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Showing 321-337 of 337 results
  1. Le drame de l’Aral: sa complexité

    L’exemple de l’Aral est significatif d’un plan d’aménagement qui aurait pu donner de bons résultats si, à chaque étape, la conception, la décision,...
    René Létolle, Monique Mainguet in Aral
    Chapter 1993
  2. Sources of Suspended Matter

    The amount of water in the sea is 1.37 x 109 km3, which is ca. 94% of all water in the hydrosphere (van der Leeden 1975; Degens 1989). In rivers and...
    Chapter 1993
  3. Manganese Supply to the Ocean

    Manganese and other elements are supplied to the ocean from various sources and by various routes. Continental massifs and the Earth’s interior under...
    Chapter 1988
  4. How to Establish and Use World Budgets of Riverine Materials

    Average river water composition is often taken as a reference of surface water chemistry (Stumm and Morgan, 1981), and global river inputs have been...
    Chapter 1988
  5. USSR--Black, Azov, Caspian, and Aral Seas

    Local changes in the nature of near-shore environments are almost exclusively caused by man’s technical intervention near and, in some instances,...
    V. Zenkovich, Y. Shuysky in Artificial Structures and Shorelines
    Chapter 1988
  6. Manganese in Marine and Oceanic Sediments

    The study of manganese in oceanic bottom sediments, with which manganese nodules are genetically associated in one way or another, was started after...
    Chapter 1988
  7. Sources of Organic Matter in the Ocean

    Organic compounds, which are present in every drop of ocean water, in every particle of suspended material, have either been first created in the...
    Chapter 1984
  8. Geopedological Examples

    All maps but one illustrating this chapter were computer-produced on the original approximate scale of 1:1000000 which is the greatest possible...
    Chapter 1974
  9. P-CaCO3-MgCO3-SiO2 Deposition in Weakly Mineralized Basins of Arid Zones

    In the description of lithogenesis in humid zones (Vol. 2), brief reference was made to the specific features that distinguish the history of...
    N. M. Strakhov, S. I. Tomkeieff, J. E. Hemingway in Principles of Lithogenesis
    Chapter 1967
  10. Terrigenous Sedimentation in Arid Zones and its Features

    The concept of “deposits of arid zones” is generally associated with the idea of saline rocks, forming from more or less mineralized waters. This...
    N. M. Strakhov, S. I. Tomkeieff, J. E. Hemingway in Principles of Lithogenesis
    Chapter 1967
  11. Stages of Humid-Climate Lithogenesis

    The formation of sedimentary rocks may be reduced, in its most general form, to the following scheme: mobilization of substances by weathering of...
    N. M. Strakhov, S. I. Tomkeieff, J. E. Hemingway in Principles of Lithogenesis
    Chapter 1967
  12. Aral sea

    Rhodes W. Fairbridge in Geomorphology
    Reference work entry 1968
  13. Pluvial lakes

    Roger B. Morrison in Geomorphology
    Reference work entry 1968
  14. Aridity and Salinity

    The arid zones of the world are characterized by the minimum of annual precipitation and the maximum of heat and aridity. The precipitation in arid...
    P. C. Raheja in Salinity and Aridity
    Chapter 1966
  15. Grain-Size Sorting of Sandy Silts and Clayey Sediments of Various Facies Types

    One of the most characteristic features of deposits in humid zones is the more or less clearly defined sorting of material according to grain size....
    N. M. Strakhov, S. I. Tomkeieff, J. E. Hemingway in Principles of Lithogenesis
    Chapter 1967
  16. Distribution and Accumulation of Clastic and Clay Minerals in Deposits of Various Facies Types

    Since fragmental grains are characterized by specific mineralogical composition, as well as by size and specific gravity, grain-size sorting involves...
    N. M. Strakhov, S. I. Tomkeieff, J. E. Hemingway in Principles of Lithogenesis
    Chapter 1967
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