Lake Chelan, Washington: Bottom and Sub-Bottom Topography
Lake Chelan, a fjordike lake in north-central Washington, consists of two basins separated by a shallow constriction. The Lucerne Basin, at the upstream end of the lake, is 466 m deep and sediments in it are relatively thin except near the upper end. The Wapato Basin is shallow, but sediments are at...
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| Veröffentlicht in: | Limnology and oceanography 1967-01, Vol.12 (2), p.253-259 |
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| container_title | Limnology and oceanography |
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| creator | Whetten, John T. |
| description | Lake Chelan, a fjordike lake in north-central Washington, consists of two basins separated by a shallow constriction. The Lucerne Basin, at the upstream end of the lake, is 466 m deep and sediments in it are relatively thin except near the upper end. The Wapato Basin is shallow, but sediments are at least 178 m thick. Both Basins probably had a glacial origin; however, they probably were carved by different glaciers of different ages. The thick sediment in Wapato Basin was probably deposited by meltwater from the Chelan glacier (which occupied Lucerne Basin) and the Okanogan glacier, which blocked the downstream end of Wapato Basin. |
| doi_str_mv | 10.4319/lo.1967.12.2.0253 |
| format | Article |
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The Lucerne Basin, at the upstream end of the lake, is 466 m deep and sediments in it are relatively thin except near the upper end. The Wapato Basin is shallow, but sediments are at least 178 m thick. Both Basins probably had a glacial origin; however, they probably were carved by different glaciers of different ages. The thick sediment in Wapato Basin was probably deposited by meltwater from the Chelan glacier (which occupied Lucerne Basin) and the Okanogan glacier, which blocked the downstream end of Wapato Basin.</description><identifier>ISSN: 0024-3590</identifier><identifier>DOI: 10.4319/lo.1967.12.2.0253</identifier><language>eng</language><publisher>American Society of Limnology and Oceanography</publisher><subject>Bedrock ; Freshwater ; Glacial lakes ; Glacial landforms ; Lakes ; Landslides ; Moraines ; Sediments ; Valleys ; Water depth ; Watersheds</subject><ispartof>Limnology and oceanography, 1967-01, Vol.12 (2), p.253-259</ispartof><rights>Copyright 1967 American Society of Limnology and Oceanography, Inc.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/2833037$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/2833037$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,778,782,801,27907,27908,58000,58233</link.rule.ids></links><search><creatorcontrib>Whetten, John T.</creatorcontrib><title>Lake Chelan, Washington: Bottom and Sub-Bottom Topography</title><title>Limnology and oceanography</title><description>Lake Chelan, a fjordike lake in north-central Washington, consists of two basins separated by a shallow constriction. The Lucerne Basin, at the upstream end of the lake, is 466 m deep and sediments in it are relatively thin except near the upper end. The Wapato Basin is shallow, but sediments are at least 178 m thick. Both Basins probably had a glacial origin; however, they probably were carved by different glaciers of different ages. The thick sediment in Wapato Basin was probably deposited by meltwater from the Chelan glacier (which occupied Lucerne Basin) and the Okanogan glacier, which blocked the downstream end of Wapato Basin.</description><subject>Bedrock</subject><subject>Freshwater</subject><subject>Glacial lakes</subject><subject>Glacial landforms</subject><subject>Lakes</subject><subject>Landslides</subject><subject>Moraines</subject><subject>Sediments</subject><subject>Valleys</subject><subject>Water depth</subject><subject>Watersheds</subject><issn>0024-3590</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1967</creationdate><recordtype>article</recordtype><recordid>eNotjk1PhDAURbvQxHH0B5i4YOVK8LWvhdadEr8SEheOcUkKLQMjQ5GWxfx7SWZWNyf35OYSckMh4UjVQ-8SqtIsoSxhCTCBZ2QFwHiMQsEFufR-BwBKCLEiqtC_Nspb2-vhPvrRvu2GbXDDY_TsQnD7SA8m-pqr-IQbN7rtpMf2cEXOG917e33KNfl-fdnk73Hx-faRPxWxZgghZryWFFEayo3AKtWKNhxSRZnMGq5rzGoBLKuMlWAqXim2VIaiSKFmVhpck7vj7ji5v9n6UO47X9t-OWzd7EuaYcqQ80W8PYo7H9xUjlO319OhZBIRMMN_RkpQeg</recordid><startdate>19670101</startdate><enddate>19670101</enddate><creator>Whetten, John T.</creator><general>American Society of Limnology and Oceanography</general><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>19670101</creationdate><title>Lake Chelan, Washington: Bottom and Sub-Bottom Topography</title><author>Whetten, John T.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a230t-24c81338d14d53b6a91f40691287f4ac37c5027bde80db4b92912d13560c2e8d3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1967</creationdate><topic>Bedrock</topic><topic>Freshwater</topic><topic>Glacial lakes</topic><topic>Glacial landforms</topic><topic>Lakes</topic><topic>Landslides</topic><topic>Moraines</topic><topic>Sediments</topic><topic>Valleys</topic><topic>Water depth</topic><topic>Watersheds</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Whetten, John T.</creatorcontrib><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Limnology and oceanography</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Whetten, John T.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Lake Chelan, Washington: Bottom and Sub-Bottom Topography</atitle><jtitle>Limnology and oceanography</jtitle><date>1967-01-01</date><risdate>1967</risdate><volume>12</volume><issue>2</issue><spage>253</spage><epage>259</epage><pages>253-259</pages><issn>0024-3590</issn><abstract>Lake Chelan, a fjordike lake in north-central Washington, consists of two basins separated by a shallow constriction. The Lucerne Basin, at the upstream end of the lake, is 466 m deep and sediments in it are relatively thin except near the upper end. The Wapato Basin is shallow, but sediments are at least 178 m thick. Both Basins probably had a glacial origin; however, they probably were carved by different glaciers of different ages. The thick sediment in Wapato Basin was probably deposited by meltwater from the Chelan glacier (which occupied Lucerne Basin) and the Okanogan glacier, which blocked the downstream end of Wapato Basin.</abstract><pub>American Society of Limnology and Oceanography</pub><doi>10.4319/lo.1967.12.2.0253</doi><tpages>7</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0024-3590 |
| ispartof | Limnology and oceanography, 1967-01, Vol.12 (2), p.253-259 |
| issn | 0024-3590 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_17362344 |
| source | Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals; Jstor Complete Legacy; Alma/SFX Local Collection |
| subjects | Bedrock Freshwater Glacial lakes Glacial landforms Lakes Landslides Moraines Sediments Valleys Water depth Watersheds |
| title | Lake Chelan, Washington: Bottom and Sub-Bottom Topography |
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