1997
DOI: 10.5962/bhl.title.154745
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Howellia aquatilis (water howellia) ponds of the Swan Valley : conceptual hydrologic models and ecological implications /

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Cited by 2 publications
(9 citation statements)
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“…1972). Pleistocene lateral moraines, basal moraine and glaciofluvial sediments deposited by one of the two major diverging trunk glaciers occupying the Swan-Clearwater Valley during the late Pleistocene are exposed at the land surface (Shapley and Lesica, 1997). The thickness of the glacial till is unknown.…”
Section: Site Descriptionmentioning
confidence: 99%
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“…1972). Pleistocene lateral moraines, basal moraine and glaciofluvial sediments deposited by one of the two major diverging trunk glaciers occupying the Swan-Clearwater Valley during the late Pleistocene are exposed at the land surface (Shapley and Lesica, 1997). The thickness of the glacial till is unknown.…”
Section: Site Descriptionmentioning
confidence: 99%
“…Seeds germinate in October under aerobic conditions and remain as a small seedling beneath the winter snowpack (Shapley and Lesica, 1997). They are then submerged as snow melt refills the wetlands in early spring (Shapley and Lesica, 1997). This wetland hydrological cycle of wetting and drying is necessary to maintain H. aquatilis populations.…”
Section: Introductionmentioning
confidence: 99%
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