Ridges as Indicators of Terrane Differences - Remote Sensing Application - Completely Remote Sensing, GPS, and GPS Tutorial
Ridges as Indicators of Terrane Differences

Earlier, we introduced the idea of ridge density (defined as total length of ridges per unit area). For the study, I produced a regional map of ridges from the 1:250,000 topographic sheet, from which I calculated densities using a computer program. This list shows that densities vary by a factor of almost two among the major terranes in the Klamaths:

Variations in ridge density for the Klamath terranes.

This density value relates to several factors, chief being the "fineness" of the drainage network.

From this map, I plotted the orientations of ridges (normalized to lengths) for the entire region:

Frequency distribution of different ridge orientations, for the entire Klamaths.

Then, using the above-mentioned program, in which the ridge data are entered as points on a digital plotting board that converts them to lines, their average trend directions were then calculated. These orientations of the ridges for any chosen area (such as a terrane or fraction thereof) were then plotted in rose diagrams similar to those shown above for the Elk and Sixes Rivers terranes. Below is a map, on which is drawn the most common orientation interval (in 5° units) in red and the second most common in blue.

Map of Klamath terranes on which are plotted the two most frequent orientations of ridges.

The prevailing direction for terranes including and east of the Yolla Bolly terrane is north-north-east, in keeping with the regional plot just shown. But, in the Elk and Sixes River terranes that direction becomes northwest.

What might account for this shift in trends? This next diagram is my speculation:

(C-4)  Model explaining possible cause of variations in ridge orientations as a function of the sequential docking of individual terranes.

In upper panel I, a new terrane smashes into the continental craton along a subduction line of a given geometry (including orientation). As the terrane slides under (or, it can override the continent), it takes on a fabric whose principal direction(s) is governed by the stress field imposed during emplacement. Now, in panel II, the subduction zone location and geometry have changed and a somewhat different fabric orientation results. In panel III, a new subduction zone (bounded by a transform fault [not shown]) adopts a notably shifted orientation and this passes on to the docking terrane. Then, as erosive processes gradually carve out topographic expressions for the terrane group, streams, whose paths tend to be controlled by the underlying structural fabric, produce valleys and intervening divides that reveal the effects of the stress fields that gave rise to the noted preferred orientations.

Summary of the Klamath Terrane Project

The foregoing report on the writer's research into terrane/terrain interrelations is, as stated, incomplete. But, it warrants several conclusions:

  1. Real differences in geomorphic expression exist among the terranes. We can separate the Klamath terranes best by ridge (and stream) density differences.
  2. Variations in hypsometric interval (curve) and related parameters among terranes may indicate relative resistance to erosion. That resistance depends on rock types and locations within the Klamath "dome".
  3. Principal directions of ridge orientations seemingly differ in individual (or clusters of) terranes. This is probably structurally controlled and could relate to subduction/accretion geometry.
  4. The principal value of space imagery is that it provides a visual overview of differences in landforms/topography expression. It helps to pinpoint areas for quantitative analysis by conventional morphometric methods.
  5. We require stereo imagery for elevation-based morphometry and structural pattern analysis. SPOT-type stereo imagery reduces the illumination bias.

The bottom line: In this study, most of the useful discriminatory data were extracted from topographic maps and, to a lesser extent, some aerial photographs. Satellite remote Sensing has a limited but positive role in the analysis of the Klamaths in particular and similar landforms in general, by virtue of its excellence in creating synoptic images that highlight regional relationships that we can interpret visually. This role will increase significantly as high resolution stereo becomes commonplace from space sensors. Ultimately, this imagery will lead to the topological expression of surfaces in a quantitative mode that will prove its worth again, as it has from aerial photography, as a prime approach to geomorphic characterization.

Source: http://rst.gsfc.nasa.gov