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  • The pedological development in a sandy loamy soil in Northern Jutland, Denmark, has been described. The profile was strongly leached, a clay migration has taken place, and a marked Bt-horizon was developed. The Bt-horizon was later slightly
  • degradated. In the eluvial horizon to this Bt-horizon a podzol has been formed, in which a new clay migration has taken place. (Ed.).
  • The determination of former shoreline positions in areas of large tidal range, with examples taken mainly from Scotland
  • Photographs taken in 1892-1893 of the United States-Mexico international boundary monuments in the Chihuahuan and Sonoran Deserts were compared to repeat photos taken 90 years later as a way of determining vegetation changes. Many areas
  • method and the manner of the dead and the development work, in the influence of the tectonics must be taken into the consideration. For the estimation of the mining safety also the knowledge about the fracture tectonics developed in the planned mining
  • section must be taken in consideration. (HL).
  • taken here is to summarize the salient ideas embodied in various theories.
  • Territorial and offspring retention and other behavioral traits must be taken into consideration in ungulate management in fragile mountain zones. - (D. W. Gade).
  • Deuterium, tritium and activity in a snow core taken on the summit of Mont Blanc (French Alps). Determination of the accumulation rate
  • , which are taken, mostly from agricultural areas, are given to illustrate these methods.
  • This paper deals with eolian deposits and dust storms in Greece. Statistics on episodes with atmospheric dust are extracted from meteorological data taken at a number of Greek weather stations. In addition eolian dust of probably Saharan origin
  • Induration of soft samples taken without disturbance allows to cut well-orientated thin sections. Their analysis goes further than the results of classical studies in Quaternary stratigraphy such as palynology, organic content, heavy minerals
  • In this report, a larger scale view will be taken, beginning with an examination of the international climate of opinion which is currently attempting to stimulate research in applied and applicable climatology at all levels, discussing some recent
  • If the host population is taken to be a dynamic variable (rather than constant, as conventionally assumed), a wider understanding of the population biology of infections diseases emerges. In this first part of a two-part article, mathematical models
  • Tibet and north of the Himalayan Range. Rather, these conglomerate beds represent a direct sedimentary response both to the uplift of the Himalayan Range and to the extensional tectonics which have taken place since Plio-Pleistocene times and which
  • The authors measured hydraulic conductivity (saturated and unsaturated) on 127 soil cores, which were taken in different horizons of a wide variety of Belgian soil series. The hot air method and the crust method were combined to obtain the complete
  • . For the experimental slope of Skrajna Turnia photographs were taken and cartographic interpretation was made. To the slope surface certain morphological, genetic and dynamic features were ascribed. Point of measurement of Quick and slow mass movement were established
  • In Hungary approximatively 600000h are taken up by sodic soils. For the past hundred years a number of specialists have investigated them. This study aims to show that quantitative values /DTG, TG/ obtained by the derivatographic methods can
  • of this variety in making relevant extrapolations from the time scale of experiments to that of natural deformations. The particular case of olivine-rich rocks, of interest in mantle studies, is taken up in more detail, with a critical survey of available
  • Data of January, April, July, and October are taken to represent the four seasons in this analysis. For the 100 MB surface, the latitudinal deviation and amplitude at both high and low latitudes change greatly in a year. The maximum deviation