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THE UNITED STATES GEOLOGICAL SURVEY IN ALASKA:<br />

This report <strong>of</strong> .accomplhhments <strong>of</strong> the U.S. Geo-<br />

logical Survey in <strong>Alas</strong>ka during I981 mtalns summary<br />

and topical accounts <strong>of</strong> the results <strong>of</strong> studies on a wide<br />

range <strong>of</strong> topics <strong>of</strong> economic and scientific interest. In<br />

addition, many more detailed maps and reports are In-<br />

cluded in the lists <strong>of</strong> references cited for each article<br />

and in the appended compilations <strong>of</strong> 277 reports on Ai-<br />

aska published by the U.S. <strong>Geological</strong> Survey and <strong>of</strong><br />

103 reports by U.S. <strong>Geological</strong> Survey authors in<br />

various other scientific publications.<br />

Rre U.S. <strong>Geological</strong> Survey is engaged in many<br />

scientific investigations on various aspects <strong>of</strong> the land<br />

and water in <strong>Alas</strong>ka. Pmlucts <strong>of</strong> the Surveyt investl-<br />

gations include reports describing the phydcal findings<br />

and their significance. This volume includes summmy<br />

discussions, topid rcwults, and some nerratives <strong>of</strong> the<br />

course <strong>of</strong> the studles on just a few <strong>of</strong> the various<br />

Earth-science subjects currently being Investigated in<br />

<strong>Alas</strong>ka. POT the reader's convenience h peruslng<br />

reports that cover specific areas <strong>of</strong> interest, the<br />

articles are grouped by areas corresponding to the SIX<br />

regional geographic onshore subdivisions shown in fig-<br />

ure 1, by <strong>of</strong>fshore average, and by those article that<br />

cover more than one geographical region or are <strong>State</strong>-<br />

wide in scope. Index maps showing the study areas or<br />

sites discussed are Lncluded near the beginning <strong>of</strong> each<br />

subdivision (figs. 1, 5, 13, 19, 23, 44, 72, 90). An<br />

author index at the back <strong>of</strong> the volume should amkt in<br />

identifying and locating work by specific authors<br />

reported herein or in the appended compilations <strong>of</strong><br />

current reports on <strong>Alas</strong>ka by U.S. <strong>Geological</strong> Survey<br />

authors and their associates.<br />

(Ffgure 1 shows the quadrangles and regions<br />

referred to in this volume)<br />

ACCOMPLlSHMENTS DURING 1981<br />

Warren L. Coonrad and Raymond 1. Elliott, Editors<br />

rangles (fig. 2) have been completed. These maps are<br />

the major summary prdcts <strong>of</strong> the U.S. Geologlcal<br />

Survey's Branch <strong>of</strong> <strong>Alas</strong>kan Geology's telegeologlc<br />

research effort, funded under the auspices <strong>of</strong> the <strong>Alas</strong>-<br />

kan Mineral Resource Assessment Program. Synthesfs<br />

<strong>of</strong> the data compiled from these studies indicates that<br />

the major features oommonly observable on Landsat<br />

images <strong>of</strong> <strong>Alas</strong>ka are lineaments, circular and arcuate<br />

features, and anomalously colored areas.<br />

Lineaments<br />

Lineaments observed in <strong>Alas</strong>ka can gener* be<br />

divided into three groups on the basis <strong>of</strong> scale: (1)<br />

<strong>State</strong>wide Uneament trends (northwest, north-south,<br />

northeast, and east-west; see Lathram and molds,<br />

1977), corresponding to the regmatic shear pattern,<br />

that not only transect tectonic and stratigraphic<br />

boundaties but also coincide with these boundaries in<br />

places; (2) regional trends, such as for the set <strong>of</strong> lin-<br />

eaments along the DenaU fault in the Talkeetna quad-<br />

rangle (Steele land Albert, 1978a) or along the Coast<br />

Range megallneament in the Ke tchikan quadrangle;<br />

and (3) local trends that ere commonly restricted to<br />

specific terranes and various geologic phenomena, or<br />

to structures caused by unknown (local) tectonlo<br />

events.<br />

That many lineaments (generally from several<br />

Wlorneters to several tens <strong>of</strong> kllometers long) which<br />

make up sets <strong>of</strong> subparallel to parellel Uneaments<br />

detected on Landset images may reflect relatively<br />

narrow (generay less than 10 krn wide) zones <strong>of</strong><br />

associated(?) fractures is particularly well shown in<br />

the Ketch- quadrangle (Steele and Albert, 1978b;<br />

Le Compte, 1981b). Only a few (1-10 percent) <strong>of</strong> the<br />

Uneaments there are faults, although many faults that<br />

are mappable at 1:250,000 scale can be detected on<br />

Landsat images. Lineament extensions beyond the<br />

terminations <strong>of</strong> the many faults mapped by field<br />

methods are also evident in places.<br />

Circular and Arcuate Features<br />

8nmlwrgat~t~e~~~lnAlngkn Circular and arcuate features detected on Land-<br />

sat Images <strong>of</strong> <strong>Alas</strong>ka can generally be divided into two<br />

BY Jam- R CMnpte, Willhrn Cltntaa b ebi and goups. The first group consists <strong>of</strong> circular and arcu-<br />

lUairnRD.Albeet ate features larger than 50 km in diameter, such as<br />

several circular features Ln the eastern Brooks hnge<br />

Landsat-image interpretation and (or) Landsat- (Le Compte, 1970a); few logical explanations have<br />

feature map for 27 Aleakan 1:250,000-scale quad- been found for features this Large. The second group

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