PE&RS December 1996

VOLUME 62, NUMBER 12
PHOTOGRAMMETRIC ENGINEERING & REMOTE SENSING
JOURNAL OF THE AMERICAN SOCIETY FOR PHOTOGRAMMETRY AND REMOTE SENSING

Peer-Reviewed Articles

1353 Revised Mapping of Lava Flows on Mount Etna, Sicily
Michael Abrams, Remo Bianchi, and Dave Pieri

Abstract
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Reports a differing approach used to determine relative ages of Etnean lava flows. Multispectral image data were acquired from aircraft overflights of Etna in 1991. The Thematic Mapper Simulator instrument obtained 12 channels of data in the visible through thermal infrared wavelength regions. Supervised classification of these data allowed the authors to group Etnean flows into age groups based on their spectral properties. About 90% of the classification agrees with the mapped lava flow ages. Results generally support the paleomagnetic age determinations for flow ages that disagree with the mapped ages. In addition, several areas were remapped, correcting errors on the published map. 

1361 The Use of Satellite and Airborne Imagery to Inventory Outlet Glaciers of the Southern Patagonia Icefield, South America
M. Aniya, H. Sato, R. Naruse, P. Skvarca, and G. Casassa

Abstract
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A Landsat TM mosaic of the Southern Patagonia Icefield (SPI), S America, was utilized as an image base map to inventory its outlet glaciers. Employing a supervised classification using Landsat TM bands 1, 4, and 5, glacier drainage basins were divided into accumulation and ablation areas, thereby determining the position of the transient snow line (TSL). After comparing with existing data, it was found that the TSL could be taken, for practical purposes, as the equilibrium line (EL). The position of the TSL was then compared with topographic maps, where available, to determine the equilibrium line altitude (ELA). Altogether, 11 parameters relating primarily to glacier morphology were inventoried. Pio XI Glacier (1265 km"SUP 2" ) is found to be the largest outlet glacier in S America, and may also be its longest. The average accumulation area ratio of 0.75 is larger than those of the Northern Patagonia Icefield and European glaciers. All but two outlet glaciers calve into fjords or pro-glacial lakes. 

1371 Applications of Spectral Stratigraphy to Upper Cretaceous and Tertiary Rocks in Southern Mexico: Tertiary Graben Control on Volcanism
Pamela E. Jansma and Harold R. Lang

Abstract
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Seven spectral stratigraphic units, each of which corresponds to a distinct lithostratigraphic unit, were delineated. Five consist of terrestrial Upper Cretaceous and Tertiary siliciclastic, volcanic, and volcaniclastic rocks; one contains Mesozoic marine rocks; and one corresponds to Quaternary alluvium. A previously undocumented NNW-trending Tertiary graben was identified in which 2000 m of lower Tertiary volcanic rocks accumulated, suggesting volcanism coeval with graben subsidence during WSW-ENE regional extension in the early Tertiary. Overlap of the western-graben bounding fault by slightly younger lower Tertiary rocks suggests subsidence ended by the close of the early Tertiary. Continued volcanism within the graben during the late Tertiary indicates a long-lived volcanic source region within the sub- surface of the NNW-trending structure and localization of younger magmatic activity within a pre- existing zone of crustal weakness. 

1379 Remote Mineralogic and Lithologic Mapping of the Ice River Alkaline Complex, British Columbia, Canada, Using AVIRIS Data
Timothy L. Bowers and Lawrence C. Rowan

Abstract
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The authors examined the alkaline complex and adjacent country rocks using Airborne Visible-Infrared Imaging Spectrometer (AVIRIS) data. This technique models each pixel spectrum in an AVIRIS image as a linear combination of unique endmember spectra. Endmember spectra were selected from well-exposed and spectrally distinct mineralogic units, vegetation, and snow. Four of the endmembers reflect mineralogic variations within the McKay group in the study area, and may represent lateral and vertical variations of sedimentary or metamorphic facies. Otherwise, the resultant spatial distribution of endmembers shows generally close agreement with the published geologic map, although, in several places, the image-map is more accurate than the published map. 

1387 Waste Site Characterization through Digital Analysis of Historical Aerial Photographs
Paul Pope, Ed Van Eeckhout, and Cheryl Rover

Abstract
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Historical aerial photographs have been used to provide a physical history and preliminary mapping information for characterizing a Department of Energy waste burial site at Los Alamos National Laboratory, New Mexico. The coregistered images were studied individually (and in comparison with each other) to identify features which were indicative of human activity at the site and to provide a physical history of natural and human induced changes. The coregistered images were imported to a geographic information system and geographically coded to a common coordinate system. The geographic information system was used to extract the boundaries of features such as suspected trenches and disturbed soil. This preliminary analysis forms a basis for planning and comparing the results from other remote sensing and geophysical surveys which will be used to improve the characterization of the waste site. 

1397 Use of Digital Image Analysis and GIS to Assess Regional Soil Compaction Risk
M.L. Bober, D. Wood, and R.A. McBride

Abstract
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A soil compaction risk study was undertaken in an agricultural region of southern Ontario, Canada. The objective was to identify land areas that are highly susceptible to traffic- and tillage- induced soil compaction given their soil mechanical properties and their use for intensive row crop production (including continuous corn monoculturing) under local climatic conditions. Spatial information on the distribution of various agricultural crops in relation to the major soil associations was acquired using an integrated approach involving digital image analysis and GIS. Error matrices showed that the user's accuracy of the crop over classification at the field level was better than 80% for all major crop types, and the correspondence to census information was equally good. The soil associations most vulnerable to compaction in three local municipalities where row crops dominate included about 75 km"SUP 2" of medium-textured soils. The silty clay loam tills were identified as being particularly at risk due to observed cropping practices.