Saturday, 12 November 2016

Magnitude 5.8 Earthquake on the east coast of Miyagi Prefecture, Japan.

The Japan Meteorological Agency recorded a Magnitude 5.8 Earthquake at a depth of about 60 km, on the coast of the Miyagi Peninsula on Honshū Island, slightly before 6.45 am on Saturday 12 November 2016 Japan Standard Time (slightly before 9.45 pm on Friday 11 November GMT). There are no reports of any damage or casualties associated with this event, people have reported feeling it across most of northern and eastern Honshū.

  Map showing the location of the 12 November 2016 Miyagi Prefecture Earthquake, and areas where the event was felt. Japan Meteorological Agency.

Japan has a complex tectonic situation, with parts of the country on four different tectonic plates. Eastern Honshū area lies on the boundary between the Pacific, Eurasian and Philipine Plates, where the Pacific Plate is passing beneath the Eurasian and Philipine Plates as it is subducted into the Earth. This is not a smooth process; the rocks of the two plates constantly stick together, only to break apart again as the pressure builds up, causing Earthquakes in the process. 
 
 The movement of the Pacific and Philippine Plates beneath eastern Honshū. Laurent Jolivet/Institut des Sciences de la Terre d'Orléans/Sciences de la Terre et de l'Environnement.
 
Witness accounts of Earthquakes can help geologists to understand these events, and the structures that cause them. The international non-profit organization Earthquake Report is interested in hearing from people who may have felt this event; if you felt this quake then you can report it to Earthquake Report here.
 
See also...

http://sciencythoughts.blogspot.co.uk/2016/10/magnitude-66-earthquake-in-tottori.htmlhttp://sciencythoughts.blogspot.co.uk/2016/08/magnitude-42-earthquake-in-chiba.html
http://sciencythoughts.blogspot.co.uk/2015/06/japan-restricts-access-to-mount-hakone.htmlhttp://sciencythoughts.blogspot.co.uk/2015/05/alert-level-around-mount-hakone-raised.html
http://sciencythoughts.blogspot.co.uk/2015/02/magnitude-57-earthquake-off-east-coast.htmlhttp://sciencythoughts.blogspot.co.uk/2014/11/magnitude-68-earthquake-in-nagano.html

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Apartment blocks evacuated after sinkhole opens up in Ephrata, Pennsylvania.

Two apartment blocks have been evacuated after a sinkhole opened close to them in the city of Ephrata in Lancaster County, Pennsylvania, on Tuesday 8 November 2016. The hole was initially reported as a small pothole at about 5.00 pm local time, but rapidly grew to be about 15 m wide and about 6 m deep, triggering the evacuations of the nearby apartments. A total of 19 residents of 12 apartments are said to have been effected, some of whom are believed to be elderly.

The site of the November 2016 Ephrata sinkhole. Ephrata Police Department.

Sinkholes are generally caused by water eroding soft limestone or unconsolidated deposits from beneath, causing a hole that works its way upwards and eventually opening spectacularly at the surface. Where there are unconsolidated deposits at the surface they can infill from the sides, apparently swallowing objects at the surface, including people, without trace.

In this case the sinkhole is thought to have been caused by a burst water main, which washed away lose sediments beneath the road, undermining the structure and causing the surface to collapse. Around 1 136 000 litres of water are thought to have been lost due to this event, which will have cost the borough about US$900, though the cost of the repairs is likely to be far higher possibly exceeding US$1 million.

See also...

http://sciencythoughts.blogspot.co.uk/2016/06/flooding-kills-26-in-west-virginia.html
http://sciencythoughts.blogspot.co.uk/2016/02/truck-swallowed-by-sinkhole-in.html
http://sciencythoughts.blogspot.co.uk/2015/03/three-homes-evacuated-after-giant.htmlhttp://sciencythoughts.blogspot.co.uk/2015/03/one-dead-and-two-injured-following-roof.html
http://sciencythoughts.blogspot.co.uk/2015/02/snow-plow-swallowed-by-sinkhole-in-new.htmlhttp://sciencythoughts.blogspot.co.uk/2014/07/five-family-members-injured-by-falling.html

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Myanmar jade mine struck by possible space debris.

Residents of Lone Khin near Hpakant in Kachin State, Myanmar, were alarmed by a mysterious object which fell from the sky on Thursday 10 November 2016. The object is described as being a metal cylinder 3.7 m in length and 1.2 m in diameter, with protruding wires and Chinese writing on the outside. After striking the ground a first time the object bounced about 50 m before coming to rest in an open area at a jade mine (Myanmar is the world's largest producer of jade). A second smaller piece of debris is reported to have damaged a nearby house, though nobody was injured by either event.

The object which fell from the sky onto a Myanmar jade mine on 10 November 2016. Yanniang Pyi Sone Aung.

The object was initially thought to be a piece of an aircraft engine, but has now been linked to the launch of an experimental X-ray pulsar navigation spacecraft, the Maichong Xing Shiyan Weixing (which is intended to test the theory that radio emissions from pulsars could be used to navigate spacecraft) on a Long March Rocket 11from the Jiuquan Satellite Launch Center in Inner Mongolia, China, earlier that day. These rockets comprise a series of booster stages that are jettisoned as the craft rises through the atmosphere. As with similar rockets launched by other nations, these jettisoned stages are intended to fall back to Earth over open water or sparsely populated regions (the Jiuquan Satellite Launch Center is in the Gobi Desert), though the possibility of one being blown to a different area by high winds does exist.

See also...

http://sciencythoughts.blogspot.co.uk/2015/12/landslide-kills-at-least-five-at-mine.html
http://sciencythoughts.blogspot.co.uk/2016/05/landslide-at-myanmar-jade-mine-kills-at.html


http://sciencythoughts.blogspot.co.uk/2015/11/hundreds-feared-dead-following.html


http://sciencythoughts.blogspot.co.uk/2015/01/at-least-two-dead-following-landslide.htmlhttps://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEibp8rLFzIwzrqY9DcMsHGSYT5TwbLq3LJOPpRI_feY2-1kHiKyTGGZVnK77kkNRgMwhpqsZBeBzDZFytm2hi2T7t3DHqF3JdTBum8tkziCaAIH9LYiQwA7zAo-O3QKXrSO2Z35F8e3XE4/s1600/Jade+Mine.jpg

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Friday, 11 November 2016

Seven homes evacuated after sinkhole opens in Ripon, North Yorkshire.

Seven homes have been evacuated after a sinkhole opened in gardens behind them in Ripon in North Yorkshire, England, on Wednesday 9 November 2016. The hole, which measures approximately 20 m by 10 m and is thought to be about 9 m deep was reported to the North Yorkshire Fire Brigade after residents felt the ground moving and investigated. Nobody has been injured due to this incident, but the homes have been evacuated as a precaution, while engineers attempt to make the houses structurally secure.

The scene of the November 2016 Ripon sinkhole. BBC.

Sinkholes are generally caused by water eroding soft limestone or unconsolidated deposits from beneath, causing a hole that works its way upwards and eventually opening spectacularly at the surface. Where there are unconsolidated deposits at the surface they can infill from the sides, apparently swallowing objects at the surface, including people, without trace.

Ripon is prone to sinkholes due to sinkholes due to Permian gypsum deposits which underlie much of the area. It is an evaporate rock, a form of calcium sulphate deposited as mineral-rich water evaporates, often around sulphurous hot springs or volcanic systems. Gypsum is a very soft rock, and soluble in water, so moisture entering gypsum deposits can cause major collapses and subsidence.

See also...

http://sciencythoughts.blogspot.co.uk/2016/05/magnitude-13-earthquake-in-cumbria.htmlhttp://sciencythoughts.blogspot.co.uk/2016/06/explosion-kills-miner-at-yorkshire.html
http://sciencythoughts.blogspot.co.uk/2015/11/magnitude-13-earthquake-in-county.htmlhttp://sciencythoughts.blogspot.co.uk/2015/12/magnitude-11-earthquake-in-cumbria.html
http://sciencythoughts.blogspot.co.uk/2015/06/magnitude-18-earthquake-in-south.htmlhttp://sciencythoughts.blogspot.co.uk/2015/07/magnitude-16-earthquake-in-cumbria.html
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Tuesday, 8 November 2016

Magnitude 5.0 Earthquake in Payne County, Oklahoma.

The United States Geological Survey recorded a Magnitude 5.0 Earthquake at a depth of 5.0 km about 2 km to the west of the city of Cushing in Payne County, Oklahoma, slightly before 7.45 pm local time on Sunday 6 November 2016 (slightly before 1.45 am on Monday 7 December GMT). No fatalities or major damage have been reported, but a number of minor injuries and damaged buildings have been reported in the Cushing area, and people have reported feeling the event across much of Oklahoma as well as parts of Kansas, Missouri, Arkansas and Texas.

Damage in Cushing, Oklahoma, following the 6 November 2016 Earthquake. AN24.

Oklahoma is naturally prone to Earthquakes, particularly in the southwest of the state, near the Meers Fault Zone, but since 2009 has suffered a sharp increase in the number of small quakes in the central and northeast parts of the state. While most of these quakes have been quite small, a few have been large enough to potentially cause problems, and any unexplained increase in seismic activity is a cause for concern.

In a paper published in the journal Geology on 26 March 2013, a team of geologists led by Katie Keranen of the ConocoPhillips School of Geology and Geophysics at the University of Oklahoma linked one of the largest of these quakes, a Magnitude 5.7 event in November 2011 which caused damage locally and was felt across 17 states, to the practice of pumping liquids (usually brine) into injection wells, which is common in the hydrocarbons industry and used to displace oil or gas, which can then be extracted from nearby extraction wells (where this is done in bursts at pressure to intentionally break up rock it is called hydraulic fracturing, or fracking). Significantly they suggested that the practice could lead to quakes years or even decades after the actual injection.

Witness accounts of quakes can help geologists to understand these events and the rock structures that cause them. If you felt this quake (or if you were in the area but did not, which is also useful information) you can report it to the USGS here.

See also...










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Wednesday, 2 November 2016

Series of controlled explosions carried out at UK schools.

A series of controlled explosions have been carried out by bomb disposal experts at schools in England and Wales over the past 24 hours after concerns were raised about the storage of a potentially explosive chemical, 2,4-­‐dinitrophenylhydrazine (or Brady's Reagent), which is used in some A-level experiments. The chemical is both flammable and an oxidising agent, and can become an explosive under some circumstances if not stored correctly, which has resulted in advice from the Department for Education to destroy any unsafely stored chemical on-site rather than risk transporting it for disposal.

The structure of 2,4-­‐dinitrophenylhydrazine. Wikimedia Commons.

2,4-­‐dinitrophenylhydrazine is only dangerous when dry, and for this reason CLEAPSS (The body which provides advice on laboratory safety to UK schools) advises that the substance be stored wet, inside a container which is placed within an outer container that also contains water. Schools are currently being asked to check the storage of any 2,4-­‐dinitrophenylhydrazine they hold and to contact CLEAPSS for advice if the outer container is dry, and under no circumstances to attempt to open an improperly stored container (2,4-­‐dinitrophenylhydrazine is a friction explosive, and any dry dust caught in a screw top could potentially ignite like a match).

A number of residents living in areas close to schools have complained about explosions being carried out without warning. More seriously, concerns have been raised that these incidents may reflect lowering safety standards in UK schools as part of the government's academies program, which aims to give schools more autonomy and control over areas such as budgets and syllabuses. Services provided by CLEAPSS were formerly provided free to all schools, but now have to be purchased in, and it is not clear what proportion of schools are now doing this (although advice on 2,4-­‐dinitrophenylhydrazine is currently available to all schools for free on the CLEAPSS website), At the same time concerns have been raised that many schools with leadership drawn from outside the science sphere may be cutting back on support in science departments, lowering the pool of available advice in areas such as chemical storage.

See also...

http://sciencythoughts.blogspot.co.uk/2016/10/selenium-arsenic-and-molybdenum-in.htmlhttp://sciencythoughts.blogspot.co.uk/2016/09/workers-rescued-after-chemical-incident.html
http://sciencythoughts.blogspot.co.uk/2016/08/passers-by-forced-to-undergo.html
http://sciencythoughts.blogspot.co.uk/2016/01/chemical-spill-at-scottish-school-puts.htmlhttp://sciencythoughts.blogspot.co.uk/2015/12/widespread-lead-poisonng-prompts-city.html
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Tuesday, 1 November 2016

Evidence of heat-treatment during the manufacture of silcrete artefacts at Klipdrift Shelter 64 600 years ago.

Heat-treatment can significantly change the physical properties of a number of types of rock, enabling the manufacture of stone tools of a higher quality than would otherwise be possible from the same material. The discovery of this by early humans is considered a significant cultural breakthrough for stone age societies, representing one of the first known instances of the intentional transformation of materials for technological reasons in the archaeological record. This breakthrough appears to have been made independently on a number of occasions around the world in the Late Pleistocene and Early Holocene, with the earliest known occurrences being at Pinnacle Point and Blombos Cave in South Africa, where the technology first appears about 70 000 years ago. In Southern Africa this technology is associated with the advanced Middle Stone Age Still Bay and Howiesons Poort cultures, both of which are known to have made extensive use of fire, which flourished 71 900-70 000 years ago (Still Bay Culture) and between about 65 800 and 59 500 years ago (Howiesons Poort Culture) respectively, then apparently disappeared and were replaced by less advanced cultures. However while individual stone tools with signs of heat-treatment have been identified, establishing how widespread and systematic this approach to tool-making was is much harder, leaving open the possibility that some heat-treated tools may have been made opportunistically from stones that had not been heated with the specific intention of later making tools.

In a paper published in the journal PLoS One on 19 October 2016, a team of scientists led by Anne Delagnes of the University of Bordeaux and the School of Geography, Archaeology and Environmental Studies and Evolutionary Studies Institute at the University of the Witwatersrand, attempt to address this problem by analysing tools from the 64 600-year-old PDB layer at the Klipdrift Shelter palaeoarchaeological site on the Indian Ocean shoreline in the De Hoop Nature Reserve in the southern Cape region.

The Klipdrift Shelter has produced a series of layers about 120 cm thick, containing well preserved archaeological assemblages, including marine and terrestrial faunal remains, organic materials, lithics (stone tools), ochre and engraved ostrich eggshells, dating from about 70 000 to about 50 000 years ago. The layer PDB layer has been dated to 64 600 years ago (plus or minus 4200 years) and is noted for a particularly rich lithic assemblage, with about 2500 stone tools recovered from an exposed surface of about four square meters. These artefacts are considered to be of the intermediate Howiesons Poort technology phase, with a large number of notched tools and a predominance of silcrete items. Of the knapped tools from this layer 46% were found to be made of silcrete, 35.4% of quartzite, 17.1% of hydrothermal quartze and 1.5% of chert or calcrete.

Map of the excavated area at KDS and site stratigraphy with OSL dates. Magnus Haaland in Delagnes et al. (2016).
 
Heat-treated can be used to modify a variety of rocks for making stone tools, most notably flint (chert) and silcrete. However the temperatures needed for heat-treatment of flint are far higher than those needed for heat-treatment of flint, and only heat-treated silcrete tools have been found at Pleistocene South African Sites. Silcrete is a highly variable rock, and the effects of heat-treatment upon it are also variable, which makes it difficult to simply pick up a piece of silcrete and say 'this has been heat-treated'. Typically when heat-treated silcrete becomes more brittle, loses porosity, is reddened and may fracture. However without knowing the original properties of a piece of silcrete it is difficult to assess whether it has been heat-treated.

Silcrete is not naturally occurring at the Klipdrift Shelter, rather it outcrops at a number of sites in the Cape Fold Mountains about 10 km to the north of the site. In order to assess whether the silcrete tools of layer PDB had been treated with fire, Delagnes et al. collected a series of comparison samples from these sites. These samples were not thought to necessarily match the outcrops which produced the material for the stone tool production, but were chosen for similarities in lithological properties (grain size, mineral composition etc.).

 Map of the KDS area showing the six sampling locations for our reference collection. The black spots correspond to primary silcrete and ferricrete outcrops georeferenced by Roberts (2003). The red x of source 5 indicates that this outcrop was not georeferenced by Roberts. Gauthier Devilder in Delagnes et al. (2016).

By comparing silcrete artefacts from layer PDB to both heat-treated and non heat-treated samples from this reference collection, Delagnes et al. were able to ascertain that 92% of these objects showed signs of heat-treatment prior to manufacture, while of the remaining items the majority were impossible to assess (primarily due to exposure to fire after their manufacture, probably as a result of being discarded in places where fires were subsequently built), while only 1.5% of the items were identified as having been manufactured without the use of fire.


 Heated blades and tools on blades from Klipdrift Shelter, layer PBD. (1)-(16): Silcrete blades showing their diversity in terms of size attributes and visual transformations after heating, (17)-(19): Backed tools including one fragment of backed tool (17), one bi-truncated tool (18), one segment (19); (20), (21): Notched blades; (22), (23): Blades with slight continuous retouch on one lateral edge. Delagnes et al. (2016).

However, simple heat-treatment prior to production does not appear to have been the entire story of the manufacture of stone tools at Klipdrift Shelter. Around 25% of the tools show signs of having been worked both before and after heating, suggesting that the heat-treatment was part of an extended manufacturing process rather than a simple pre-treament. Furthermore about 7% of the items show signs of heat-induced fracturing, which does not appear to have been a catastrophe to the tool-makers, since they were able to work these incidental surfaces into their eventual design rather than being forced to abandon the objects.

Heated blade cores from layer PBD, Klipdrift Shelter. Caption for drawings: (1) Knapping platform preparation, (2) convexity preparation, (3) blade removal without initiation, (4) blade removal with initiation, (5) indeterminate removal, (6) cortex, (7) preheating surface, (8) heat-induced non-conchoidal fracture (HINC), (9) post-heating removal. Note that all three cores (A, B, C) show a sequence of core exploitation (preparation and blade production) that follows a heat treatment which has resulted for A and C in heat-induced fractures, and which was preceded for A and B by a first stage of core exploitation. Delagnes et al. (2016).

Delagnes et al. further reason that it is likely that a higher proportion of blocks underwent heat-induced fracturing during preparation, as in many cases reworking may have subsequently removed all traces of the heat fractured surface. With this in mind they reason that the deliberate heat-fracturing of material may even have been part of the manufacturing process. Such fractures tend to occur along plains where there are pre-existing (but invisible) weaknesses in the rock, such as those caused by iron oxide or hydroxide concentrations (which produce water vapour when heated, fracturing the rock), preventing wastage and accidents later in the manufacturing process. Such deliberate heat-fracturing of rocks has been recorded among modern stone tool-makers in North America, the Andaman Islands and Zimbabwe, and is believed to have been used by the tool-makers of the Sauveterrian culture of the French Mesolithic (8500-7500 years ago).

See also...

http://sciencythoughts.blogspot.co.uk/2015/08/evidence-of-cereal-cultivation-by-sea.htmlhttp://sciencythoughts.blogspot.co.uk/2016/03/middle-palaeolithic-stone-tools-from.html
http://sciencythoughts.blogspot.co.uk/2015/04/late-pleistocene-lithic-artefacts-from.htmlhttp://sciencythoughts.blogspot.co.uk/2014/10/acheulian-and-levallois-technologies.html
http://sciencythoughts.blogspot.co.uk/2014/10/stone-tools-from-middle-to-late.htmlhttp://sciencythoughts.blogspot.co.uk/2013/10/toolmaking-in-northeastern-thar-desert.html
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