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Vol. 11, No. 9 A Publication of the Geological Society of America September 2001 INSIDE " Stream Piracy Revisited: A Groundwater-Sapping Solution, p. 4 Darryll T. Pederson " Northeastern Section Meeting, p. 22 " Field Forum Scheduled, p. 43 Contents GSA TODAY (ISSN 1052-5173) is published monthly by The Geological Vol. 11, No. 9 September 2001 Society of America, Inc., with offices at 3300 Penrose Place, Boulder, Colorado. Mailing address: P.O. Box 9140, Boulder, CO 80301-9140, U.S.A. Periodicals postage paid at Boulder, Colorado, and at additional mailing offices. Postmaster: Send address changes to GSA Today, Member Services, P.O. Box 9140, Boulder, CO 80301-9140. science article Copyright © 2001, The Geological Society of America, Inc. (GSA). All rights 4 reserved. Copyright not claimed on content prepared wholly by U.S. Stream Piracy Revisited: A Groundwater-Sapping Solution . government employees within scope of their employment. Individual scientists Darryll T. 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Pederson, p. 4–10. 10% Postconsumer GSA TODAY, SEPTEMBER 2001 3 Darryll T. Pederson, Department of energy to the system as increased logic settings, such as in a delta, stream Geosciences, University of Nebraska, recharge causes groundwater levels to piracy is a cyclic event. The final act of Lincoln, NE 68588-0340, USA rise, accelerating stream piracy. stream piracy is likely a rapid event that should be reflected as such in the geo- INTRODUCTION logic record. Understanding the mecha- The term stream piracy brings to mind nisms for stream piracy can lead to bet- ABSTRACT an action of forcible taking, leaving the ter understanding of the geologic record. Stream piracy describes a water-diver- helpless and plundered river poorer for Recognition that stream piracy has sion event during which water from one the experience—a takeoff on stories of occurred in the past is commonly based stream is captured by another stream the pirates of old. In an ironic sense, on observations such as barbed tribu- with a lower base level. Its past occur- two schools of thought are claiming vil- taries, dry valleys, beheaded streams, rence is recognized by unusual patterns lain status. Lane (1899) thought the term and elbows of capture. A marked of drainage, changes in accumulating too violent and sudden, and he used change of composition of accumulating sediment, and cyclic patterns of sediment “stream capture” to describe a ground- sediment in deltas, sedimentary basins, deposition. Stream piracy has been re- water-sapping–driven event, which he terraces, and/or biotic distributions also ported on all time and size scales, but its envisioned to be less dramatic and to be may signify upstream piracy (Bishop, mechanisms are controversial. Some the common mechanism for stream 1995; Pissart et al., 1997; Mather et al., researchers conclude that stream piracy piracy. Crosby (1937) took issue with 2000; Johnsson, 1999). Recognition that is a rare event and happens only on Lane (1899 and later papers) and argued piracy is happening now is based on small scales; this is based on a recogni- that surface water is the principal agent observed higher erosion rates for streams tion that surface-water energy decreases of stream piracy in most settings. This with steeper gradients on one side of a near divides and the belief that ground- set up a debate on the relative roles of drainage divide relative to the other, water-sapping processes decrease in surface-water erosion and groundwater- with the steeper gradient stream captur- effectiveness near divides and are not sapping erosion that persists today. This ing the headwaters of the lower gradient effective in rock and cohesive sediment. paper contends that groundwater-flow stream (Bates, 1961; Vogt, 1991; Ries et In contrast, numerous studies show that patterns and groundwater-sapping pro- al., 1998). As variants, development of groundwater-sapping is effective in rock cesses are important in most cases of karst aquifers can lead to underground and cohesive sediment, focused by the stream piracy, and the final act of piracy capture of rivers over time, such as the intersection of the extending channel can be rapid because of the developing recognition of loss of upper Danube with the water table, and effective in geometry. There is a predictable imprint flows (Hötzl, 1996), and cyclic develop- hillslope processes. Further, destruction of groundwater flow, and groundwater ment of lobes on the Holocene Missis- of evidence by surface water is the rea- sapping is effective at all scales and in sippi River delta is modulated by stream son for the general lack of recognition all geologic material. capture (Roberts, 1997). of groundwater-sapping effects. I argue The issue of stream piracy is more While the identity of the villain (mech- that the persistence of groundwater-flow than an academic discussion because it anism) remains controversial, there are systems, coupled with the evolving geo- is an important geologic process—past common elements in stream piracy metry as a pirating stream approaches a and present. Sediment-deposition pat- regardless of the erosion process. To divide, can sustain