This study investigates the morphological impacts of the 1872 Baltic storm flood on a beach-ridge system (sandy spit) in south-easternDenmark and evaluates the frequency of extreme storm flood events in the area over a longer time perspective
Stable carbon and nitrogen isotope ratios from bones of contemporaneous Late Atlantic aurochs and early cattle in easternDenmark are significantly different and provide information on the origin and feeding strategies of the earliest domestic
cattle. This study focuses on the eastern part of Denmark, the area from where most of the examined and dated material originates.
Clusters in an age of increasing internalisation, highlighted by the closing cluster of Herning, Denmark
Clothing industry ; Denmark ; Developing countries ; Industrial concentration ; Industry ; International competition ; Internationalization ; Textile industry
The paper examines the textile and clothes production cluster of Herninging western Jutland, Denmark, which came into existence from the 1930s and expanded successfully after World War II. Meeting competition from the low wage countries of Central
-Eastern Europe and East Asia after 1990, it has survived with virtually no unemplyment. On this background, three problems are discussed : the meeting of globalization by openness, innovation and entrepreneurship. Current cluster theories, which
This paper introduces the concept of Integrated Coastal Zone Management (ICZM) in a definition with relevance for Denmark. Partly influenced by the Rio Conference the Danish government now deals with the concept of a sustainable development
This article describes the influence of man on the coastal landscapes along the Danish and part of the German west coast. While the tidal coast south of Blåvandshuk was formed by man since premedieval times, the northern part of Jutlands coast
Glacial ice-flows on the islands of Bornholm and Christianso, Denmark
This paper contains results from studies of ice flow directions on the islands of Bornholm and Christianso, Denmark, as indicated by striae and other marks of glacial erosion on the bedrock surface.