1 / 14

Soils and Geologic Time

Soils and Geologic Time. soil = f (time, …) Soil formation can be a slow process Not always observable on human time scale Need appreciation of geologic time scale. Soil Age and Geomorphic Surfaces. Soil age is dictated by age of “ geomorphic surface ” - Erosional Constructional

sauda
Télécharger la présentation

Soils and Geologic Time

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript

  1. Soils and Geologic Time soil = f (time, …) Soil formation can be a slow process Not always observable on human time scale Need appreciation of geologic time scale

  2. Soil Age and Geomorphic Surfaces Soil age is dictated by age of “geomorphic surface” - Erosional Constructional Geological maps Soil = f (age of geomorphic surface, …)

  3. On-Going Erosional Geomorphic Surfaces: Age ~ Residence Time = soil (kg or cm)/soil input or loss (kg or cm) ≈ soil / soil production rate

  4. FROG HOLLOW, AUSTRALIA

  5. EROSIONAL GEOMORPHIC SURFACES Soil Thickness ~ Hillslope Curvature

  6. SOME GEOMORPHIC SURFACES NO LONGER EXPERIENCE SIGNIFICANT EROSION OR DEPOSTION Soil Age = Elapsed Time Since Erosion/Deposition Stopped Terrace ages range from ~ 102 to > 1.5 Ma

  7. Relative Geological Time One of great intellectual developments of last millenium 4 Eras of time related to major biological events or changes - Precambrian Neary 4 billion years of time Evolution of bacteria and simple forms of life that still dominate our planet Paleozoic Cambrian “explosion” of life Evolution of land plants Ended with large extinction Mesozoic Age of dinasaurs Ended with extinction Cenozoic Age of mammals Tertiary vs. Quaternary Now experiencing great extinction event

  8. Geomophic Surfaces and Soil Age Earth’s surface is very dynamic (on geological time scale) Much, or most, of earth’s surface has been altered inQuaternary period, and much of earth surface is Holocene in age Glaciation Loess deposition Fluvial deposition Erosion Pedology is therefore greatly concerned with Pleistocene and Holocene epochs

  9. Relative Geological Time Scale

  10. The Significance of Humans in Relative Time

  11. Numerical Geological Time Truly developed in 20th century with advances in chemistry and the devolopment of radioactive “clocks” Variety of clocks continues to grow and is now especially useful in dating geomorphic surfaces

  12. Soils and the Recognition of the Immensity of Geological Time Jame Hutton and his paradox of the soil

  13. Hutton’s Paradox Background of Hutton Viewed as originator of modern geology Yet he a unlikely candidate: conventional Christian, gentleman farmer The Paradox World is adapted to to the purpose of man, which must include soils Hutton realized soil formation requires destruction of rocks, lowering of land surface, and ultimate loss of land fertilty How can a ‘well balanced’ earth have both soil and denudation? Hutton recognized that regenerative forces of uplift and volanism are required The slowness of this process, combined with rocks in every stage of the cycle invked enormous magnitudes of time

  14. Geological Unconformity that Contributed to Huttons Recognition of Geological Time Hutton: If the succession of worlds is established in the system of nature…the result of our present enquiry is that we find no vestige of a beginning, no prospect of an end. John Playfair: We felt ourselves carried back to the time when the schitus on which we stodd was yeat at the bottom of the sea…The mind seemed to grow giddy by looking so far back into the abyss of time.

More Related