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Schoenbohm, Edward R. Sobel, Peter G. The Pamir is the western continuation of Tibet and the site of some of the highest mountains on Earth, yet comparatively little is known about its crustal and tectonic evolution and erosional history. Both Tibet and the Pamir are characterized by similar terranes and sutures that can be correlated along strike, although the details of such correlations remain controversial. The erosional history of the Pamir with respect to Tibet is significantly different as well: Most of Tibet has been characterized by internal drainage and low erosion rates since the early Cenozoic; in contrast, the Pamir is externally drained and topographically more rugged, and it has a strongly asymmetric drainage pattern. U-Pb ages from rivers draining the northeastern Pamir are Mesozoic to Proterozoic and show affinity with the Songpan-Ganzi terrane of northern Tibet, whereas rivers draining the central and southern Pamir are mainly Mesozoic and show some affinity with the Qiangtang terrane of central Tibet. AFT data show strong Miocene-Pliocene signals at the orogen scale, indicating rapid erosion at the regional scale. Despite localized exhumation of the Mustagh-Ata and Kongur-Shan domes, average erosion rates for the northeastern Pamir are up to one order of magnitude lower than erosion rates recorded by the central and southern Pamir.

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Petroglyphs, a type of carved rock art engraving, were once commanding cultural symbols for the ancient tribes who lived in the Pamir Mountains of Tajikistan. These intricate drawings were chipped away into rocks and stones and used to express everyday life in the mountains. They were carved into low terraces, on burial sites, the walls of fortresses, on riverbanks and lakeshores, in hunting zones, and within the ruins of ancient settlements like the Ratm fortress.

Basically any surface that shone in the sun and could be easily engraved upon was suitable for an ancient petroglyph. Dating back centuries upon centuries, the Pamir petroglyphs often portrayed animal hunting scenes of wild goats, ibex, yaks, and deer as well as everyday routines and important religious ceremonies. The different groups of Pamir Petroglyphs, Tajikistan, are located in different areas and were created at different time periods using ancient tools to whittle away at the natural rock.

The oldest Pamir petroglyphs date back to the Bronze Ages while the more recent are from the early Middle and Modern Ages. You will find some great examples of age-old petroglyphs in the Pamirs and in other areas of Tajikistan; some are more easily reached or better preserved than others. The highest concentration of petroglyphs in Tajikistan can be found in the mountains above the village of Langar in the Ishkashim District.

This is the easternmost settlement in the Western Pamir Plateau and its isolation can be felt. There are over 6, ancient petroglyphs and pictographs carved into granite rocks here in the upper part of the Wakhan Valley. Seeing all of the Langar rock art sites on one trip is an ambitious adventure as they are scattered throughout the valley from the slopes of the Shohdara Valley all the way to the watershed.

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This project, in which research teams from Germany, France, Russia, Ukraine and Tajikistan are taking part, aims to improve and deepen understanding of a geological chronometer with growing scientific importance and obtain new geological knowledge on the basis of its application on minerals from various crustal environments. Progress will be made co-operatively through developing the analytical trace amount technique by modernising equipment and methodical procedures in order to facilitate very sensititive Xe isotope measurements of high precision and accuracy.

This technique will also be used to evaluate new measurements on minerals where the behaviour of the hosting rocks during evolutionary steps of earth history is well known. Efforts will therefore be focused on minerals mainly pitchblende, zircons for which other chemical and isotopic information above all chronometric data are already available or will be supplied by the partners of this research project.

Owing to the well established qualities of the uranium-lead and the samarium-neodymium methods, results obtained by these chronometers will play an important part in the evaluation of the Xe data. Technical and methodological improvements will be carried out on geological samples of current scientific interest to the partners.

They will be taken from high-grade Precambrian metamorphic terrains of Antarctica or the Baltic Shield and from hydrothermal deposits of central Europe. Improvements to the analytical Xe isotope equipment at the Vernadsky Institute are expected. These improvements will make the instruments analytically more sensitive and less susceptible to everyday hazards, thus making a greater amount of analysis possible.

On the basis of the intercomparisons and intercalibrations, ideas will be developed by which the extraordinary Xe retentivity of zircon may be explained. The new age determinations, performed in Moscow, Rennes and Heidelberg, will be contributions to the geological history of the areas and structures from where the samples originate.

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In ancient times, what is now or is close to modern Dushanbe was settled by various empires and peoples, including Mousterian tool-users, various neolithic cultures, the Achaemenid Empire , Greco-Bactria , the Kushan Empire , and the Hephalites. In the Middle Ages , more settlements began near modern-day Dushanbe such as Hulbuk and its famous palace. From the 17th century to the early 20th, Dushanbe began to grow into a market village controlled at times by the Beg of Hisor , Balkh , and finally Bukhara.

Soon after the Russian invasion in , the town was made the capital of the Tajik Autonomous Soviet Socialist Republic in , which commenced Dushanbe’s development and rapid population growth that continued until the Tajik Civil War. After the war, the city became capital of an independent Tajikistan and continued its growth and development into a modern city.

Dushanbe was at a crossroads where a large bazaar occurred on Mondays.

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Tajikistan is the poorest of the former Soviet states. It shares borders with Afghanistan, China, Kyrgyzstan and Uzbekistan. After navigating my way through an airport that would have to take out first prize as the worst in the world , I was in for an initiation like no other. I was caught in a car blockade, amidst a drug bust, and surrounded by black leather clad men clutching AK47s.

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Thick and widespread loess deposits in southern Tajikistan provide insight into the regional climatic changes in arid Central Asia ACA during the Quaternary. However, because of the lack of robust chronological constraints, the environmental implications of these deposits are not yet fully understood. Here, we report a detailed medium-grained quartz optically stimulated luminescence OSL dating analysis on a loess sequence deposited since the Lateglacial in southern Tajikistan.

The single-aliquot regeneration SAR and standardized growth curve SGC methods were used for equivalent dose determination. On the basis of the obtained OSL ages, we reconstructed the dust accumulation rates and mass accumulation rates. Our results show that the dust flux continued to decline whereas the precipitation increased stepwise after the end of the Last Glacial Maximum. Changes in the dust flux and precipitation in ACA were sensitive to the gradual warming since the Lateglacial.

Quartz optically stimulated luminescence dating of loess in Tajikistan and its paleoclimatic implications for arid Central Asia since the Lateglacial Palaeogeography, Palaeoclimatology, Palaeoecology IF 2.

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