Geological Setting at White Mountain, Utah - Remote Sensing Application - Completely GPS, GIS dan Remote Sensing tutorial -
Geological Setting at White Mountain, Utah

We now investigate a superb illustration of this last situation. Here is a Landsat Thematic Mapper (TM) subscene of an area in southwestern Utah:

A Landsat TM natural color subscene with the altered zone at White Mountain near the center.

The subscene, about 35 km (22 mi) on a side, resides within Beaver Co., Utah. It is about 24 km (15 mi) west of the small town of Milford and 64 km (40 mi) north of Cedar City, gateway to Zion National Park to its south. The physiographic setting places this area well within the Basin and Range Province, which, geologically, is a series of generally north-south trending mountain blocks that are upfaulted between downdropped valleys or basins. The area lies within the High Desert country of the U.S. Southwest. On the left side of the image is a part of the Wah Wah Range, a typical block-fault mountain system. To the right are a group of isolated hills composed of eroded volcanic flows and small outliers, such as White Mountain (gray roundish landform near the image center), of Paleozoic sedimentary rocks. Lowlands within the scene extend into basins filled with eroded debris from the uplands, including alluvial wash that form sloping aprons. Distinguish this terrain from the clouds and their shadows. Just to the left of White Mountain is an elongated (east-west) area, about 8 km (5 mi) long, characterized in this false color version (Bands 2,3,4) by blotchy orange-brown to tan tones. These colors are a classic expression of gossan staining associated with a mineralized zone.

This is an enlargement of the scene above, but produced as a color ratio composite (the altered zone still has a brownish-yellow tone):

Color ratio composite of White Mountain.

Here, we show a part of this area in a natural color aerial photo (somewhat overly red-brown in its printing) obtained during the NASA Aircraft Mission 340 flown for the writer (NMS) in 1976 (see page 2-3 for details).

Near natural color aerial photo of part of the alteration at White Mountain, acquired during the NASA aircraft overflight.

In a ground photo, we see the same area consists of gentle rolling terrain covered sporadically by cedar and sagebrush.

 Ground photo showing both iron and sulphate alteration patches on the volcanic rocks and soil at the surface.

In the satellite image, this vegetation does not stand out as blotches of red, suggesting that cedar has a weak reflectance response in the near-IR.

A published geologic map (Stringham and Brooke, 1962) of this area indicates a wide variety of alteration types have developed here. Their report states that mineralization consists of pyrite and chalcopyrite (copper-bearing). The latter is not of sufficient grade (amounts) for mining. A group of volcanic rocks called andesites show the most alteration. After they flowed into this region and cooled, volcanic gases and hot solutions modified some of them. One alteration type is kaolinite, a common clay mineral used in ceramics. It is light brownish-white at this location. A second, light-gray mineral is alunite, a hydrous potassium aluminum sulphate. The principal alteration mineral is hematite, the anhydrous iron oxide, which is medium grayish-red. Minor amounts of limonite are present, but the yellow-brown color of the space image corresponds mainly to altered hematite rather than the similar gossan. Very white areas of siliceous sinter are scattered about and a few areas contain natural sulphur, which comes from the breakdown of the original sulphides. In the ground-based photograph above, the light patch coincides with mainly a kaolinite-alunite (k/a) mix, and the reddish area is hematitic staining on weathered volcanics. To appreciate their general distribution in this subscene, examine the map below, a simplified version of the published map, which didn't reproduce well on this Web Page. This map can be printed for ease of reference in studying the images below.

Geologic map, adapted from Stringham and Brooke, of the White Mountain alteration zones.

We now consider a set of Landsat images we processed to illustrate how to apply remote sensing data effectively in mineral exploration. Suppose, to start, that we are modern prospectors, searching for some metal (gold is the obvious choice, but copper is often the more likely find). If we had chosen a large region in which to hunt, we would be grateful for Landsat imagery that encompasses many thousands of square miles. Even in a full scene, the anomalous color in the White Mountain area (as this alteration district is known) would grab our attention because it is typical of a gossan signature. Our first logical step would be to zoom in on our image processor to the immediate area showing this signature in a natural color (TM Bands 1-3) rendition.

White Mountain TM subscene rendered in approximate natural color.

Dark areas in the subscene relate mainly to the volcanics. On the left side, the map shows that these are basalts (an almost blackish rock, typical of Hawaiian volcanoes and of the Snake River volcanic plains of Idaho). Those dark areas at the top and bottom are somewhat lighter (but still dark grayish-brown) andesites, which are typical of volcanoes in the western U.S., such as Mt. St. Helens. White Mountain stands out on the right in light bluish-gray tones. It contains a radial pattern that corresponds to furrowed gullies draining down from its central peak. The main alteration zones make up a pattern with an east-west branch that meets a north-south segment on the left. Most of this alteration is displayed in the yellow-browns seen in the regional subscene. Other zones are much lighter (sort of tan) in this image. These two principal zonal types broadly match the hematite and k/a areas on the generalized map shown above. Areas on that map that we identified as alluvium (soil and loose surface debris) show up in several variant colors in the subscene. Those with a color similar to the hematite are alluvial deposits, derived from the altered hematitic zones. An equivalent subscene made from Bands 2,3,4 (not reproduced here) contains very little discrete red patches, confirming the sparsity of active, reflectant vegetation.