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Hydrologic Implications of Seasonally Draining Lakes in the Oregon Cascades: Sensor and Planet Data 2026


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Created: Jun 11, 2026 at 11:25 p.m. (UTC)
Last updated: Jun 11, 2026 at 11:40 p.m. (UTC)
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Abstract

The hydrogeology of volcanic terrain exhibits characteristics that reflect both a legacy of volcanic construction and transient evolution of bedrock hydraulic conductivity over geologic time. Here, we seek to elucidate hydrogeologic structure in a Holocene-active region of the Central Oregon Cascade Range by measuring the drainage behavior of several lakes partially dammed by lava flows within the watershed of Clear Lake (the highest elevation permanent source of the McKenzie River). We measure the drainage of two seasonal lakes with in-situ sensors and satellite remote sensing, and compare this with the larger scale summer recession of the McKenzie River at the outlet of perennial Clear Lake. Clear Lake recession can be explained via drainage through two parallel linear reservoirs, which we interpret to reflect mixing of waters derived from old and young end-members of the Cascade Critical Zone state shift. Synthesizing our results with previous work we infer watershed scale transmissivity that varies with spatial scale of the aquifer. The filling and draining of the seasonal lakes depends on volume of snowmelt and the permeability of their porous lava dams. We also find, using remote sensing-derived timeseries, that all three systems, but particularly the draining lakes, have responded to declining snowpack since 1990. These results suggest that seasonal variations in surface water storage encode the structure of volcanic aquifers, and can be used to infer groundwater dynamics in the Cascade Range.

This resource represents our most recent Hobo pressure-temperature data and Planet remote sensing data for Lost and Fish Lakes, as well as air pressure data from the Carmen Diversion Dam (operated by EWEB).

Subject Keywords

Coverage

Spatial

Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
North Latitude
44.4472°
East Longitude
-121.8914°
South Latitude
44.3950°
West Longitude
-122.0545°

Content

Credits

Contributors

People or Organizations that contributed technically, materially, financially, or provided general support for the creation of the resource's content but are not considered authors.

Name Organization Address Phone Author Identifiers
Eugene Water and Electric Board

How to Cite

Simpson, A., E. Levenson (2026). Hydrologic Implications of Seasonally Draining Lakes in the Oregon Cascades: Sensor and Planet Data 2026, HydroShare, http://www.hydroshare.org/resource/4f634f67b3a14b5daee8ecc576bd988a

This resource is shared under the Creative Commons Attribution CC BY.

http://creativecommons.org/licenses/by/4.0/
CC-BY

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