Skip navigation.

exploreopera

| Help

Sign up | Help

olelog

What on earth

Toba - A Significant Geological Event

,

The theme of the ninth Accretionary Wedge hosted by Julian at Harmonic Tremors is significant geological events. I suppose that an event that nearly wiped out all human beings could be called significant.

In 1998 Stanley Ambrose proposed that the eruption of the supervulcano Toba reduced the world's human population to 10,000 or even a mere 1,000 breeding pairs. The findings were supported by DNA evidence. The last glacial period was preceded by one thousand years of the coldest temperatures of the Later Pleistocene, 71 to 70 thousand years ago. The intriguing but as yet unproven speculation is that it was caused by the eruption of Toba, Sumatra, leading to a “volcanic winter”. Toba was the largest known explosive eruption in the last two million years.

The length or severity of global cooling caused by the Toba eruption is debatable. The Indian subcontinent contains extensive deposits from the eruption. In a series of stone artefacts unearthed in southern India (Jwalapuram) suggest that local human populations remained in the region after the Toba eruption. The prehistoric tools were found in more than 7.5 m of sedimentary layers sandwiching a layer of ash produced by the Toba eruption, and the tools above were essentially at the same level of evolution as those below. The findings published in Science of 6 July 2007 seem to indicate that the impact of the Toba eruption was not as significant as earlier thought.

The Toba supervolcano-eruption produced the largest known volcanic eruption on earth during the past 2 million years. About 71,500 years ago, give or take a rough 4,000 years, an estimated minimum of 2800 km3 of magma were erupted, of which at least ca. 800 km3 was transported in atmospheric ash plumes that blanketed an area from the South China Sea to the Arabian Sea. This total volume is even more than the Yellowstone super-volcano eruption, much debated a couple of years ago, with a volume of an estimated 2500 km3 . The eruption led to the final formation of one of Earths largest calderas, the 35x100 km wide Toba caldera (See landsat image).

There have been no eruptions at Toba in historical time. Toba is located near the Sumatra Fracture Zone. I have marked this fracture zone as “Fault Zone” on the landsat image, where it is clearly visible as a light line. On the map it is marked by _._._. The movement directions are shown by arrows. Stratovolcanoes in Sumatra are part of the Sunda arc. Volcanism is the result of the subduction of the Indian Ocean plate under the Sunda plate. The subduction zone is marked by the Java Trench. The geologic symbol for a subduction zone is a line with "teeth" (black triangles). The teeth are on the over-riding plate. The rate of subduction is 6.7 cm per year.




A Tale of Two Shetlands

Where is the Shetland Plate?

When I hear or read about Shetland I think of a group of islands somewhere north of Scotland. Technically speaking they are Danish - although Denmark does nothing to claim them. A fascinating side of Shetland and Orkney's history that makes it completely unique in the world is the 1468/69 pawning of the islands by King Christian of Denmark to King James III of Scotland. King Christian had agreed to provide a 60,000 florins dowry on the occasion of the marriage of his daughter to the Scots King. When he was unable to come up with the whole amount, his novel solution was to pawn first Orkney, then Shetland to King James. The pawning had no time limit and has never been revoked or legally challenged. Few people know, but the fact has been used lately as argument for more autonomy. (More at the site of the Shetland & Orkney Udal Law group).

These islands are however not drifting on their own private little tectonic plate (yet).

The South Shetland Islands are a group of Antarctic islands, lying about 120 kilometres north of the Antarctic Peninsula. Under the Antarctic Treaty 1959, the Islands' sovereignty is neither recognized nor disputed by the signatories and they are free for use by any signatory for non-military use. The Islands are claimed by Argentina (since 1943) as part of Argentine Antarctica, Tierra del Fuego Province and by Chile (since 1940) as part of Antártica Chilena Province. They have been claimed by the UK since 1908 and are part of British Antarctic Territory since 1962.

The South Shetland Islands is a volcanic arc, and formed part of the Andean-West Antarctic subducting-plate margin in late Jurassic to Miocene times. Later the islands began to drift away from Antarctica. Continental crust is underlying the South Shetland Islands. Tectonic uplift due to the subduction in the western Antarctic trench system make the South Shetland Islands a rapidly rising island arc.

As seen on the fragment below from a map produced by USGS the South Shetland Islands are situated on a small crustal plate - the Shetland (Island) Plate.





Danish Blue

Hopefully you associate “Danish Blue” with delicious Danish cheese - a bit in the style of Roquefort and Stilton. This post is, however, about a parrot, bereft of life.

In the journal Palaeontology of May 2008 Waterhouse et al. describe two fossil parrots found in Denmark. They are so far the oldest fossil parrots, the most northerly found fossil parrots and one of them is the largest fossil parrot yet known. In fact all that remains of this early Danish parrot is a single upper wing bone (humerus). But, this small bone contains characteristic features that show that it is clearly from a member of the parrot family, about the size of a Yellow-crested Cockatoo. The bone, which is 6.5 cm long, was found on the island Mors in 2003, it is on display in a museum on Mors, the Molermuseum, and has now been determined by a team of palaeontologists. Image of bone in this Danish Article. With the present day climate there are no wild parrots (Psittacidae) in Denmark (although a small population of parakeets has established itself recently). Today parrots only live in the tropics and the southern hemisphere.

The new species, officially named 'Mopsitta tanta', has got the nick-name 'Danish Blue Parrot,' derived from a famous comedy sketch about a 'Norwegian Blue Parrot' in the 1970s BBC television programme 'Monty Python.' The Scandinavian connection makes links to Monty Python's notoriously demised bird irresistible, but the parallels go further. The famous sketch revolves around establishing that a bird purchased by John Cleese is a dead parrot, and these fossils are certainly dead.
The scientifique name Mopsitta tanta is derived from mo after moler (see below), psitta and tanta are latin for respectively 'parrot' and 'large' - the large ‘mo clay’ parrot. When Mopsitta was alive, which was only 10 million years after the dinosaurs were wiped out, most of Northern Europe was experiencing a warm period, with a large shallow tropical lagoon covering much of Germany, South East England and Denmark. (See map. Green = land, white = sea, All of the present Denmark was covered by sea). Denmark was closer to the equator at that time, and the poles were not covered with ice as now.

The fossils were found in a sort of diatomite, locally called moler, meaning whitish clay. Moler consists of cirka 45-65 % silica and silica shells of algae (diatoms - see image below of modern marine diatoms under microscope), 30-45 % clay and 10 % volcanic ashes. The sea bottom was depleted of oxygen, and the thick moler deposits are rich in fossils, including fossils of some 30 different bird species. Most of these would together with flying insects, also fossilised, have flown in from the exposed land areas in what is now Norway and Sweden.

The Danish moler deposit is up to 60 m thick. In other parts of the world there are no known deposits above 10 m thick.

Apart from the Molermuseum on Mors there is another interesting little geological museum on the island of fur, with fossils found in the local moler cliffs.

Reference:
Waterhouse et al.
Two New Parrots (Psittaciformes) From the Lower Eocene Fur Formation of Denmark
Palaeontology, Volume 51 Issue 3 Page 575-582, May 2008

English links
http://www.blackwell-synergy.com/doi/abs/10.1111/j.1475-4983.2008.00777.x
http://www.ucd.ie/news/2008/05MAY08/150508_parrot.html
http://www.sciencecentric.com/news/08051531.htm
http://www.mirror.co.uk/news/topstories/2008/05/16/video-monty-python-s-norwegian-blue-parrot-did-exist-89520-20419112/
http://www.dailymail.co.uk/pages/live/articles/news/news.html?in_article_id=566600&in_page_id=1770

Danish links
http://politiken.dk/videnskab/article509541.ece
http://www.dr.dk/Nyheder/Indland/2008/05/15/220046.htm?rss=true
http://ing.dk/artikel/88153?rss
http://stenfugle.blogs.ku.dk/
http://geologi.snm.ku.dk/nyheder_gm/nyhed160508/
http://nyhederne.tv2.dk/article.php/id-11591242.html?ss




Journal of Flood Risk Management

A new Journal has seen the light. The first issue of Journal of Flood Risk Management, a new publication for 2008, published jointly with the Chartered Institution of Water and Environmental Management (CIWEM) and Wiley-Blackwell is just (in the library and) on line.

With the recent cyclone flooding Myanmar in mind, that affected between 1.6 million and 2.5 million people with estimated death tolls that range from 68,833 and 127,990, the timing seems appropriate. With the way the military regime handles the situation, I fear that more deaths will follow from famine and disease. No doubt Myanmar is on the brink of a public health catastrophe.

Articles published in Journal of Flood Risk Management will be freely available to download in 2008. If interested click on this link to view articles from the first issue.



Mangrove as Flood Protection

No doubt large-scale destruction of protective mangroves along the coasts of Myanmar aggravated the devastation wreaked by the tropical cyclone Nargis. Mangrove provide significant flood protection in low coastal areas, but never the less Mangrove forests are one of the world’s most threatened tropical ecosystems. In January 2008, the UN Food and Agriculture Organization warned that Asia is fast losing its coastal mangroves, with more than 1.9 million hectares being destroyed each year. Mangroves are only suitable for planting on coastal mud-flats and lagoons, but such mud-flats and lagoons cover about 25% of the continental coastline of the Bay of Bengal.

The protective benefits were clearly demonstrated when the Boxing Day Tsunami on 26 December 2004 flooded the coasts of the Indian Ocean. In regions with lesser tsunami intensity areas with coastal tree vegetation were markedly less damaged than areas without. A study published in Science of 28 October 2005 titled The Asian Tsunami: A Protective Role for Coastal Vegetation describe how Cuddalore District in Tamil Nadu, India, provided a unique experimental setting to test the benefits of coastal tree vegetation in reducing coastal destruction by tsunamis (and other flooding events). Cuddalore has a relatively straight shoreline, a fairly uniform beach profile, and a homogenous continental slope. Moreover, the shoreline comprises vegetated as well as non-vegetated areas and was documented by cloud-free pre- and post-tsunami satellite images.

Salt-marshes, mangroves and other forested wetlands act as the front-line defence against incoming storms. They help minimise the impact of storms by reducing wind action, wave action and currents, while the roots of the plants help to hold the sediment in place. The Government of Bangladesh has invested considerable sums of money in re-planting mangroves in previously storm flooded areas to assist in storm protection.

Mangroves are also important for fisheries. Furthermore I must confess that I have had some of my best bird watching experiences in mangrove areas, which may though be of less economic importance.

Predicted effects of climate change over the next 50-100 years will place both coastal and inland wetlands in some parts of the world under a great deal of pressure through increased prevalence of tropical storms, changing patterns of precipitation, and sea level rise.



China Earthquake

,

The most powerful earthquake to hit China in 30 years has killed at least 10,000 people in south-western Sichuan province, with thousands more trapped. The figures are expected to rise dramatically

The M 7.9 strong earthquake was shallow, with a depth of only 10 km, and hit less than 100 km north-east of Chengdu, a city of about 11 million inhabitants. The quake devastated a region of small cities and towns set amid steep hills. The epicentre was relatively far from any plate boundary, but earthquakes in this area are not unknown as can be seen from this USGS map of earthquakes from 1990 to present. Since 1900 the area of this map has known 8 earthquakes larger than M 7.

Kim at All of my Faults are Stress-related has an exellent post on the Tectonics of the May 12 Sichuan earthquake which explains the tectonic situation much better than I would ever be able to, so please go and read it.

The Eastern Sichuan quake ruptured about 275 kilometers of a fault running northeastward between the easternmost mountains of the Tibetan Plateau and the densely populated Sichuan Basin. The violent quake is probably linked to a shift of the Tibetan plateau to the north and east. Earthquakes are frequent and deadly along the fringes of the Tibetan plateau, which was raised when India collided into Eurasia, starting some 50 million years ago.

http://sciencenow.sciencemag.org/cgi/content/full/2008/512/1?rss=1
http://www.abc.net.au/science/articles/2008/05/13/2243183.htm



PS:
A strong aftershock measuring 6.1 on the Richter scale rocked Chengdu itself around 3:10 p.m. Tuesday 13 May 2008. The region has suffered more than 1,950 aftershocks in the past 25 hours, including three over 6 on the Richter scale and 14 between 5 and 6. Heavy rainfall, storm and wrecked roads hamper rescuers' efforts to reach the hardest-hit areas.

PS of 14 may 2008
More about the earthquake including information (and Tectonic Summary) as Reported by USGS at Geology.com




Sahara - from Green to Desert

, ,

Around 14,800 years ago, a strengthening of the summer monsoons - moist tropical Atlantic monsoons from south-west - led to a dramatic climatic change in North Africa and created a “green Sahara”. How did this North African humid period come to an end and lead to the the world’s largest warm desert today. Was it abruptly or gradually?

The drying of the Sahara in the Holocene, that is approximately the last 11,550 years, is widely believed to have been an abrupt event, completed within a few hundred years, but new research published in Science of 9 may 2008 indicates that it happened gradually over the last 6000 years.

The authors of Climate-Driven Ecosystem Succession in the Sahara: The Past 6000 Years studied a sediment record from Lake Yoa in northern Chad. Lake Yoa is one of the very few Saharan lakes in which sediments have accumulated without a break during the Holocene. Despite its extremely arid location, the lake is fed by ancient groundwater and therefore does not dry up.

The vegetation history of the surroundings is reconstructed from pollen. The reconstructed salinity values provide a record of changing precipitation. The input of atmospheric dust to the lake reflects wind regimes and the extent of vegetation cover in the surrounding landscape. The results show that vegetation and dust flux changed gradually over the past 6000 years, accompanied by the slowly weakening monsoon. The pollen source area implies that average north-easterly wind strength must have increased during this time, either because wintertime trade-wind circulation intensified or because a change in the mean position of the Libyan high-pressure cell now channeled low-level northeasterly flow more effectively through the Tibesti-Ennedi corridor.

Tibesti Mountains is a volcanic region to the west of Lake Yoa and the Ennedi Plateau, which is located to the east of the lake, is a sandstone plateau surrounded on all sides by sands, that encroach the deep valleys of the Ennedi.

However fast the drying occurred, it pushed people out of north-central Africa, and that climatically forced migrations might have led to the rise of the pharaohs and Egyptian civilization.

According to the lead author there are now signs of a tiny shift back towards greener conditions in parts of the Sahara, apparently because of global warming.

* http://www.sciencemag.org/cgi/content/short/320/5877/752
* http://sciencenow.sciencemag.org/cgi/content/full/2008/508/2?rss=1
* http://www.abc.net.au/science/articles/2008/05/09/2240138.htm
* http://www.nytimes.com/2008/05/09/science/09sahara.html?_r=1&partner=rssnyt&emc=rss&oref=slogin
* http://www.iht.com/articles/2008/05/09/africa/09saha.php
* http://www.redorbit.com/news/science/1378928/sands_of_sahara_moved_slowly/index.html?source=r_science



Tornadoes

,

Today 9 May 2008 on CNN: Reported twister tears through central North Carolina

About 80 % of tornadoes in the world happen in the United States. They have however been observed on every continent except Antarctica. (Including my part of the world, where they are fortunately seldom). A Tornado is usually defined as a violently rotating column of air which is in contact with both the surface of the earth and a cloud.

The US tornadoes occur when cool Canadian air mixes with warm moist air coming from the Gulf of Mexico, and most of them in the so-called tornado alley (see map). April is, normally, the tornado season.

The south-eastern and Midwestern United States (or something like a quarter of the area of US) were hit by a record-breaking series of over 400 tornadoes within a ten-day period in May 2004. The damage ran into many millions of $, and 42 people died.

The Tornado Project discloses The Terrific, Timeless and Sometimes Trivial Truths about Those Terrifying Twirling Twisters!


Norwesters in Bangladesh

,

Over 30 people have been killed this month and hundreds more injured as ‘norwesters’, wreaked havoc across Bangladesh.

Nor'wester thunderstorms, locally known as Kal-baishakhi, often blow over Bangladesh in April-May from a northwesterly direction. Nor'wester thunderstorm coincides with the setting in of the summer season. From mid-March to April the temperature in Bangladesh rises sharply compared to the preceding months (i.e. winter months). In the middle of April the whole country, especially the northwestern part, records a sharp rise in day temperature. Presence of warm and moist air in the lower layer of the atmosphere is an essential precondition for the development of a nor'wester.

The main reasons behind the nor'wester is the warm and moist air coming from the southeast which rises up to 2 kilometres, mixes with the relatively cold and dry jet streams coming from the northwesterly and westerly directions. The mixing of these two dissimilar air masses causes storms. The warm and moist air rises due to the Chotanagpur Plateau, Himalayan ranges, and Assam Plateau. Thunder and lightning is common with a nor'wester. Nor'westers are more frequent in the late afternoon because of the influence of surface heating in producing convection currents in the atmosphere. In the western region of Bangladesh, nor'westers come in the late afternoon and before evening but in the eastern side it comes generally after evening, moving from a northwesterly to a easterly and southeasterly direction. In this season the morning remains calm. Temperature begins to rise from noon creating a convective current and the storm is formed. The average wind speed of a nor'wester is 40-60 km per hour. But in exceptional circumstances the wind speed may exceed 100 km. The duration of the storm is generally less than an hour but sometimes it may exceed an hour.

Much of the country’s rural population lives in huts made of corrugated iron or mud and straw which are ill-equipped to withstand winds powerful enough to uproot trees and knock down electricity pylons.

Norwesters may also strike later in November. Given their ferocity and destructive capacity `norwesters’ are also referred to as tornadoes. For nearly 60 days during the two storm seasons, locally generated storms have hit various parts of the country almost on a daily basis. So far there is no effective early warning system for these storms. They are so local in nature and take shape so suddenly that modern tracking devices can only locate them when they begin to move, at times with a whirling speed of 200 km.

In Dhaka, trees were uprooted and thatched roofs blown away after a powerful storm struck the capital on 2 May 2008. The storms are so frequent in number and so destructive in nature that the total damage done by them is perhaps only second to the damage caused by the annual floods. In terms of damage to life and property, they do more than the floods.

Norwesters often strike when the country’s ‘boro’ crop - the country’s main rice harvest - is ready for harvest, and jute, a major cash crop for the impoverished nation, is at a critical stage of growth. According to the department of meteorology, 30-50 percent of standing crops are damaged in areas where ‘norwesters’ hit.

The crop loss could be minimised or even avoided if the pattern of cultivation is changed, either by planting the crops two to three weeks earlier than now, or by shortening the harvesting season. Most of those who die, die indoors, crushed under mud walls or hit by flying tin roofs - the construction of disaster-resilient houses could save thousands of lives lost under falling roofs and walls.

http://www.irinnews.org/report.aspx?ReportId=78089
http://banglapedia.search.com.bd/HT/N_0208.htm



Baltic Sea Ice

As a long-term average the Baltic Sea is ice covered for about 45% of its surface area at maximum annually. The ice-covered area during such a typical winter includes the Gulf of Bothnia, the Gulf of Finland, Gulf of Riga and Väinameri in the Estonian archipelago. The remainder of the Baltic itself does not freeze during a normal winter, with the exception of sheltered bays and shallow lagoons such as the Curonian Lagoon. The ice reaches its maximum extent in February or March; typical ice thickness in the northernmost areas in the Bothnian Bay, the northern basin of the Gulf of Bothnia, is about 70 cm for landfast sea ice. The thickness decreases further south.


Freezing begins in the northern coast of Gulf of Bothnia typically in middle of November, reaching the open waters of Bothnian Bay in early January. The Bothnian Sea, the basin south of it, freezes on average in late February. The Gulf of Finland and the Gulf of Riga freeze typically in late January.

The ice extent depends on whether the winter is mild, moderate or severe. Severe winters can lead to ice formation around Denmark and southern Sweden, and on rare occasions the whole sea is frozen, such as in 1942 and 1966. In 1987, some 96% of the Baltic Sea was ice-covered, leaving only a small patch of open water in the south-west around Bornholm. However, in milder winters only restricted parts of the Bay of Bothnia and Gulf of Finland are ice covered, in addition to coastal fringes in more southerly locations such as the Gulf of Riga. In recent years a typical winter produces only ice in the northern and eastern extremities of the Sea. In 2007 there was almost no ice formation except for a short period in March.
From Wikipedia.

The extent of ice covering the Baltic sea this winter (2007/2008) reached an all-time low. New figures from Sweden's meteorological agency (SMHI) indicate the lowest levels since measurements began more than a century ago. Overall, 49,000 km2 of the Baltic sea were covered in ice compared to the usual 180,000 km2. That was just over a quarter of the normal level, and the ice season had ended two weeks early. The highest levels of ice cover in the Baltic came in the winter of 1986 and 1987 when 420,000 km2 of its waters were covered.

The ringed seal had to change its usual habits and give birth much closer to land.

I would like to stress than one warm winter in a local area like the Baltic Sea proves nothing about global warming. Global warming is about a trend in climate change over many years. At the same time I would like to stress that Americans should NOT take their cold winter that same winter 2007/2008 as a sign that this global warming trend has suddenly stopped.

http://www.thelocal.se/11526/20080503/
http://www.terradaily.com/reports/Baltic_sea_ice_cover_hits_an_all-time_low_meteorologists_999.html

More in Swedish from SMHI at
http://www.smhi.se/cmp/jsp/polopoly.jsp?d=103&a=34774&l=sv



May 2008
MTWTFSS
April 2008June 2008
1234
567891011
12131415161718
19202122232425
262728293031