History[ edit ] In , iodine was discovered by French chemist Bernard Courtois , [5] [6] who was born to a manufacturer of saltpeter an essential component of gunpowder. At the time of the Napoleonic Wars , saltpeter was in great demand in France. Saltpeter produced from French nitre beds required sodium carbonate , which could be isolated from seaweed collected on the coasts of Normandy and Brittany. To isolate the sodium carbonate, seaweed was burned and the ash washed with water. The remaining waste was destroyed by adding sulfuric acid. Courtois once added excessive sulfuric acid and a cloud of purple vapour rose. He noted that the vapour crystallised on cold surfaces, making dark crystals. They described the substance to a meeting of the Imperial Institute of France.

Cosmogenic Nuclide Dating

Late Neogene passive margin denudation history—cosmogenic isotope measurements from the central Namib desert In this paper, we review ideas on the geomorphological history of the southwest African passive margin, focusing on the central Namib sector and presenting new evidence on the late Neogene landscape evolution of this region. The hyperarid central Namib Desert occupies the — km-wide pediment at the foot of the Great Escarpment and forms part of the southwest African passive margin, which formed after breakup in the South Atlantic at around Ma.

Aridity of the Namib Desert is generally assumed to have started with the onset of Benguela upwelling in the SE Atlantic at 10—15 Ma and to have prevailed ever since. It has been implied that during this period, the landscape has undergone only marginal change. Here, we present new evidence from in situ cosmogenic 21 Ne dating of pediment surfaces, river terraces and river cut bedrock benches.

Correlation of terrace sediment bodies defining ancient river courses is supported by a sediment provenance study using heavy mineral analyses.

Quaternary alluvial fans, and shorelines, spits and beach bars were dated using 10 Be terrestrial cosmogenic nuclide (TCN) surface exposure methods in Death Valley. The 10 Be TCN ages show considerable variance on individual surfaces. Samples collected in the active channels date from ~ 6 ka to ~ 93 ka, showing that there is significant 10 Be TCN inheritance within cobbles and boulders.

Hoke, Q, Xu, W. Sentinel-1 observations of the Menyuan earthquake: Structure and geometry of the Aksay restraining double bend along the Altyn Tagh Fault, northern Tibet, imaged using magnetotelluric method. Geophysical Research Letters, 44, , doi: How complex is the Mw 7. Bulletin of the Seismological Society of America, 2 , doi: Frequency-dependent rupture process, stress change, and seismogenic mechanism of the 25 April Nepal Gorkha Mw 7. Science China Earth Sciences, 60, doi: Li, , Geomorphic offsets along the creeping Laohu Shan2 section of the Haiyuan fault, northern Tibetan Plateau, submitted.

The Larsen C Ice Shelf growing rift

Antarctic Peninsula ice shelves Ice shelf collapse on the Antarctic Peninsula Rifting on Larsen C Impact of calving the large iceberg Sea level rise following ice-shelf collapse References Comments Antarctic Peninsula ice shelves The Antarctic Peninsula is fringed by floating ice shelves. They are floating extensions of the glaciers on land, and receive mass by snowfall and marine freeze-on.

They lose mass by melting at their base and by calving icebergs. Larsen C Ice Shelf, the largest ice shelf on the Antarctic Peninsula, is currently being closely watched.

The total exposure from a to 5 Ma of a given surface of archaeological origin can be determined by surface exposure dating. The range of burial dating is from ~ to 5 Ma.

Lalonde AMS Laboratory at uOttawa Timeline Preparation of accelerator mass spectrometry targets takes a minimum of one week of mineral purification and an additional week to 10 days for target chemistry. In the case of 10Be, 26Al, or 36Cl the chemistry involves ion chromotography and controlled precipitations.

For the 14C extraction from quartz we use a tube furnace and flux to melt the quartz and our custom built ultrahigh vacuum stainless steel extraction line to purify the 14CO2 gas. The wait times for accelerator mass spectrometry can be long months , during which time the required elemental analyses are also completed, either by our in-house ICP-OES or by other instruments off campus. The time for data reduction and initial interpretation ranges from a few hours to a week.

Projects that involve computation with available calculators or the development of new models or theory will take longer. We normally have samples in the quene for all isotopes. For 10Be and 26Al we average about 6 months before starting new samples.

The Larsen C Ice Shelf growing rift

They will therefore sample boulders that are subrounded, faceted, bear striations, or show other signs of subglacial transport. There are about nuclides in nature that have never observed to decay. How can we date rocks?

Cosmogenic nuclide dating uses the interactions between cosmic rays and nuclides in glacially transported boulders or glacially eroded bedrock to provide age estimates for rock at the Earth’s surface. It is an excellent way of directly dating glaciated regions.

What is happening around the Antarctic Peninsula? This is a region of very rapid warming, and this has resulted in a whole suite of glaciological changes. What are the implications of this change for us? How do glaciers respond to climate change, how are they related and linked, and what is driving these changes? This article summarises glaciers and climate change around the Antarctic Peninsula.

Temperatures are rising Figure 2. This image shows the instrumental record of global average w:

Greg Balco

The current version of the portion of this calculator that computes surface exposure ages, which I believe is something like 2. This fairly limited selection of nuclide-mineral options is just because i the Be in-quartz pair is by far the most common exposure-dating technique, and ii Be and Al can be simultaneously extracted from quartz samples with just a little bit more work than just measuring Be , so these two nuclides are commonly both measured. However, there are lots of other nuclide-mineral pairs out there that can be used for exposure-dating.

Cosmogenic exposure dating An age determined by measurement of the amount of each nuclide would be an estimate of the minimum time that the particular surface had been exposed, but would not date the maximum age of the surface exposure, that is, the surface could have been exposed for much longer than the minimum calculated age.

NORM results from activities such as burning coal, making and using fertilisers, oil and gas production. Uranium mining exposes those involved to NORM in the uranium orebody. Radon in homes is one occurrence of NORM which may give rise to concern and action to control it, by ventilation. All minerals and raw materials contain radionuclides of natural origin. The most important for the purposes of radiation protection are the radionuclides in the U and Th decay series.

For most human activities involving minerals and raw materials, the levels of exposure to these radionuclides are not significantly greater than normal background levels and are not of concern for radiation protection. However, certain work activities can give rise to significantly enhanced exposures that may need to be controlled by regulation. Material giving rise to these enhanced exposures has become known as naturally occurring radioactive material NORM.

NORM is the acronym for Naturally Occurring Radioactive Material, which potentially includes all radioactive elements found in the environment. However, the term is used more specifically for all naturally occurring radioactive materials where human activities have increased the potential for exposure compared with the unaltered situation.

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Contributions and unrealized potential contributions of cosmogenic-nuclide exposure dating to glacier chronology, [J]. Quaternary Science Reviews, ,30 Terrestrial in situ cosmogenic nuclides:

Cosmogenic nuclides (or cosmogenic isotopes) are rare nuclides created when a high-energy cosmic ray interacts with the nucleus of an in situ Solar System atom, causing nucleons (protons and neutrons) to be expelled from the atom (see cosmic ray spallation).

Cave and Karst Science, Vol. Transactions of the British Cave Research Asso Transactions of the British Cave Research Association. Terrestrial cosmogenic nuclide 10 Be surface-exposure ages are reported for three glacially-transported gritstone boulders and one glacially-scoured exposure of gritstone bedrock in the vicinity of Stump Cross Caverns, North Yorkshire.

Although the ages do not form a statistically consistent cluster, three of them nevertheless indicate that the transport and deposition of boulders was by ice of the last Late Devensian glaciation. The ages provide evidence for glacier ice at the Wharfe—Nidd interfluve, in contrast to previously held views that these uplands had remained above the level of the last ice sheet. This is consistent both with surface-exposure ages from sites elsewhere around the southern margin of the Yorkshire Dales and with uranium-series dated speleothems in Stump Cross Caverns.

Cave shaft sediments in northwest England associated with the 9. Both the opening of the cave shaft to the surface and its infilling by clastic sediments are attributable to accelerated landscape erosion associated with the 9. Evidence that wild boar had died in winter or spring suggests that their deaths relate to the prolonged periods of annual snow cover experienced by the uplands of northwest England during the 9. The dominance of wild boar in the pit fall assemblage is explained by the snow pack concealing the open shaft and turning it into a baited trap for wild boar whenever it contained carrion.

Wild boar bones splintered and chewed by wild boar demonstrate carrion cannibalism. Human presence is attested by slight butchery to an aurochs Bos primigenius. How Mesolithic people adapted to climate change associated with the 9.

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Video about cosmogenic surface exposure dating: It is an excellent way of directly dating glaciated regions. Wherever we are on Earth, when we are outside, we are constantly bombarded by these cosmic rays.

exposure dating that cosmogenic nuclide dating has proven itself as an effective tool for measuring absolute ages that every quaternary geologist should keep in their analytical arsenal. Emanating from the centre of the Milky Way galaxy is a steady stream of randomly.

Analysis of the long-lived cosmogenic radionuclides 10Be, 26Al and 36Cl provided by the CIAF can be used to determine surface exposure ages and denudation rates on timescales of – years, which yield fundamental information about rates of landscape evolution. Cosmogenic nuclide inventories also contribute fundamental information towards understanding paleoclimates and climate system studies, tracing oceanic circulation, and assessing natural hazards, which tie into the sustainability of local, regional, and global economies.

The establishment of this facility recognises the rapidly growing demand for cosmogenic isotope data from researchers in geomorphology, Quaternary science, and allied areas of the Earth and Environmental Sciences. Detailed coverage of the technical aspects of cosmogenic isotope analysis can be found in: Journal of Quaternary Science 23 5 , A review of geomorphological applications is provided by Cockburn, H. Progress in Physical Geography 28, A useful summary of the major applications of cosmogenic isotopes can be found in a series of articles in a special issue on cosmogenic techniques in the journal Elements, Volume 10 issue 5 October at: Currently there is capability for chemical separation of cosmogenic 10Be and 26Al in quartz, and for cosmogenic 36Cl in calcite or basalt.

Chemical separation for 10Be from minerals other than quartz is being developed. CIAF has an “open-door” policy for all existing and potential users of its facilities at all stages of their research projects, and laboratory visits and collaboration are strongly encouraged.

14–Cosmogenic Radionuclide Geochronology (LIPI Indonesia lectures 2013)