An Anglo-Saxon Hut on the Car Dyke, at Waterbeach

1927 ◽  
Vol 7 (2) ◽  
pp. 141-146 ◽  
Author(s):  
T. C. Lethbridge

Considerable interest attaches to the Car Dyke as it has been claimed as a Roman work by several authorities (Dr. Cyril Fox, Archaeology of the Cambridge Region, p. 179). In June of this year I attempted to make sure of the date by cutting a section through the fosse.When a well was sunk through the bank of the dyke at the Lodge, Waterbeach, many years ago, the workmen cut through a boat of some kind. It seems reasonable to suppose that this boat dates from the time when the dyke was still full of water, and had been left moored in some little creek or dock probably near a settlement site. I therefore cut a section as near as possible to the well, that is, within a few yards of the south-east corner of the Lodge. It has not been possible to complete the section or reach the bottom of the ditch owing to the wet summer. The water-level was found at a depth of 4 ft. The section, however, cut through the middle of a small dwelling on the very lip of the ditch, debris from it forming a thin stratum separating different layers of silt. From the contents of the midden which formed the floor of the hut it was evident that the site was one of the Pagan Saxon Period.

Author(s):  
Stephen Rippon

During the early medieval period eastern England was occupied by two major Anglo-Saxon kingdoms—the East Saxons and East Angles—alongside a region that Bede referred to as ‘Middle Anglia’. There has been a widespread assumption that Essex (‘the East Saxons’) and Suffolk and Norfolk (the ‘South Folk’ and ‘North Folk’ of East Anglia) were direct successors to these Anglo-Saxon kingdoms (e.g. Carver 1989, fig. 10.1; 2005, 498; Yorke 1990, 46, 61; Warner 1996, 4, plate 1; Pestell 2004, 12; Chester-Kadwell 2009, 46; Kemble 2012, 8; Gascoyne and Radford 2013, 176; Reynolds 2013, fig. 4), which would imply a strong degree of territorial continuity from at least the early medieval period through to the present day. There is, however, a recognition in the Regional Research Framework that regional differences within early medieval society across eastern England have seen little investigation (Medlycott 2011b, 58), something that the following chapters hope to address. This chapter will explore the documentary evidence for these early medieval kingdoms and their relationship to later counties, before turning to the archaeological evidence for Anglo- Saxon immigrants and their relationship to the native British population in Chapters 8–10. The clear differences between the Northern Thames Basin, East Anglia, and the South East Midlands that are still evident during the seventh to ninth centuries are outlined in Chapter 11. Finally, Chapter 12 explores the boundaries of the early medieval kingdoms, and in particular the series of dykes constructed in south-eastern Cambridgeshire.Table 7.1 provides a timeline of key historical dates for early medieval England, and key developments within the archaeological record. The earliest list of territorial entities is the Tribal Hidage. The original document has been lost—it only survives in a variety of later forms—but it is thought to have been written between the mid seventh and the ninth centuries (Hart 1970; 1977; Davies and Vierck 1974, 224–7; Yorke 1990, 10; Blair 1991, 8; 1999; Harrington and Welch 2014, 1). The Tribal Hidage lists at least thirteen peoples in and around eastern England, some of whom clearly occupied quite extensive areas, such as the East Angles (assessed as 30,000 hides), East Saxons (7,000 hides), and the Cilternsætna (4,000 hides).


Sensors ◽  
2019 ◽  
Vol 19 (16) ◽  
pp. 3510
Author(s):  
Nengfang Chao ◽  
Gang Chen ◽  
Zhicai Luo ◽  
Xiaoli Su ◽  
Zhengtao Wang ◽  
...  

The Danjiangkou Reservoir (DJKR) is the freshwater source for the Middle Route of the South-to-North Water Diversion Project in China, and its water level and storage changes are important for water resource management. To maximize the potential capacity of the Gravity Recovery and Climate Experiment (GRACE) mission, an improved Lagrange multiplier method (ILMM) is first proposed to detect terrestrial water storage anomalies (TWSA) in the small-scale basin (DJKR). Moreover, for the first time, water diversion fingerprints are proposed to analyze the spatiotemporal pattern of the TWSA in the DJKR. The results indicate that the increased water level and storage signals due to the DJKR impoundment in 2014 can be effectively detected by using the ILMM, and they agree well with the results from altimetry and in situ data. Additionally, the water diversion fingerprints due to the DJKR impoundment are inferred, and describe the progression of spatiotemporal variability in water storage. The results show that water storage decreased in the upper Hanjiang River and increased in the DJKR as well as to the east of it during the period 2013–2015. Our research provides a scientific decision-making basis for monitoring the water resources of the DJKR and managing the South-to-North Water Diversion Project.


2020 ◽  
Author(s):  
Satoshi Nakada ◽  
Hiroki Haga ◽  
Maho Iwaki ◽  
Keisuke Hatano ◽  
Kohji Mabuchi ◽  
...  

Abstract Global activities of typhoons and hurricanes are gradually changing, and these storms can drastically affect lake ecosystems through the recession of submerged macrophytes that regulate the water quality in lakes. Using an echosounder, we captured the short-term, massive loss of submerged macrophytes attributed to the abnormal fluctuation of the water level induced by the approach of a catastrophic super typhoon in the south basin of Lake Biwa, Japan. This paper investigates the physical processes responsible for the loss of vegetation using a high-resolution circulation model in Lake Biwa as a pilot study area. The circulation model was coupled with dynamical models of the fluid force and erosion acting on the vegetation. Our simulation successfully reproduced the water level fluctuation and high-speed current (torrent) generated by the typhoon gale. The simulated results demonstrate that the fluid force driven by the gale-induced torrent uprooted submerged macrophytes during the typhoon approach and that this fluid force (rather than erosion) caused the outflow of vegetation. As a result, this uprooting attributed to the fluid force induced the massive loss of submerged macrophytes in a large area of the south basin, which might have increased primary production and reduced the stock of fish such as bluegill in the lake. Our approach is practical for evaluating changes in lake environments attributed to the massive outflow of submerged macrophytes under various climate change scenarios. (227 words)


Author(s):  
V. M. Popenko ◽  

In the 70s of the XXth century, the nesting of the Eurasian spoonbill in Ukraine was known only in the lower reaches of the Danube and Dniester, and at the beginning of the XXIst century, it began to spread to the East and the Eurasian spoonbill began to nest on the Tiligulskiy Liman, Karkinit Bay, Western and Eastern Sivash. Since 2016, the Eurasian spoonbill has been observed during the breeding season in the upper reaches of the Utlyukskiy Liman and the estuarine areas of the Bolshoy and Maly Utlyuk Rivers. According to observations that were held in 2016-2020, first there were: a pair with unproven nesting (2016), then flocks of up to 17-26 individuals (2018-2019). In 2020, both individual pairs with nesting behavior and flocks were found near a mixed colony of the Gray heron and the Great egret. Finally, on 24.05.2020, the Eurasian spoonbill nests were found in this colony. Among the 8 nests, one contained 2 eggs and two chicks, four nests contained 4 eggs and the other three - 3 ones. Nests are located on the periphery of the heron colony on clump of reeds. The height of the nesting platforms is about 4-70 cm above the water level, the minimum distance between the nests is about 4 m. It is possible that the flock of 26 adult and young individuals, that was observed on 2.08.2018, consisted of local nesting birds. Thus, another nesting location was found in the South of Ukraine.


Author(s):  
Aidan J. Thomson

Scholars of Arnold Bax have long acknowledged the influence of the Irish Literary Revival on the composer’s compositional output up to about 1920, of Sibelius from the late 1920s onwards, and of the continuity of styles between these two periods. In this article I argue that this continuity relies on what Bax draws from early Yeats, which is less Celtic mythology or folklore than a particular way of imagining nature; that Bax’s use as a compositional stimulus of what he called the ‘Celtic North’ (essentially the landscapes of western Ireland and north-western Scotland) had parallels in the literature and art of 1920s Ireland; and that the ‘Celtic North’ offers a means of critiquing inter-war English pastoralism, which has traditionally been associated with what Alun Howkins, after Hilaire Belloc, has called the ‘South Country’. Bax thus offers a musical engagement with nature that is essentially dystopian, sublime and (within the discourse of British pastoralism) non-Anglo Saxon.


2012 ◽  
Vol 1 (33) ◽  
pp. 48
Author(s):  
Christopher Bender ◽  
William Miller ◽  
Ashley Naimaster ◽  
Tucker Mahoney

The South Carolina Surge Study (SCSS) used the tightly coupled SWAN+ADCIRC model to simulate tropical storm surge events. The tightly coupled model allowed calculation of wave-induced water level changes within the storm surge simulations. Inclusion of the wave-induced water level changes represents a more physics-based approach than previous methods that added wave setup after model simulations ended. Development of the SWAN+ADCIRC model included validation of water levels to local tidal forcing and for three historical hurricanes — Hazel (1954), Hugo (1989), and Ophelia (2005). The validation for waves did not include Hurricane Hazel because measured data was unavailable. Additional comparisons with WAM model results provided supplemental support to the SWAN model results. Model output applied in comparisons included contour plots of maximum wave parameters, time series of wave parameters at selected locations, and wave spectra.


Author(s):  
Simon Roffey

Winchester lays claim to being one of the most important cities in British history. The city has a central place in British myth and legend and was once ancient capital and residence of the Anglo-Saxon and early Norman kings. Winchester is also one of the most extensively excavated medieval towns in England and was the training ground for modern British archeology. Situated in south-central England, Winchester was close to key communication routes via the south coast and the important medieval port at Southampton. Founded in the Roman period as Venta Belgarum, close to the site of the Iron Age market settlement, Winchester quickly grew into a prosperous Roman civitas. After the decline of Roman power in Britain, Winchester remained as an important power center in the south and by the mid-7th century was the pre-eminent town in the newly established Anglo-Saxon kingdom of Wessex. With the consolidation of Wessex’s power in the 9th and 10th centuries and the eventual re-establishment of control over the former Viking-influenced areas of the midlands and the north, Winchester became the seat of English royal power. With the Norman Conquest in 1066, the early Norman kings sought to keep Winchester as the royal seat. However, with the rising pre-eminence of London in the mid-12th century, Winchester’s power declined as royal and secular power shifted to London. Nevertheless, Winchester was still to remain of some importance throughout the medieval period and its bishop one of the most powerful, influential, and richest lords in medieval England; a status still attested to by the city’s medieval cathedral. As a city of many religious foundations, Winchester’s fortunes waned after the Reformation to be briefly reborn in the later 17th century with the planned construction of Charles II palace on the site of the former medieval castle. Charles’ plans to reinvent Winchester as a revitalized English royal city were aborted with his untimely death in 1688, with the palace, designed by Christopher Wren, barely finished.


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