge submarine volcano.

A series of eruptions from the Titan Ridge submarine volcano, beneath the Bismarck Sea in the southwest Pacific Ocean, has produced a large volume of pumice (a light volcanic rock, produced by the rapid cooling of gas rich lava from submarine eruptions, which can float on the sea), much of which has washed up onto the shores of Manus Island, the largest of the Admiralty Islands and a province of Papua New Guinea. This has caused serious problems for the local population, as it has formed a barrier between them and the sea, too dense to push a boat through, but too quicksand-like to walk across. This in turn has prevented them from harvesting fish and other seafood, the main staples of the island, as well as forcing them to become entirely dependent on the islands limited supply of freshwater for washing and hygiene, rather than bathing in the sea. The large accumulations of pumice are also likely to have smothered local coral reef ecosystems, harming longer-term fishing prospects in the region.

Residents of Manus Island on a beach covered by pumice. ABC.

Pumice forms when hot lava from submarine volcanic eruptions encounters seawater and cools rapidly, simultaneously crystalising and degassing to form a lightweight volcanic rock with many gas filled vesicles (bubbles) within it, which often floats on the sea surface. Big submarine eruptions can produce large volumes of pumice, forming rafts of pumice that cover hundreds of square kilometres, and drift on the ocean surface for months before dissipating or washing ashore. 

Titan Ridge, also known as the Central Bismarck Sea Volcano, is located about 125 km to the southeast of Manus, on the northern edge of the South Bismarck Plate. It is located on the boundary between the Willaumez Transform Fault and an unnamed section of area of seafloor spreading, where the South Bismarck and Pacific plates are being pulled apart, while at the same time the Pacific Plate is moving to the west and the South Bismarck Plate to the east. Here fresh material from the upper mantle is rising up through the fault and being erupted from the volcano as volcanic material, primarily pumice caused by the rapid cooling of a liquid melt containing dissolved gasses. 

See also...




Friday, 20 February 2026

Eruption on Mount Kanloan causes ashfall events across Negros Island.

Mount Kanlaon, a 2465 m stratovolcano (cone shaped volcano made up of layers of ash and lava) on the northern part of Negros Island in the central Philippines, erupted slightly before 3.40 pm local time on Thursday 19 February 2026, according to the Philippines Volcano Observatories. The eruption comprised a series of explosions which lasted about two minutes and produced an ash column about 2 km high, and followed by a longer period of gas emissions. 

An eruption on Mount Kanloan, Negros Island, the Philippines, on Thursday 18 February 2026. Philippines Volcano Observatories.

The geology of the Philippines is complex, with the majority of the islands located on the east of the Sunda Plate. To the east of this lies the Philippine Sea plate, which is being subducted beneath the Sunda Plate (a breakaway part of the Eurasian Plate); further east, in the Mariana Islands, the Pacific Plate is being subducted beneath the Philippine Sea Plate. This is not a smooth process, and the rocks of the tectonic plates frequently stick together before eventually being broken apart by the rising pressure, leading to Earthquakes in the process. Material from the subducting Philippine Plate is heated by the temperature of the Earth's interior, causing lighter minerals to melt and the resultant magma to rise through the overlying Sunda Plate, fuelling the volcanoes of the Philippines.

Subduction beneath the Philippines. Yves Descatoire/Singapore Earth Observatory.

See also...

Sunday, 7 December 2025

Did an unknown volcanic eruption create the conditions for the Black Death to enter medieval Europe?

Between 1347 and 1353, the Black Death spread across Europe, killing up to 60% of the population, leading to long-lasting demographic, economic, political, cultural, and religious changes which changed the continent, and eventually the world, beyond recognition. Recent palaeogenetic studies have now confirmed the long held belief that the pandemic was caused by the Plague Bacterium, Yersinia pestis, a zoonotic disease with wild reserves in a number of Rodent species. Despite the presence of a wild reserve, outbreaks of Yersinia pestis in Human and Domestic Animal populations are quite rare, with only three documented pandemics of the disease. The first of these, the Plague of Justinian, began around 541 AD, and persisted into the eighth century. The second, the Black Death, began around 1338 in Central Asia, and persisted in places into the early nineteenth century. The third began in China in the 1770s, and spread around the world; arguably this third Plague pandemic is still ongoing, with all wild reserves and outbreaks outside Asia apparently derived from this source.

Studies of the archaeological, historical and ancient genomic records have suggested that the Black Death was a genetically distinct strain of the Yersinia pestis Bacterium which probably originated in arid foothills of the Tien Shan mountains west of Lake Issyk-Kul in modern-day Kyrgyzstan. This spread along the trade routes of Central Asia, entering Europe via the northern Black Sea region in the 1340s. Notably, the Black Death abruptly entered Venice and other Mediterranean ports in 1347, presumably through the importation of infected Fleas from the Black Sea reason. 

From this time, there were repeated outbreaks of Plague across Europe until the early nineteenth century, although it is unclear if these represent a series of re-introductions, or the presence of a wild-reserve within Europe. Nor is it entirely clear why the Plague appeared in multiple Mediterranean ports at the same time, having been established in the Black Sea region for some time prior to this, without previously making the jump, though it has been suggested by several people that some socio-economic challenge led to a change in Human behaviour at this time, giving the disease an opportunity to spread.

In a paper published in the journal Communications Earth & Environment on 4 December 2025, Martin Bauch of the Department Humans and Environment at the Leibniz Institute for the History and Culture of Eastern Europe, and Ulf Büntgen of the Department of Geography at the  University of Cambridge, the Global Change Research Institute of the Czech Academy of Sciences, and the Department of Geography at Masaryk University, present evidence for a volcanic eruption at an unknown location in the years prior to the Black Death reaching the Mediterranean, which caused a regional famine, leading traders to seek new sources of grain, and thereby opening the region to the arrival of the Plague.

Bauche and Büntgen note that there has been extensive previous research into potential links between a volcanically induced climate crisis at the start of the  Late Antique Little Ice Age and the onset of the Plague of Justinian, but little previous investigation into such a link to the onset of the Black Death. They also note that ice cores from Greenland and Antarctica have revealed a spike in sulphur concentrations in 1345 considerably larger than the one caused by the Mount Pinatubo eruption of 1991, which probably represents an injection of about 14 megatons of sulphur into the atmosphere. Furthermore, there were also major spikes in 1329, 1336 and 1341, representing eruptions which would have injected roughly 3.7, 0.7, and 1.2 megatons of sulphur into the atmosphere, respectively.

Weather records from Japan, China, Germany, France, and Italy, all record the years from 1345 to 1349 as being exceptionally cloudy. A lunar eclipse in 1345 is recorded as having been exceptionally dark by witnesses in both Bohemia and China; something which can be another sign of a high volcanic dust level within the atmosphere. 

Studies of tree rings have shown that trees in the Spanish Pyrenees produced 'blue rings' in 1345 and 1346, which are interpreted as signs severe cold spells during the growing seasons affected growth. The production of blue rings in consecutive years is considered exceptionally rare. Studies of wood density across the Northern Hemisphere have suggested a progressive cooling from 1345 to 1347, with 1347 being the coolest year since 1257, when a cold spell was linked to an eruption on Mount Samalas on Lombok Island, Indonesia. 

May–September (MJJAS) temperature anomalies from 1119–2020 AD (uncertainties are expressed by grey shading), based on 534 maximum latewood density (MXD) measurement series from living and relict samples from Mountain Pine, Pinus uncinata, trees from undisturbed upper treeline ecotones in the Spanish central Pyrenees.  The pre-Black Death cold phase is indicated by the vertical blue shading. The right-side double-stained thin section shows two consecutive Blue Rings that were formed in 1345 and 1346 AD in a Mountain Pine, Pinus uncinata, from the upper treeline in the central Spanish Pyrenees. Bauche & Büntgen (2025).

While it is harder to assess rainfall in past than temperature, tree-ring data suggests that the cool period from 1345 to 1347 was accompanied by a prolonged west-east dipole in Europe, with wetter conditions around the eastern Mediterranean and dryer conditions around the western Mediterranean. Morocco, the British Isles, northern France, the Low Countries, Germany and southern Scandinavia, all appear to have suffered dry conditions, while the Iberian Peninsula, Italy, and the Balkans, had high spring and summer rainfall in those years.

Bauche and Büntgen also examined historical records from across Europe and beyond, which show a declining agricultural output from across Europe from 1345, and in particular a failure of (environmentally sensitive) Grape crops from northwestern Italy. Severe flooding was also recorded in Italy in the autumn of 1345 and the springs of 1346 and 1347, along with accompanying problems such as soil erosion. The winter of 1344/45 was exceptionally cold and snowy in the Middle East, with the winters of 1345/46 and 1347/48 being marked by drought and Locust invasions. 

Late medieval Italy had a highly urbanised population, with a complex grain supply system in place to support this population. Many city states, including major centres such as Bologna, Florence, Genoa, Siena, and Venice, had limited farmland and large urban populations, consequently importing grain over long distances to redress this imbalance. Only Rome and Milan were largely self-sufficient. Cities developed communal granaries run by officials with the power to manage these granaries, source supplies of grain from elsewhere, and prevent the export of grain from cities troubled by poor harvests or military conflicts. Typically, managing grain supplies was the second-largest source of expenditure for any late medieval Italian city-state, behind only military spending. Maritime powers such as Venice, Genoa, and Pisa, negotiated treaties with grain-producing areas such as Apulia, Sicily, Sardinia, North Africa,  the Aegean and the Black Sea region. 

In 1346/7 severe famines were recorded across parts of Spain, southern France, northern and central Italy, Egypt, and the Levant. This led to spikes in the price of grain in Spain, Italy, Egypt, and even the Arabian Peninsula. Strict grain regulations were implemented in many Italian cities from 1346, at least in part to grain-shortage induced civil unrest.

Northern Italy suffered a series of famines during this interval, which appear unrelated to any political crisis, supporting a climate-related problem as the cause. Initially, this shortfall was met by increased imports from southern Italy, but it quickly became clear that this would not be sufficient to alleviate the crisis, and that more imports would be needed from further afield. 

At this time, Venice and Genoa were in a state of conflict with the Mongols of the Golden Horde, who had been trying to eliminate Italian power in the Black Sea region. This had led to the Italian cities blockading the ports of the Black Sea, preventing the Mongols from trading with the Mediterranean. However, the onset of famine in Italy led to a re-appraisal of this situation, with a ceasefire and renegotiation of trading arrangements leading to a restoration of grain trading, saving Venice from starvation.

The Plague Bacterium, Yersinia pestis, had been present in the Black Sea region for some time, and it is likely that it would eventually have reached the Mediterranean at some point. However, Bauche and Büntgen contest that the lifting of the trade embargo against the Golden Horde in response to the volcanically-induced famine affecting northern Italy was the immediate cause of the Black Death reaching multiple Mediterranean ports in a short interval. 

The trade embargo was lifted in 1347, and shortly thereafter, Venetian and Genoan trading vessels began entering the trading ports of the northern Black Sea and the Sea of Azov, returning to Italy laden with grain. The Plague appeared in Venice less than two months after the first such trading vessel. In March 1348 Venice lifted an embargo on the export of grain to Padua, with the first Plague outbreak there coming shortly after. Records of the grain trade to Florence and Sienna are less clear, but again the first Plague outbreaks in these cities were associated with the abating of the famine. Notably, this first wave of Plague outbreaks did not affect cities such as Rome, Milan,Verona, Ferrara, Ravenna, and Bari, which controlled larger grain producing areas, and were not involved in grain imports from the Black Sea region. Elsewhere around the Mediterranean, Marseille, Palma de Mallorca, and many other important port cities had Plague outbreaks before the end of 1347, probably as a result of grain shipments from Genoa. Smaller cities such as Savona, Ventimiglia, and Tunis, began to suffer outbreaks in April 1348, again probably linked to Genoan grain shipments. The reached Trento along with grain shipments from Venice, and from their spread across the Alps into northern Europe. 

Grain trade and plague dispersal. Main aspects of the Venetian, Genoese, and Pisan grain trade network that prevented much of Italy from starvation in 1347 AD but also brought the Plague Bacterium, Yersinia pestis, to Venice and other Mediterranean harbours during the second half of 1347 AD, from where it spread rapidly. Location of the tree ring-based climate reconstructions is indicated (with two sites in Scandinavia not shown). Map is an equal-area, pseudo-cylindrical Mollweide projection with greyscale referring to elevations above sea level. Bauche & Büntgen (2025).

In 1344, a decade-long papal embargo on trade with the Mameluke Sultanate was lifted, enabling Italian merchants to resume trade with the Middle East. Following the resumption of trade with the Black Sea region, Venetian ships began carrying grain to Alexandria, and the ports of the Levant, while Mameluke traders began visiting the ports of the Crimea. While individual shipments are harder to trace for these ports than those of Italy, these ships are probably responsible for the arrival of the Black Death in North Africa and the Middle East.

Thus the resumption of trade with the Black Sea region appears to have resolved the immediate problem of a widespread famine, but also led to the simultaneous import of the Black Death to ports around the Mediterranean. The subsequent rapid spread and high fatality rate for the disease may also have been a result of a population weakened by famine. The sophisticated trade system developed by the Italian city states to ensure against famine appears to have made those states, and their allies around the Mediterranean and Europe, particularly vulnerable to the spread of the Plague. Bauche and Büntgen conclude that the Black was not just a singular event, but rather the culmination of a prolonged crisis which began with a climate crisis and then a famine.

See also...

Monday, 24 November 2025

Ethiopian volcano erupts for first time in recorded history.

Hayli Gubbi, a shield volcano in the Afar Region of Ethiopia, erupted on Sunday 23 November 2025, for what appears to be the first time in recorded history. The volcano erupted for under twelve hours, from about 11.30 am to about 11.00 pm local time (about 8.30 am to about 8.00 pm GMT), producing an ash column about 14 km high, which drifted to the east over the Red Sea, according to the Toulouse Volcanic Ash Advisory Centre. Nobody was directly hurt by the eruption, but local farmers report crops being covered with ash, which may potentially lead to famine in the region.

An ash cloud over Hayli Gubbi on 23 November 2025. Afar Government Communication Service.

Hayli Gubbi is a 493 m high scoria cone (cone of ash) sitting on an older shield volcano (dome shaped volcano made up of layers of lava) located at the southernmost end of the Erte Ale Volcanic Chain. The volcano has never been observed to erupt before, and it is thought not to have erupted since the Late Pleistocene, more than 12 000 years ago, although the remote location of the volcano means that it has not been studied well. 

The deserts of Northern Ethiopia and Southern Eritrea are extremely volcanicly active, with dozens of volcanoes fed by an emerging divergent margin along the East African Rift; the Erta Ale Chain lies on the Ethiopian Rift, the boundary between the Nubian Plate and the Danakil Microplate. The African Plate is slowly splitting apart along the Ethiopian Rift and the East African Rift to the south (which is splitting the Nubian Plate to the West from the Somali Plate to the East). Arabia was a part of Africa till about thirty million years ago, when it was split away by the opening of the Red Sea Rift (part of the same rift system), and in time the Ethiopian and East African Rifts are likely to split Africa into a number of new landmasses.

Rifting in East Africa. The Danakil Microplate is the red triangle to the east of the Afar depression at the southern end of the Red Sea. Università degli Studi di Firenze.

See also...

Wednesday, 19 November 2025

Eruption on Mount Semeru.

People living close to Mount Semeru, a 3676 m high stratovolcano (cone-shaped volcano made up of layers of ash and lava) close to the city of Lumajang in East Java, have been advised to avoid going near the volcano, following an eruption on Wednesday 19 November 2025. The volcano began erupting at about 4.00 pm local time (about 9.00 am GMT) producing an ash column about 5.6 km high, and triggering a series of pyroclastic flows (avalanches of hot rock, ash and gas) which reached as far as 7.00 km from the volcano.

A column of Ash above Mount Semeru on 19 October 2025. Badan Geologi/AP.

Mount Semeru forms part of the Tengger Volcanic Complex is a string of five overlapping stratovolcanoes (cone-shaped volcanoes) forming a single massif, extending northward from Semeru. The whole massif sits within a vast caldera (volcanic crater), left by the explosion of an ancient volcano about 150 000 years ago. The volcanoes are at the center of this caldera, surrounded by a vast sea of sand, the Tengger Sand Sea.

The approximate location of Mount Semeru. Google Maps.

The Indo-Australian Plate, which underlies the Indian Ocean to the south of Java, is being subducted beneath the Sunda Plate, a breakaway part of the Eurasian Plate which underlies Java and neighbouring Sumatra, along the Sunda Trench, passing under Java, where friction between the two plates can cause Earthquakes. As the Indo-Australian Plate sinks further into the Earth it is partially melted and some of the melted material rises through the overlying Sunda Plate as magma, fuelling the volcanoes of Java and Sumatra.

Subduction along the Sunda Trench. Earth Observatory of Singapore.

See also...