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Displacement at the ground surface was measured approximately daily (the time of record varied throughout the monitoring period) at locations upon the upper (E1), middle (E2), and lower (E3) parts of the landslide along its left lateral (southeastern) boundary using electronic cable extension transducers (extensometers; Celesco PT8101 model) with manufacturer-stated ±0.7 mm accuracy (extensometer_data.csv). Sensors and their anchors were installed above the ground surface on galvanized steel posts partly driven by hand into the ground on opposite sides of a strike-slip fault forming the landslide’s left margin. Posts were driven into the ground at angles such that the extension cable was oriented parallel to the fault and measured the length of cable extending from the sensor housing approximately parallel to the direction of landslide movement. Sensors had approximate maximum ranges of 1524 mm and were episodically reset to lower values by moving extension cables to newly driven anchor posts located closer to the sensors. However, sensors sometimes over-ranged and failed, likely providing inaccurate data when the maximum range was reached until failure occurred. Additional errors and omissions in the data likely resulted from problems with the solar- and battery-powered dataloggers including power loss, loading of rain, snow, and ice on extension cables and anchor posts, frost heaving, animal activity, and other factors. Erroneous data are excluded from the data provided here when that error was clear during inspection; however, it is almost certain that some error remains.\n\nAny use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government.\n\nAcknowledgements\nJon Mckenna, David Kibler, Joel Smith, Brett Shurtleff, Sarah Rickard (formerly Galloway), Joanna Panosky, Jeff Coe, Giulia Biavati, Mason Einbund, Kelli Baxstrom, and Olivia Hoch are thanked for their assistance with installing and maintaining the monitoring 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