Prices of food products in Polish Territory as index of climatic oscillations in the Little Ice Age
Climate oscillation ; Climatic variation ; Economic indicators ; Historical geography ; Little ice age ; Poland ; Price
oscillations corresponding with climatic changes are found in this diagram. Three periods of a relatively rapid growth of prices can be distinguished which correspond with three cooling waves during Little Ice Age.
Elevational shifts of Coleogyne ramossissima in the Mojjave Desert during the Little Ice Age
California ; Climatic variation ; Desert ; Little ice age ; Nevada ; Palaeo-ecology ; Palaeogeography ; Precipitation ; United States of America ; Vegetation
In this paper, the AA. add to the knowledge of vegetation changes in the Mojave desert during the Little Ice Age through study of fossil woodrat middens located in the eastern part of the desert where substantially greater amounts of precipitation
Washington Schools, Little White Man Schools und Indian Schools - bildungsgeographische Fragestellungen dargestellt am Beispiel der Navajo Indianerreservation
Washington Schools, Little White Man Schools et Indian Schools - questions concernant la géographie de l'éducation, l'exemple de la réserve des Indiens Navajos
Two colleagues and former students look back at the contribution of Franklin's research. Franklin was an eclectic scholar for whom traditional boundaries, disciplinary and geographical meant little and this has challenged any categorisation.
Climatic variation ; Climatic warming ; Czech Republic ; Global change ; Historical geography ; Little ice age ; Model ; Precipitation ; Temperature
. The prevalence of extremly cold and also rainy periods, as an expression of the Little Ice Age, is most conspicuous in the 15th century. Since the latter half of the 19th century a rising temperature trend has manifested itself. A regional climatic scenario
of institutionalized obstacles to effective leader participation, are studied. This population has little opportunity to reverse this decay. Tey are obstacles to control neighborhood change.
The hydraulics of composite overland flow around surface stones are extremely complex and have been little studied. The purpose of this paper is to review both field and laboratory research on this subject and to discuss briefly the implications
Theoretical model experiments demonstrate that non-periglacial sorted nets can develop on any piece of unobstructed ground surface that has little or no gradient, if it bears a loose, discontinuous cover of pebble-sized stones and if these particles
Although medium-size and large villages are among the typical forms of settlement in the Great Plain, they have received little attention in settlement studies. An outline is provided on the development and main properties of this settlement studies
C 14 dating ; Climatic variation ; Fluvial processes ; Fluvial terrace ; Geochronology ; Land use ; Little ice age ; Palaeo-ecology ; Palynology ; Scotland ; United Kingdom
In Las Cuevas north of Azua 80 farmers were interviewed about their soils : 48% of them were aware of soil erosion, but had little interest in soil conservation. None of the farmers named more than six kinds of soil. Stoniness or soil depth were
In addition to the immigration caused by the employment market, a new type of immigration has developed over the last few years: poverty and refugee immigration. However, there has been little change in the regional distribution pattern
This article addresses the question of whether or not distinct glacial and non-glacial landforms can survive beneath ice sheets and ice caps with little or no morphological alteration. In glaciated areas, patches preserved under dry (cold)-based
towards patterns of territorial organization, where little cities and villas are involved in the economic progress of the more undeveloped rural areas. - (AAG)
The AA. describe rock glaciers and Matthes-age (Little Ice Age) moraines in the Sierra Nevada, and discuss their formation, extent, and climatological significance. They conclude for the Sierra that most valley-floor rock glaciers (i.e., tongue