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WRRCTR No.189 Geology and hydrogeology of the island of Pohnpei, Federated States of Micronesia

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dc.contributor.author Spengler, Steven R.
dc.contributor.author Peterson, Frank L.
dc.contributor.author Mink, John F.
dc.date.accessioned 2008-07-17T22:31:11Z
dc.date.available 2008-07-17T22:31:11Z
dc.date.issued 1991-03
dc.identifier.citation Spengler SR, Peterson FL, Mink JF. 1991. Geology and hydrogeology of the island of Pohnpei, Federated States of Micronesia. Honolulu (HI): Water Resources Research Center, University of Hawaii at Manoa. WRRC technical report, 189.
dc.identifier.uri http://hdl.handle.net/10125/1977
dc.description.abstract The island of Pohnpei is the eroded remnant of a large shield volcano that was built up from the surrounding sea floor by the repeated eruption of mildly alkalic lava. The main island is composed entirely of volcanic material erupted episodically over the last 9 million yr. The volcanic construction of Pohnpei can be divided into three stages-of activity. The first was a shield-building phase dominated by the frequent eruption of alkali olivine basalt, which was followed after an eruptive hiatus of roughly 1.5 million yr by sporadic volcanic activity dominated by basanitic and hawaiitic composition lavas (Awak volcanic stage). Shortly after the end of the shield-building stage, a large-scale landslide event is postulated to have removed much of the northwestern portion of the original shield volcano. The final stage of volcanic activity (Kupwuriso volcanic stage) produced voluminous flows of undersaturated lavas, which blanketed much of the southern half of the island. The thick, massive, low-permeability post-shield-building lavas of the Awak and Kupwuriso volcanic stages dominate the present-day geomorphology and hydrogeology of the island. Due to regional subsidence and sea-level rise (roughly 5.5 m over the last 6,000 yr), Pohnpei lacks extensive coastal plains of sedimentary material around its perimeter. Instead, volcanic rock and fringing mangrove swamps occur along the coastline around much of the island. Rainfall on the island is abundant year-round and ranges from 400 cm/yr along the coastline to an estimated high of 900 cm/yr in the island's interior. A high runoff-rainfall ratio (0.67) is estimated for the island's river basins. An evapotranspiration rate of 140 cm/yr is estimated for the island. These values lead to an estimated islandwide groundwater recharge of 600 to 750 million liters per day. Groundwater development on Pohnpei has been limited mainly to areas in the northern part of the island in and around the town of Kolonia and Palikir, the new Federated States of Micronesia capital site. Wells in the Kolonia area exploit local unconformities between flow units of the late-stage volcanics and the unconformity between these volcanics and the underlying shield-building lavas. Somewhat more productive wells located in the Palikir area exploit relatively unweathered shield-building lavas. Groundwater development in the northern half of the island is hindered by the low permeability of the basement rock and by the lack of an extensive, low permeability capping layer to impede the movement of basal groundwater out into the lagoon. More favorable conditions for the development of basal groundwater are thought to exist in the southern half of the island due to the presence of relatively thick deposits of low-permeability ash near the coast, although groundwater has not yet been developed there.
dc.description.sponsorship U.S. Department of the Interior, Geological Survey Grant/Contract No. B-249
dc.format.extent ix + 79 pages
dc.language.iso en-US
dc.publisher Water Resources Research Center, University of Hawaii at Manoa
dc.relation.ispartofseries WRRC Technical Report
dc.relation.ispartofseries 189
dc.subject hydrogeology
dc.subject geologic mapping
dc.subject groundwater
dc.subject geochemistry
dc.subject gravity
dc.subject dikes
dc.subject rainfall-runoff relationships
dc.subject evapotranspiration
dc.subject Pohnpei
dc.subject Ponape
dc.subject Eastern Caroline Islands
dc.subject.lcsh Geology -- Micronesia (Federated States) -- Pohnpei Island.
dc.subject.lcsh Groundwater -- Micronesia (Federated States) -- Pohnpei Island.
dc.subject.lcsh Hydrogeology -- Micronesia (Federated States) -- Pohnpei Island.
dc.title WRRCTR No.189 Geology and hydrogeology of the island of Pohnpei, Federated States of Micronesia
dc.type Report
dc.type.dcmi Text
Appears in Collections: WRRC Technical Reports


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