History of the Geological Research in Egypt

Author(s):  
Mohamed El-Sharkawi ◽  
Nagy Shawky Botros ◽  
Ahmed A. Madani ◽  
Mohamed Ahmed ◽  
Bassam Abdellatif ◽  
...  
1997 ◽  
Vol 17 (1) ◽  
pp. 16-22 ◽  
Author(s):  
W. Brian Harland

Useful records of observations perhaps began in 1596 with Barents' voyage and resulting chart. The many expeditions until the middle of the eighteenth century were primarily for whaling with minor additions to the charts. In 1758 A. R. Martin led a Swedish voyage and in 1773 C. J. Phipps commanded a British naval expedition, the first of several, to seek a northeast passage to the Pacific. They penetrated no further than Spitsbergen and made useful observations. At that time and for many years the British Admiralty was concerned with extensive Arctic exploration. The elaborate nature of these expeditions was not so much designed for scientific purposes as for useful employment for enterprising officers, with ships in numbers no longer needed in the period of naval supremacy after 1805. Hydrographic survey was often the principal achievement. In terms of efficiency and Arctic know-how the early whalers such as Scoresby were superior.1827 may be considered as the year when geological work began, with expeditions from Norway (B. M. Keilhau 1831) and Britain (Capt. Parry, e.g. Horner 1860; Salter 1860). Keilhau, a geologist, visited Edgeoya and Bjornoya. Admiral Parry, Hydrographer of the Navy, wintered on HMS Hecla in Sorgfjorden where further specimens were collected. In 1837 an early Swedish expedition was directed by Loven. Then, 1838 to 1840, the French voyage of La Recherche took place under the Commission Scientifique du Nord (e.g. Robert 1840).Only a selection of the many expeditions in the second half of the century are noted here.


Author(s):  
Akif A. Alizadeh ◽  
Ibrahim S. Guliyev ◽  
Fakhraddin A. Kadirov ◽  
Lev V. Eppelbaum

2015 ◽  
Vol 34 (3) ◽  
pp. 101-116 ◽  
Author(s):  
Magdalena Ratajczak-Szczerba ◽  
Iwona Sobkowiak-Tabaka ◽  
Iwona Okuniewska-Nowaczyk

Abstract The region of the Lubusz Lakeland in western Poland where there are a lot of subglacial channels provides opportunity for multi-proxy palaeoenvironmental reconstructions. None of them has not been the object of a specific study. The developmental history of the palaeolakes and their vicinity in the subglacial trough Jordanowo-Niesulice, spanning the Late Glacial and beginning of the Holocene, was investigated using geological research, lithological and geomorphological analysis, geochemical composition, palynological and archaeological research, OSL and AMS-radiocarbon dating. Geological research shows varied morphology of subglacial channel where at least two different reservoirs functioned in the end of the Last Glacial period and at the beginning of the Holocene. Mostly during the Bølling-Allerød interval and at the beginning of the Younger Dryas there took place melting of buried ice-blocks which preserved the analysied course of the Jordanowo-Niesulice trough. The level of water, and especially depth of reservoirs underwent also changes. Palynological analysis shows very diversified course of the Allerød interval.


2021 ◽  
Vol 12 (2) ◽  
pp. 173-198
Author(s):  
O. V. Petrov ◽  
A. I. Khanchuk ◽  
S. P. Shokalsky ◽  
G. A. Babin ◽  
I. I. Pospelov

An overview of the history of tectonic mapping in Russia is presented, and the principles of tectonic mapping are briefly described. Here, out attention is focused on the Tectonic Map of North, Central and East Asia (scale 1:2500000, 2014) and the Tectonic Map of the Arctic (scale 1:5000000, 2019) prepared by international projects of Karpinsky Russian Geological Research Institute (VSEGEI). The projects included participants from geological service agencies, universities and the academies of sciences of 13 countries. We describe the mapping approaches, structural features, legends, graphical design, and information at the map margins. The experience gained with the projects of these two tectonic maps will be used to compile the International Tectonic Map of Asia, scale 1:5000000 (ITMA-5000) and the Tectonic Map of Russia, scale 1:2500000.


2021 ◽  
Author(s):  
Marina Shelakina ◽  

The article discusses the development of engineering and geological research on the example of prospecting and exploration of popular common (construction) minerals in the Krasnodar Territory. A comparative characteristic of the history of engineering geology development is given by analyzing the data of the Fund of the "KUBANGEOLOGY" and the planned economy of the USSR. The set goals and objectives of the planned economy of the USSR directly stimulated engineering and geological research. The peak of prospecting and exploration of popular common (construction) minerals in the Krasnodar Territory falls on the decade from 1970 to 1980, and the main rates - for the period from 1950 to 1980 - during the intensive growth of road, industrial and civil construction. Having arisen to solve the problems of engineering and economic development of territories, engineering geology developed not only in a geological, but geotechnical channel, as evidenced by the separation of surveys from it. The final differentiation from the beginning of 1960 of engineering geology into engineering-geological surveys and engineering geology of building materials proves the need for separation of surveys due to the accumulated regulatory framework and the scale of engineering-geological research, therefore, of the "KUBANGEOLOGY" switched to monitoring of hazardous processes of the geological environment, which is confirmed by the analysis of the fund.


Author(s):  
Anne O'Connor

Ideas about the British Palaeolithic and its connections to geological time changed enormously between the days of the early eighteenth century, when Bagford wondered whether the implement found by Conyers at Gray’s Inn Lane had been left by an Ancient Briton near the bones of a Roman elephant, and the century covered in this book. In the hundred years that followed the acceptance of human antiquity—between c.1860 and c.1960— similar tools were scrutinized by many other interested eyes; they were labelled and classified, and their age and meaning were vigorously debated. In the present study, I have provided a picture of changing ideas about British Palaeolithic tools and their place in geological time, and have also tried to recover the excitement of the arguments that swept through this century of geological research and its little-known relations with archaeology. Views of the past were not built up by dispassionate authorities, coolly observing the range of available and expanding data; the gaze of each individual was restricted by different questions and expectations that encouraged them to describe, interpret, and defend different patterns in the ancient stone tools of Britain. It is now time, before closing this chapter on the history of British Palaeolithic research, to stand back and take a broader look at some of the reasons for these differing beliefs and for their varying success. But first, a recapitulation is offered of the major developments. In this summary, presented below, the Gray’s Inn Lane implement is followed through time to highlight the changes in perception of the Palaeolithic. During the latter part of the tale, this pear-shaped ‘hand-axe’ found by Conyers is accompanied by the Clactonian industry, which has supplied a more familiar anchor point for the shifting interpretations described in previous chapters. Human antiquity was widely accepted in learned circles after they heard the famous papers of 1859. But it was a few years more before the hand-axe from Gray’s Inn Lane became described as the contemporary of many extinct prehistoric animals and assigned to post-submergence, post-glacial times. The work of geologists was central to the task of placing such implements more precisely in Britain’s distant past. Chapters 1 and 2 described how geologists had been attracted in increasing numbers to the once-unpopular drifts and the bones and tools that they preserved.


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