Parochial Structure and the Dissemination of Protestantism in Sixteenth Century England: A Tale of two Cities

1979 ◽  
Vol 16 ◽  
pp. 269-278
Author(s):  
Claire Cross

When, after the abrupt changes in religion in the reigns of Henry VIII, Edward VI and Mary, Elizabethan protestants set about consolidating the protestant reformation they looked upon towns as one of the chief agencies for the conversion of the countryside. From the first moment of his appointment as lord president of the council in the north in 1572 that enthusiastic layman, the third earl of Huntingdon, made this assumption a guiding principle of his governorship. ‘I do all I can to get good preachers planted in the market towns of this country’, he told William Chaderton, bishop of Chester in 1584, adding with a characteristic note of realism, ‘in which somewhat is already done, but much remaineth to be done.’ Huntingdon’s close associate and fellow worker in the north, archbishop Grindal, had earlier informed the queen in similar terms that ‘the continual preaching of God’s word in Halifax’ in the 1560s had been responsible for the town’s stalwart loyalty to the crown during the Rebellion of the Earls. Yet both Grindal and Huntingdon knew very well from personal experience that towns in general and northern towns in particular had not by any means all accorded an automatic or unqualified welcome to protestantism. A comparison between York and Hull demonstrates forcefully how two towns in close geographical proximity could differ very considerably in their initial acceptance of protestantism and in the readiness of their ruling élites to further the propagation of protestant doctrines among the townspeople at large.

2010 ◽  
pp. 99-106 ◽  
Author(s):  
Dejana Dzigurski ◽  
Slobodanka Stojanovic ◽  
Aleksa Knezevic ◽  
Ljiljana Nikolic ◽  
Branka Ljevnaic-Masic

The Jegricka, once a natural watercourse traversing the southwestern part of the Backa region, has been turned into a canal, which became part of the main canal network of the hydro-system Danube-Tisza-Danube (Hs DTD). In its turn, the Hs DTD is part of the European waterway linking the North Sea to the Black Sea, i.e., part of the navigable Rhine-Main-Danube Canal. The watercourse is 65.4 km long and it is divided into three levels. The presence of the regulated and the nonregulated sections of the canal, frequent and abrupt changes in water level in the individual sections, different depths and surface water widths of the various sections and the fishpond constructed in the lower section cause considerable vegetation diversity. The vegetation comprises aquatic associations of the classes Hydrochari-Lemnetea Oberd. 1967 and Potametea Tx. et Prsg. 1942. The class Hydrochari-Lemnetea Oberd. 1967 includes the following phytocoenoses: Salvinio-Spirodeletum polyrrhizae Slavnic 1956, Ceratophylletum demersi (So? 27) Hild. 1956, Lemno-Utricularietum vulgaris So? 1928 and Hydrocharidetum morsus-ranae Van Langendonck 1935. The class Potametea Tx. et Prsg. 1942 includes the associations Myriophyllo-Potametum So? 1934, Najadetum marine Fukarek 1961, Nymphaeetum albae Vollmar 1947, Nymphoidetum peltate (Allorge 1922) Oberd. et M?ller 1960 and Trapetum natantis M?ller et G?rs 1960.


2017 ◽  
Vol 26 (1) ◽  
pp. 30-49 ◽  
Author(s):  
Gregory A. Houseman

Istanbul and Bucharest are major European cities that face a continuing threat of large earthquakes. The geological contexts for these two case studies enable us to understand the nature of the threat and to predict more precisely the consequences of future earthquakes, although we remain unable to predict the time of those events with any precision better than multi-decadal. These two cities face contrasting threats: Istanbul is located on a major geological boundary, the North Anatolian Fault, which separates a westward moving Anatolia from the stable European landmass. Bucharest is located within the stable European continent, but large-scale mass movements in the upper mantle beneath the lithosphere cause relatively frequent large earthquakes that represent a serious threat to the city and surrounding regions.


2021 ◽  
Author(s):  
Hongmei Ren ◽  
Ang Li ◽  
Pinhua Xie ◽  
Zhaokun Hu ◽  
Jin Xu ◽  
...  

<p>      Water vapor transport affects regional precipitation and climate change. The measurement of precipitable water and water vapor flux is of great significance to the study of precipitation and water vapor transport. In the study, a new method of computing the precipitable water and estimating the water vapor transport flux using multi-axis differential optical absorption spectroscopy (MAX-DOAS) were presented. The calculated precipitable water and water vapor flux were compared to the European Centre for Medium-Range Weather Forecasts (ECMWF) reanalysis data and the correlation coefficient of the precipitable water, the zonal and meridional water vapor flux and ECMWF are r≥0.92, r=0.77 and r≥0.89, respectively. The seasonal and diurnal climatologies of precipitable water and water vapor flux in the coastal (Qingdao) and inland (Xi’an) cities of China using this method were analyzed from June 1, 2019 to May 31, 2020. The results indicated that the seasonal and diurnal variation characteristics of the precipitable water in the two cities were similar. The zonal fluxes of the two cities were mainly transported from west to east, Qingdao's meridional flux was mainly transported to the south, and Xi'an was mainly transported to the north. The results also indicated that the water vapor flux transmitting belts appear near 2km and 1.4km above the surface in Qingdao and appeared around 2.8km, 1.6km and 1.0km in Xi'an. </p>


Author(s):  
Carla Gardina Pestana

Religion shaped the early modern Atlantic world in many ways. Although Iberian expansion began before the Protestant Reformation, Europe soon divided between Protestant and Catholic, and this division created a context for European understandings of the purpose of expansion. With permission from the pope to evangelize outside the Old World, the Spanish and the Portuguese split the extra-European world between them; Spain was responsible for most of the Americas (excluding only the area that would become Brazil), while Portugal took Brazil and Africa (as well as Asia). Soon representatives of each kingdom were at work, conquering, colonizing, and evangelizing. Protestantism, although it arrived late in the contest for colonies and trade in this New World, was central to Spanish understanding of its work; evangelizing the native peoples of the Americas would add additional souls to the church, making up for those who had been lost to the Protestant Reformation. When Protestants finally became involved in colonizing the Americas and trading with Africa, they similarly understood their role as combating the reach and influence of their Catholic rivals. If in 1600 the European presence outside of Europe was overwhelmingly Catholic, by 1700 a map of the spread of Christianity showed varied results. Spain controlled the central area of the Americas, including much of South America and the Caribbean, all of Central America, and all the southern area of North America (from Florida and New Mexico south). Portugal had Brazil, while Catholic France held Quebec to the north and selected islands in the Caribbean. The Protestant presence was predominantly British, and included eastern North America between Quebec and Florida as well as some islands in the Caribbean. The Protestant Dutch also held island colonies and a South American outpost. West Africa and West Central Africa hosted trading forts controlled by most of these European powers, from which were shipped slaves as well as trade goods. The religious rivalries of early modern Europe had been effectively exported. Every faith represented along the shores of the Atlantic prior to contact would participate in the intermixing that occurred afterward. The history of religion in the Atlantic world therefore explores the variety of traditions within that world and the effects of the circulation, transplantation, and encounter of these various faiths.


Nature ◽  
2003 ◽  
Vol 421 (6921) ◽  
pp. 354-357 ◽  
Author(s):  
Anil K. Gupta ◽  
David M. Anderson ◽  
Jonathan T. Overpeck

2013 ◽  
Vol 9 (4) ◽  
pp. 3871-3917
Author(s):  
J. T. Andrews ◽  
A. E. Jennings

Abstract. In the area of Denmark Strait (~66° N) the two modes of the North Atlantic Oscillation (NAO) are expressed in changes of the northward flux of Atlantic Water and the southward advection of Polar Water in the East Iceland Current. Proxies from marine cores along an environmental gradient from extensive to little or no drift ice, capture low frequency NAO-like variations over the last 2000 cal yr BP. Key proxies are the weight% of calcite, a measure of surface water stratification and nutrient supply, the weight% of quartz, a measure of drift ice transport, and grain-size. Records from Nansen and Kangerlussuaq fjords show variable ice-rafted debris (IRD) records but have distinct mineralogy associated with differences in the fjord catchment bedrock. High-resolution detrended records from Kangerlussuaq Trough show abrupt, significant multi-decadal changes (72 and 56 yr for calcite, and 94 and 65 yr for quartz), and parallel the 2000 yr Arctic summer temperature reconstructions. The calcite minimum occurred ca. 1550 AD whereas the quartz maxima occurred 200 yr earlier. Changes in calcite wt% from N and SW Iceland show similar abrupt changes to those in Kangerlussuaq Trough with an abrupt calcite peak ~1320 AD. Quartz values increased at two N Iceland sites in the last 500 yr whereas values declined in the East Greenland site.


2014 ◽  
Vol 8 (4) ◽  
pp. 43-49
Author(s):  
Brigitta Palatinus

The main reason of the research is to make a survey of the habits of foreign visitors arriving in Debrecen by air and their satisfaction. What was experienced in 2013 regarding low foreign proportion is also noticable in 2014. In the examined two months, of the whole passenger traffic between London and Debrecen only 10-15% is tourism by foreign visitors. There was not any information before about consumption of tourists arriving in Debrecen by air. In the course of my research I was examining the main elements of consumptions. From the gathered infromation from the questionaires it can be ascertained that on many occasions service providers failed to accomplish satisfying levels, quality. Underachievement occured and the experience of the visitors was worse than their expectations. This gives reasons for the indicators detailed analysis. The results of the satisfaction test might be an essential basis to further develop the city’s tourist products and services in the future. Personal experience of either visitors satisfaction or dissatisfaction, gets stored as a memory which influences future decisions on travelling. Because of this the city has to make an effort to provide higher standards of quality to people travelling into Debrecen by air from the first moment of arrival till the last moment of departure and leave satisffied.


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