Dansens relevans i folkmusikutbildningar

The Relevance of Dance in Folk Music Education The aim of this study was to investigate why and how dance and dance teaching can be relevant in educational programmes in folk music in Sweden. Many of these programmes include dance within them and that fact, in combination with my observation that there is an underlying cultural assumption that dance and music belong together, inspired this research. I wished to look at the function of dance within folk music programmes, and music teachers’ observations of how dance affects their students’ playing. The study has been conducted through qualitative interviews with four music teachers from different institutions, covering three themes: the purpose(s) of including dance in this kind of education, if and how they can see that the students have use for the dance knowledge in their playing, and how they look at the connection between dance and music in this genre. The result shows that there are several reasons for teaching dance as a part of educational programmes in folk music and also that the music teachers themselves use references to dance in their music teaching. These reasons can give dance pedagogues information about how some music teachers think dance is relevant and can be used in the planning of dance teaching. In conclusion, there is a discussion of how this study can be a part of understanding and developing pedagogy within the folk music genre

Dansens relevans i folkmusikutbildningar

The Relevance of Dance in Folk Music Education The aim of this study was to investigate why and how dance and dance teaching can be relevant in educational programmes in folk music in Sweden. Many of these programmes include dance within them and that fact, in combination with my observation that there is an underlying cultural assumption that dance and music belong together, inspired this research. I wished to look at the function of dance within folk music programmes, and music teachers’ observations of how dance affects their students’ playing. The study has been conducted through qualitative interviews with four music teachers from different institutions, covering three themes: the purpose(s) of including dance in this kind of education, if and how they can see that the students have use for the dance knowledge in their playing, and how they look at the connection between dance and music in this genre. The result shows that there are several reasons for teaching dance as a part of educational programmes in folk music and also that the music teachers themselves use references to dance in their music teaching. These reasons can give dance pedagogues information about how some music teachers think dance is relevant and can be used in the planning of dance teaching. In conclusion, there is a discussion of how this study can be a part of understanding and developing pedagogy within the folk music genre

Petrology and ion microprobe U-Pb chronology applied to a metabasic intrusion in southern Sweden: A study on zircon formation during metamorphism and deformation

The Aker metabasite occupies a key position in a major tectonic lineament in southernmost Sweden, the Protogine Zone, which coincides closely with the eastern boundary of the late Mesoproterozoic Sveconorwegian orogen of southwest Scandinavia. Metamorphic reactions, associated with the transformation from isotropic gabbro to foliated garnet amphibolite, were identified from disequilibrium textures of which some involved release of zirconium (Zr) and growth of metamorphic zircon. Ion microprobe dating of igneous zircon gave 1562 +/- 6 Ma, whereas metamorphic zircons yielded ages of 1437 +/- 21, 1217 +/- 75, and 1006 +/- 68 Ma. The presence of baddeleyite pseudomorphs made up of saccharoidal zircon and a higher abundance of older rather than younger metamorphic zircons suggest redistribution of Zr into new zircon, first by the breakdown of baddeleyite (ZrO2) and later by the consumption of igneous phases containing trace amounts of Zr. Several generations of metamorphic zircon and the presence of 1.56 and 1.22 Ga mafic intrusions along the Protogine Zone call for a complex tectonic history probably reaching back to at least similar to1.56 Ga. Growth of metamorphic zircon at similar to1.44 Ga may relate to a regional, compressional event. The WNW trending deformational structures on both sides of the Protogine Zone may possibly relate to that event. The similar to1.22 Ga metamorphic zircons are coeval with the emplacement of numerous granitic, syenitic, and mafic intrusions along and parallel to the Protogine Zone. The age around 1.0 Ga, finally, marks Sveconorwegian metamorphism for which thermobarometry of the Aker garnet-amphibolite suggests 1000-1200 MPa at 600degreesC-630degreesC. Thereafter, significant relative uplift of the rocks to the west of the Protogine Zone occurred on nearly vertical, north-south trending deformation zones

Remotely Sensed Nightlights to Map Societal Exposure to Hydrometeorological Hazards

This study used remotely sensed maps of nightlights to investigate the etiology of increasing disaster losses from hydrometeorological hazards in a data-scarce area. We explored trends in the probability of occurrence of hazardous events (extreme rainfall) and exposure of the local population as components of risk. The temporal variation of the spatial distribution of exposure to hydrometeorological hazards was studied using nightlight satellite imagery as a proxy. Temporal (yearly) and spatial (1 km) resolution make them more useful than official census data. Additionally, satellite nightlights can track informal (unofficial) human settlements. The study focused on the Samala River catchment in Guatemala. The analyses of disasters, using DesInventar Disaster Information Management System data, showed that fatalities caused by hydrometeorological events have increased. Such an increase in disaster losses can be explained by trends in both: (i) catchment conditions that tend to lead to more frequent hydrometeorological extremes (more frequent occurrence of days with wet conditions); and (ii) increasing human exposure to hazardous events (as observed by amount and intensity of nightlights in areas close to rivers). Our study shows the value of remote sensing data and provides a framework to explore the dynamics of disaster risk when ground data are spatially and temporally limited