scholarly journals The Imaginary North in Finnish Comics on Migration

Nordlit ◽  
2020 ◽  
Author(s):  
Ralf Kauranen ◽  
Olli Löytty

This article analyses three comics published in Finland that are focused on migration and offer differing insights into the representation of ‘the north’: Pentti Otsamo’s Kahvitauko (2012), Leen van Hulst’s Maitoa ja lunta / Milk and Snow (2011) and Lauri Ahtinen’s Elias (2018). These albums are both representative of the field in general and unique with respect to their treatment of the connections between place and migration. The analysis of the imaginary north is structured around the three tropes of the northern suburb, the northern climate, and the northern natural environment. What is common to them all is a construction of the north as a place without clear limitations and as an amalgamation of various relationships. A central aspect of what a place is in the globalized world is that it constitutes a meeting place. In Kahvitauko, the drinking of coffee is used to show how ‘north’ and ‘south’ are connected on a global scale. In Elias, the symbols of the north, the snow, and the bear, are tied together with Afghanistan. Maitoa ja lunta / Milk and Snow provides another viewpoint, as it lacks the representation of xenophobia. Read in parallel with the other two comics it not only shows that migrants of different kinds are treated differently, but also highlights how a place such as the north is defined in different terms depending on reasons for migration, race and ethnicity, and privilege in general. A place is precisely a place for articulation of networks of meanings, experiences, and people. In addition, the three albums are posited in the broader field of Finnish comics on migration. This is carried out with a focus on how the very concrete places in the comics in the field are named and visually anchored.

2021 ◽  
Vol 77 (1) ◽  
pp. 67-74
Author(s):  
Jessica Donahue ◽  
Steven Hoehner ◽  
Ben Li

This article focuses on the problem of analytically determining the optimal placement of five points on the unit sphere {\bb S}^{2} so that the surface area of the convex hull of the points is maximized. It is shown that the optimal polyhedron has a trigonal bipyramidal structure with two vertices placed at the north and south poles and the other three vertices forming an equilateral triangle inscribed in the equator. This result confirms a conjecture of Akkiraju, who conducted a numerical search for the maximizer. As an application to crystallography, the surface area discrepancy is considered as a measure of distortion between an observed coordination polyhedron and an ideal one. The main result yields a formula for the surface area discrepancy of any coordination polyhedron with five vertices.


Author(s):  
William B. Meyer

One of the earliest historians of the Civil War saw it as a fundamental clash between the peoples of different latitudes. Climate had made the antebellum North and South distinct societies and natural enemies, John W. Draper argued, the one democratic and individualist, the other aristocratic and oligarchical. If such were the case, the future of the reunited states was hardly a bright one. But Draper saw no natural barriers to national unity that wise policy could not surmount. The restlessness and transience of American life that many deplored instead merited, in his view, every assistance possible. In particular, he wrote, Americans needed to be encouraged to move as freely across climatic zones as they already did within them. The tendency of North and South to congeal into hostile types of civilization could be frustrated, but only by an incessant mingling of people. Sectional discord was inevitable only if the natural law that "emigrants move on parallels of latitude" were left free to take its course. These patterns of emigration were left free, for the most part, but without the renewed strife that Draper feared. After the war as before it, few settlers relocating to new homes moved far to the north or south of their points of origin. As late as 1895, Henry Gannett, chief geographer to the U.S. Census, could still describe internal migration as "mainly conducted westward along parallels of latitude." More often as time went on, it was supposed that race and not merely habit underlay the pattern, that climatic preferences were innate, different stocks of people staying in the latitudes of their forbears by the compulsion of biology. Thus, it was supposed, Anglo-Saxons preferred cooler lands than Americans of Mediterranean ancestry, while those of African descent preferred warmer climates than either. Over time, though, latitude loosened its grip and exceptions to the rule multiplied. As the share of the population in farming declined, so did the strongest reason for migrants to stay within familiar climates. Even by the time Gannett wrote, the tendency that he described, though still apparent, was weaker than it had been at mid-century. It weakened because a preference for familiar climates was not a fixed human trait but one shaped by experience and wants, and capable of changing as these variables changed.


2014 ◽  
Vol 955-959 ◽  
pp. 3777-3782 ◽  
Author(s):  
Xiao Feng Zhao ◽  
Bin Le Lin

We evaluated land suitability for Jatropha cultivation at a global scale under current and future climate scenarios. Areas that are suitable for Jatropha cultivation include southern South America, the west and southeast coasts of Africa, the north of South Asia, and the north and south coasts of Australia. In the predicted climate change scenarios, areas near the equator become less suitable for Jatropha cultivation, and areas further from the equator become more suitable. Our analyses suggest that the rank order of the six climate change scenarios, from the smallest to the largest effects on Jatropha cultivation, was as follows: B1, A1T/B2, A1B, A2, and A1FI.


2012 ◽  
Vol 9 (8) ◽  
pp. 9119-9162
Author(s):  
M. Meybeck ◽  
M. Kummu ◽  
H. H. Dürr

Abstract. Questions related to water such as its availability, water needs or stress, or management, are mapped at various resolutions at the global scale. They are reported at many scales, mostly along political or continental boundaries. As such, they ignore the fundamental heterogeneity of the hydroclimate and the natural boundaries of the river basins. Here, we describe the continental landmasses according to eight global-scale hydrobelts strictly limited by river basins, defined at a 30′ (0.5°) resolution. The belts were defined and delineated, based primarily on the annual average temperature (T) and runoff (q), to maximise interbelt differences and minimise intrabelt variability. The belts were further divided into 29 hydroregions based on continental limits. This new global puzzle defines homogeneous and near-contiguous entities with similar hydrological and thermal regimes, glacial and postglacial basin histories, endorheism distribution and sensitivity to climate variations. The Mid-Latitude, Dry and Subtropical belts have northern and southern analogues and a general symmetry can be observed for T and q between them. The Boreal and Equatorial belts are unique. The hydroregions (median size 4.7 Mkm2) contrast strongly, with the average q ranging between 6 and 1393 mm yr−1 and the average T between −9.7 and +26.3 °C. Unlike the hydroclimate, the population density between the North and South belts and between the continents varies greatly, resulting in pronounced differences between the belts with analogues in both hemispheres. The population density ranges from 0.7 to 0.8 p km−2 for the North American Boreal and some Australian hydroregions to 280 p km−2 for the Asian part of the Northern Mid-Latitude belt. The combination of population densities and hydroclimate features results in very specific expressions of water-related characteristics in each of the 29 hydroregions. Our initial tests suggest that hydrobelt and hydroregion divisions are often more appropriate for water-relative global analysis and reporting than conventional continental or political divisions.


1878 ◽  
Vol 5 (7) ◽  
pp. 305-310
Author(s):  
Townshend M. Hall

The Meeting of the British Association at Plymouth has not unnaturally been the means of directing attention to some of the most complex points of Devonshire geology, and of reviving the discussion as to the age and position of the Devonian series in North and South Devon. Mr. Jukes, it will be remembered, died in 1869. Had he lived longer, his energy of purpose would doubtless have led him to carry on the work he had begun, until he could either prove the correctness of his views, or satisfy himself that the generally accepted classification was, after all, the right one. The followers of Jukes seem to confine themselves to those portions only of the district which he had more specially studied—North Somerset, Lynton and Pickwell Down; searching in almost hopeless despair amongst the lower rocks, instead of beginning at the other end of the scale, with the Millstone-grit, and tracing the beds downwards. As a result, the fossiliferous beds of the Upper Devonian have been almost entirely neglected, and their relation to the Carboniferous slates passed over.


Author(s):  
Henrich Neumann

The Ballachulish slates, exposed to the north and south of Loch Leven in Argyllshire, contain, in most places, cubes of pyrite up to half an inch in diameter. During a visit to the area in the spring of 1949 the writer's attention was attracted by the dark colour of the 'pyrite' cubes in the North Ballaehulish slate quarry a little more than a mile east of Onich. On examination these proved to consist of a mass of haphazardly orientated crystals of pyrrhotine with irregular outlines. Slates collected from the main working quarry on the south shore of Loch Leven, on the other hand, contain cubes which are single crystals of unaltered pyrite.


C. Vann Woodward’s lecture compares two commemorations of the Civil War fifty years apart, one in 1911 and the other in 1961. The first one reflected sectional reunification predicated on a shared understanding of the tragic nature of war but also a sense that the conflict had solved the problem of sectional animosity. In so doing Woodward notes that whites in the North and South could only accomplish this by excluding meaningful African-American participation. The lecture then outlines the cycles of Reconstruction historiography, and looks at the dual psychological traumas the North and South experienced in the aftermath of Reconstruction. Woodward maintains that after the North emerged victorious from the war it failed to live up to its ideals, leaving wracked guilt, self-criticism, and remorse. The South emerged with a predilection for extortion, indignation, and extreme bellicosity, consistently blaming its own weaknesses on Reconstruction. Woodward suggests that historians should act as therapists, enabling the nation to come to terms with the psychological traumas triggered by the past.


Author(s):  
Roger Ling ◽  
Paul Arthur ◽  
Georgia Clarke ◽  
Estelle Lazer ◽  
Lesley A. Ling ◽  
...  

The casa degli amanti (house of the lovers), at the south-west corner of the insula, falls into two fairly distinct halves: the atrium complex, oriented on the street to the west, and the peristyle with its surrounding rooms, oriented on the street to the south and on the property boundary to the east. In the atrium complex, the atrium is misplaced to the south of the central axis, allowing space for two large rooms to the north, one of which was possibly a shop or workshop (5.50 m. × 4.70 m.), with a separate entry from the street (I 10, 10), while the other (5.80 m. × 4.50 m.), decorated with mythological wallpaintings and provided with a wide opening on to the peristyle, must have been a dining-room or oecus (room 8). Each of these had a segmental vault rising from a height of about 3.50 m. at the spring to slightly over 4 m. at the crown. In the first the vault is missing, but the holes for some of its timbers are visible in the east wall and a groove along the north wall marks the seating for the planking attached to them; at a higher level, in the north and south walls, are the remains of beam-holes for the joists of the upper floor or attic (see below). The arrangements in room 8 are now obscured by the modern vault constructed to provide a surface for the reassembled fragments of the ceiling-paintings; but the shape of the vault is confirmed by the surviving plaster of the lunettes, while a beam-hole for the lowest of the vault-timbers is visible above the corner of the western lunette in an early photograph (Superintendency neg. C 1944). The shop I 10, 10 had a small window high in the street wall to the south of Its entrance; whether there were any additional windows above the entrance, it is impossible to say, since this part of the wall is a modern reconstruction. Room 8 was lit by a splayed window cut in the angle of the vault and the eastern lunette, opening into the upper storey of the peristyle.


2017 ◽  
Vol 51 (2) ◽  
pp. 117-141
Author(s):  
Günther Schlee

Omaha kinship terminologies are distributed globally to the north and south of the belt of ancient “high cultures” which stretches from the Mediterranean Sea to East and Southeast Asia in the Old World and includes parts of Mesoamerica and the Andes in the New World. This article offers an explanation for this curious distribution of Omaha terminologies. In so doing, it reviews examples of Omaha terminologies in Central Asia and on the Horn of Africa, noting their defining characteristics and those other aspects of social organization with which they are associated. In conclusion, it is suggested that a continuum of lineage-based systems, including systems with Omaha terminologies, was split into two areas of concentration, one to the north and the other to the south, as ancient “high cultures,” based on intensive agricultural production, arose among them, reverting, in the process, to terminological systems with a cognatic bias like those of the Eskimo type that are associated with urbanization and statehood.


1928 ◽  
Vol 8 (1) ◽  
pp. 69-75
Author(s):  
W. Douglas Simpson

The ruins of Kindrochit Castle stand in the heart of the much-frequented village of Braemar, near the head of the river Dee, amid the wild mountains of western Aberdeenshire. The castle occupies a very strong position on the east brink of a rocky gorge formed by the Clunie Water, and on the other side was defended by an ancient mill-lade, taken off the Clunie above the castle, and rejoining it below, so as to complete the insulation of the site. In the name of the castle (Kindrochit = ‘bridge-head’) is enshrined its early importance as a fortified post guarding the passage of the great north road across the Clunie Water. The map (fig. 1) clearly indicates how the significance of the castle is to be found not in the east-and-west or blind-alley strategy of the Dee valley, but rather in the north and south or transversal strategy of the ancient trunk roads converging northwards across the ‘Mounth’ or mountain barrier between Strathmore and Mar.


Sign in / Sign up

Export Citation Format

Share Document