Denison bibliography: all known references that deal with Denison.

"The Alaska Peninsula and Aleutian Islands form one of the conspicuously arcuate lines of volcanoes that border the Pacific Ocean. The name Aleutian Range is applied to this 1,600 mile long, narrow belt of peaks reaching from Mount Spurr opposite Anchorage to the island of Attu, close to the continent of Asia."

Powers, H. A., 1958, Alaska Peninsula-Aleutian Islands: in Williams, H., (ed.), Landscapes of Alaska, Los Angeles, CA, University of California Press, p. 61-75.

"NVEWS - a National Volcano Early Warning System - is being formulated by the Consortium of U.S. Volcano Observatories (CUSVO) to establish a proactive, fully integrated, national-scale monitoring effort that ensures the most threatening volcanoes in the United States are properly monitored in advance of the onset of unrest and at levels commensurate with the threats posed. Volcanic threat is the combination of hazards (the destructive natural phenomena produced by a volcano) and exposure (people and property at risk from the hazards)."

Ewert, J.W., Guffanti, Marianne, and Murray, T.L., 2005, An assessment of volcanic threat and monitoring capabilities in the United States: framework for a National Volcano Early Warning System NVEWS: U.S. Geological Survey Open-File Report OF 2005-1164, 62 p.
full-text PDF : 2.90 MB

Keller, A. S., and Reiser, H. N., 1959, Geology of the Mount Katmai area, Alaska: U.S. Geological Survey Bulletin B 1058-G, p. 261-298, 2 sheets, scale 1:250,000.
full-text PDF : 4 MB
plate 29 PDF : 32 MB
plate 32 PDF : 227 KB

"Quaternary Aleutian volcanism extends for over 2,500 km, from Buldir Island on the west to Mount Hayes on the east (fig. 1). This belt of volcanic activity lies immediately north of the Aleutian trench, a convergent boundary between the North American and Pacific lithospheric plates."

Motyka, R. J., Liss, S. A., Nye, C. J., and Moorman, M. A., 1993, Geothermal resources of the Aleutian Arc: Alaska Division of Geological & Geophysical Surveys Professional Report PR 0114, 17 p., 4 sheets, scale 1:1,000,000.
website with links to PDF and MrSID files

Volcanism and tectonism in the eastern Aleutian arc are controlled by the subduction of the Pacific plate beneath the North American plate. Worldwide earthquake data and data from local seismic networks in Cook Inlet, on the Alaska Peninsula and on Kodiak Island have defined the arcuate plate boundary and the Wadati-Benioff zone. A calc-alkaline volcanic arc of approximately 20 volcanic centers is well developed above the subduction zone.

Kienle, J., Swanson, S. E., and Pulpan, H., 1983, Magmatism and subduction in the eastern Aleutian Arc: in Shimozuru, D. and Yokoyama, I., (eds.), Arc volcanism: physics and tectonics, IAVCEI symposium, Proceedings, Tokyo and Hakone, Japan, Aug. 3l -Sept. 5, 1981, Tokyo, Terra Scientific Publishing Co., p. 191-224.

"From the first accounts of the explosion of Katmai Volcano, in Alaska, in June, 1912, it was clear that it must rank among the dozen greatest historic eruptions. Nevertheless, these early narratives contained no accounts of the events of the eruption itself, but were confined to the description of its effects at great distances."

Griggs, R. F., 1921, Our greatest national monument: The National Geographic Society completes its explorations in the Valley of Ten Thousand Smokes: National Geographic Magazine, v. 40, n. 3, p. 219-292.

"The borders of the Pacific Ocean are studded with volcanoes and the products of volcanic activity. The volcanoes are arranged in crudely arc-shaped groups, and most of the arcs are conves toward the ocean. In addition to the bordering arcs, the Pacific contains many individual volcanic islands and a few non-arcuate groups of volcanic islands, like the Hawaiian Islands. The curving chain of volcanoes from Kiska Island near the western end of the Aleutian Islands to Mt. Spurr on the mainland constitutes one of the Pacific volcanic arcs. This report is concerned with the past activity of the volcanoes of this arc, herein called the Aleutian arc."

Coats, R. R., Past volcanic activity in the Aleutian arc: U.S. Geological Survey Volcano Investigations Report 1, 18 p.
full-text PDF : 22.3 MB

Alaska Volcano Observatory, 1999, September-December 1999: Alaska Volcano Observatory Bimonthly Report, v. 11, n. 5 and 6, 51 p.
Part 1 PDF : 425 KB
Part 2 PDF : 1.7 MB
Part 3 PDF : 549 KB

"The Alaska Peninsula is a 775-km-long southwestward extension of mainland Alaska (fig. 1). The peninsula is about 225 km wide at the northeast end and narrows to less than 10 km near the southwest end. The southeast side is bordered by rugged mountains that rise sharply out of the Pacific Ocean. Many large bays and fiords cut the southeast shoreline. The northwest side, bordering Bristol Bay, is level and rarely more than 100 m above sea level; the coastline is nearly smooth and is broken by only a few large bays. At least 37 principal volcanic centers dot the length of the peninsula, and at least 30 have erupted during the Holocene (Miller and Richter, 1994). The present Aleutian volcanic arc overlies an early Mesozoic magmatic arc and a middle Tertiary volcanic arc."

Detterman, R. L., Case, J. E., Miller, J. W., Wilson, F. H., and Yount, M. E., 1996, Stratigraphic framework of the Alaska Peninsula: U.S. Geological Survey Bulletin B 1969-A, 74 p.
full-text PDF : 2.7 MB

"The feasibility of measureing volcanic deformation or monitoring deformation of active volcanoes using space-borne synthetic aperture radar (SAR) interferometry depends on the ability to maintain phase coherence over appropriate time intervals."

Lu, Z., and Freymueller, J. T., 1998, Synthetic aperture radar interferometry coherence analysis over Katmai volcano group, Alaska: Journal of Geophysical Research, v. 103, n. B12, p. 29,887-29,894.

A methodology to systematically rank volcanic threat was developed as the basis for prioritizing volcanoes for long-term hazards evaluations, monitoring, and mitigation activities.

Ewert, John, 2007, System for ranking relative threats of U.S. volcanoes: Natural Hazards Review, v. 8, n. 4, p. 112-124.

"On the afternoon of June 6, 1912, a volcanic eruption cloud rose 100,000 ft (32 km) into the sky above the Katmai region, 280 miles (450 km) southwest of Anchorage on the Alaska Peninsula (Fig. 1). Explosions were even heard in Cordova, over 370 miles (600 km) away from the Alaska Peninsula. Winds pushed the ash cloud east and within a few hours, ash from a huge volcanic eruption began to fall on Kodiak Island, approximately 100 miles (170 km) southeast of the volcano."

Adleman, Jennifer, 2002, The great eruption of 1912: National Park Service Alaska Park Science Winter 2002, Anchorage, AK, http://www.nps.gov/akso/AKScience2002.pdf, p. 4-11.
full-text PDF : 1.54 MB

Calc-alkaline volcanism and oceanic plate subduction are intimately linked in the eastern Aleutian arc. The volcanic arc is segmented: larger caldera-forming volcanic centers tend to be located near segment boundaries. Intrasegment volcanoes form smaller stratocones. Ten of the 22 volcanoes that make up the 540 km long volcanic front in the eastern Aleutian arc have erupted in recorded history and another six show hydrothermal activity.

Kienle, Juergen, and Swanson, S. E., 1983, Volcanism in the eastern Aleutian Arc: late Quaternary and Holocene centers, tectonic setting and petrology: Journal of Volcanology and Geothermal Research, v. 17, n. 1-4, p. 393-432.

Nye, C. J., Queen, Katherine, and McCarthy, A. M., 1998, Volcanoes of Alaska: Alaska Division of Geological & Geophysical Surveys Information Circular IC 0038, unpaged, 1 sheet, scale 1:4,000,000, available at http://www.dggs.dnr.state.ak.us/pubs/pubs?reqtype=citation&ID=7043 .
website with links to sheets in MrSID format