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  1. Loess - Wikipedia

    Loess is a periglacial or aeolian (windborne) sediment, defined as an accumulation of 20% or less of clay with a balance of roughly equal parts sand and silt (with a typical grain size from 20 to …

  2. Loess | Wind-Deposited Sediment & Soil Formation | Britannica

    Loess, an unstratified, geologically recent deposit of silty or loamy material that is usually buff or yellowish brown in colour and is chiefly deposited by the wind.

  3. Local regression - Wikipedia

    LOESS is a multivariate smoother, able to handle spatial data with two (or more) predictor variables, and uses (by default) local quadratic fitting. Both LOWESS and LOESS are …

  4. Loess - National Geographic Society

    Jul 3, 2024 · In some parts of the world, windblown dust and silt blanket the land. This layer of fine, mineral-rich material is called loess.

  5. The Geology of Loess: A Detailed Analysis - numberanalytics.com

    May 30, 2025 · This in-depth article examines the geological processes that shape loess, its characteristics, and its far-reaching implications for the environment and human societies.

  6. LOESS Definition & Meaning - Merriam-Webster

    The meaning of LOESS is an unstratified usually buff to yellowish brown loamy deposit found in North America, Europe, and Asia and believed to be chiefly deposited by the wind.

  7. Loess and Paleosols - National Centers for Environmental …

    Dec 5, 2022 · Loess are silt-sized particles deposited on the Earth's surface by winds. Extensive loess deposits formed during the Ice Ages in areas bordering large, continental glaciers.

  8. Loess Explained

    What is a Loess? A loess is a clastic, predominantly silt -sized sediment that is formed by the accumulation of wind-blown dust.

  9. Loess genesis and worldwide distribution

    Feb 1, 2020 · Loess formation generally involves the four main stages of production, deflation, transportation, and deposition of loess particles. Traditionally, loesses are classified as glacial, …

  10. Loess - Age, Origin, Deposits | Britannica

    The mineral constituents of loess (quartz and feldspar, for example) are reduced to minute particles by weathering action, principally in semiarid and arid regions.