Field guide to Mount Baker volcanic deposits in the Baker River valley: Nineteenth century lahars, tephras, debris avalanches, and early Holocene subaqueous lava

Author(s):  
David S. Tucker ◽  
Kevin M. Scott ◽  
David R. Lewis
Balcanica ◽  
2004 ◽  
pp. 91-158
Author(s):  
Milos Lukovic

With the partitioning in 1373 of the domain of Nikola Altomanovic, a Serbian feudal lord, the old political core of the Serbian heartland was shattered and the feudal Bosnian state considerably extended to the east. The region was crossed by the Tara river, mostly along the southeast-northwest "Dinaric course". Although the line along which Altomanovic?s domain was partitioned has been discussed on several occasions and over a comparatively long period, analyses show that the identification of its section south of the Tara is still burdened by a number of unanswered questions, which are the topic of this paper. An accurate identification of this historical boundary is of interest not only to historiography, but also to archaeology ethnology, philology (the history of language and dialectology in particular) and other related disciplines. The charters of Alphonse V and Friedrich III concerning the domain of herceg Stefan Vukcic Kosaca, and other historical sources relating to the estates of the Kosaca cannot reliably con?rm that the zupa of Moraca belonged to the Kosaca domain. The castrum Moratsky and the civitate Morachij from the two charters stand for the fortress near the village of Gornje Morakovo in the zupa of Niksic known as Mrakovac in the nineteenth century, and as Jerinin Grad/Jerina?s Castle in recent times. The zupa of Moraca, as well as the neighbouring Zupa of Brskovo in the Tara river valley, belonged to the domain of the Brankovic from the moment the territory of zupan Nikola Altomanovic was partitioned until 1455, when the Turks ?nally conquered the region thereby ending the 60-year period of dual, Serbian-Turkish, rule. Out of the domain of the Brankovic the Turks created two temporary territorial units: Krajiste of Issa-bey Ishakovic and the Vlk district (the latter subsequently became the san?ak of Vucitrn). The zupa of Moraca became part of Issa-bey Ishakovic?s domain, and was registered as such, although the fact is more di?cult to see from the surviving Turkish cadastral record. The zupa of Moraca did not belong to the vilayet of Hersek, originally established by the Turks within their temporary vilayet system after most of the Kosaca domain had been seized. It was only with the establishing of the San?ak of Herzegovina that three nahiyes which formerly constituted the Zupa of Moraca (Donja/Lower Moraca, Gornja/Upper Moraca and Rovci) were detached from Issa-bey?s territory and included into the San?ak of Hercegovina. It was then that they were registered as part of that San?ak and began to be regarded as being part of Herzegovina.


Author(s):  
Andrew S. Natsios

How did the British and Egyptian colonial period set the stage for later Sudanese conflicts after independence? The British and Egyptian rule continued and accelerated the discontinuities of nineteenth-century development in Sudan. The disparity between the development of the Nile River Valley and the neglect...


2017 ◽  
Vol 44 (1) ◽  
pp. 216-225
Author(s):  
Sławomir Superson ◽  
Piotr Gębica ◽  
Adam Michczyński ◽  
Piotr Kołaczek ◽  
Kazimierz Szczepanek

Abstract The paper presents the results of the latest radiocarbon dating and the palynological analyses of organic sediments found in the alluvia of the Wisłok River valley between the towns of Łańcut and Przeworsk. The study conducted in the gravel pit made possible the dating of several alluvial fills of the 7–8 m high Holocene terrace and the 5–6 m high floodplain. The oldest channel alluvia and palaeochannel sediments of the 7–8 m high terrace were dated at 10 100–9300 BP (11 960–10 500 cal BP). According to the anthracological analysis the top cover of clay overbank alluvia, which bears charcoal fragments, was deposited in the Subboreal and/or the Subatlantic Phases. In the sequence of the 5–6 m high floodplain, the bottom fills of palaeochannels, dated at 10 195–9885 cal BP (probability level: 68.2%; GdS-3233: 8900 ± 95 BP ) and 11 095–10 755 cal BP (probability level: 68.2%; GdS-3228: 9575 ± 95 BP), were truncated by erosion and covered by alluvia of palaeomeanders, which were active in the 19th century. Preservation of the erosional bench of the Early Holocene organic sediments indicates the predomination of lateral migration of the river channel during the last 200 years and the formation of wide erosional floodplain that has been aggraded with recent flood alluvia. In the 20th century the floodplain aggradation was simultaneous with the deepening of the Wisłok riverbed.


Renascence ◽  
2021 ◽  
Vol 73 (2) ◽  
pp. 81-100
Author(s):  
Geoffrey Reiter ◽  

In contemporary academic circles, the fields of science, theology, and literature may be compartmentalized with relatively little interaction. However, such distinctions were less rigid in the early nineteenth century. One of the figures whose writings stretched across these disciplinary boundaries was Edward Hitchcock, a world-renowned geologist and president of Amherst College who also had extensive theological training. Now best-known among paleontologists for his discovery of fossil footprints in the Connecticut River Valley, Hitchcock made use of his considerable talents in an 1836 poem entitled “The Sandstone Bird.” This poem—often known to historians of science but little remarked among students of American literature—effectively uses formal verse to draw out theological dimensions to the prehistoric world conjured up by Hitchcock’s own paleontological discoveries.


2020 ◽  
Vol 560-561 ◽  
pp. 259-272
Author(s):  
Shaddai Heidgen ◽  
Elena Marinova ◽  
Raiko Krauß ◽  
Oliver Nelle ◽  
Martin Ebner ◽  
...  
Keyword(s):  

2009 ◽  
Vol 106 (13) ◽  
pp. 5014-5018 ◽  
Author(s):  
A. J. Ranere ◽  
D. R. Piperno ◽  
I. Holst ◽  
R. Dickau ◽  
J. Iriarte
Keyword(s):  

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