Submitted by dylan on Wed, 2006-06-14 00:06.
Submitted by dylan on Fri, 2006-02-03 04:14.
Submitted by dylan on Fri, 2006-02-03 03:37.
Depicting the relative density of sampling can be an interesting task, especially when the points are highly clustered and sparse. Three simple operations that can reveal subtle patterns in the spatial distribution of sample points were explored:
Submitted by dylan on Thu, 2006-02-02 22:32.
Raw LiDAR data is so detailed that localized flow routing algorithms often fail to produce meaningful results. The terraflow algorithm is one such method that appears to work well on such massive grid objects (Homepage).
Submitted by dylan on Mon, 2006-01-02 18:57.
Submitted by dylan on Wed, 2005-09-28 23:12.
More often than not geographic data come in a format that is essentially two-dimensional: i.e. raster grids and vector points, lines, and areas with only (x,y) style coordinates.
Submitted by dylan on Mon, 2005-08-22 22:23.
Submitted by dylan on Thu, 2005-08-11 00:10.
100 iterations of mass removal based on preferential flow of water as calculated by r.topidx in GRASS. Notice how landform is cutdown most in stream channels, least at the ridges. The basins between ridges appear to "fill" with sediment near the 50th iteration as the entire landform is lowered to sea level (0m). Absolute change in elevation is visble in the elevation profiles below. Example GRASS commands below. Here is a link to a movie, containing all 100 iterations.
Submitted by dylan on Tue, 2005-07-19 21:31.
Submitted by dylan on Sun, 2005-06-26 19:20.
There are few opportunities to see an Oxisol outside of the tropics. The Ione soil is one example of an Oxisol formed in a tropical paleoclimate, protected by a layer of ironstone, and later exposed during recent times. This soil is thought to have originally formed from highly weathered alluvium washed down from the original Sierra Nevada (Eocene age) and deposited in a low energy environment. Subsequent uplift coupled with repeated wetting and drying cycles transformed plinthite near the surface into ironstone. This extremely hard surface of iron stone protected the underlying material from erosion, and was eventually buried by cobbly alluvium of similar age to that of the China Hat formation. Later uplift of the Sierra Nevada and the resulting erosion of overlying material re-exposed the Ione formation materials. Recent colluvial deposits have created a considerable layer of overburden, masking the properties of the original Ione material near the surface. The subsurface of this polygenic soil contained oxic horizons: a horizon with less than 10% weatherable minerals in the sand fraction and a high content of low activity clays such as kaolinite (Buol et al., 2003). In addition, redoximorphic features such as iron concretions and nodules were found throughout the oxic horizons. Concentrations of hematite, goethite, and plinthite were also visible in the oxic horizons (See Figure 1). For the classification of Oxisols, an otherwise xeric soil moisture regime is recognized as ustic in the Keys To Soil Taxonomy 9th edition. This characteristic coupled with a base saturation greater than 35% is recognized at the great group level classification of this soil: an Eutroustox.