Quick Report

October 16, 2009

Okay, lack of sleep and long hours have been catching up to me. Here is the latest:

On October 15, 2009, Jack Powell (FP), and Isabelle Sarikhan (DGER) investigated the Nile landslide on Highway 410 and the older Sanford Pasture Landslide approximately 10 miles west of Naches. There is concern that the Sanford Pasture Landslide could reactivate as a result of the recent movement of the Nile Landslide. We also investigated potentially new activity within the Nile Landslide, continued risk to public safety and the safety of crews working on the ground, and collected additional data.

No immediate danger was found for continued progression of failures. No cracks or fissures were found above slope of the Nile Landslide and a traverse of the crest of the hill above the Nile Landslide also found no cracks or fissures. Further, evidence was found that the Nile Landslide occurred below the failure plane of the Sanford Pasture Landslide, greatly reducing the risk of movement by the release of pressure from the Nile Landslide. However, because of the size and wide scale impact that the movement of Sanford Pasture can cause, further surveys for recent cracks and fissures further uphill on the western edge of the Sanford Pasture Landslide should be conducted.

The Nile Landslide had moved several feet since Sunday. During our visit on Oct. 15, no rapid signs of movement were occurring, but the landslide is probably still moving at a speed of inches per day. The speed will gradually slow, but movement might not completely stop for months. Sudden catastrophic movement is unlikely and the risk of public safety and workers on the ground should be low if they stay a safe distance from the landslide. The most unstable parts of the landslide are the toe, which is oversteepened and can result in shallow failures and the scarps, both internal and the main scarp, which can ravel or result in shallow failures without warning.

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2 Responses to “Quick Report”

  1. Scott Linneman Says:

    Well done Isabelle! My Geomorph class is following your updates. Can you tell us the basic bedrock geology? CRB w/interbeds?

  2. Isabelle Says:

    Thanks Scott. The geology is basically the upper flows of the Columbia River Basalts with interbeds of the Ellensburg Formation. We found that the landslide is made up mostly of talus on what we think is the failure plane of Collins(?) sandstone (an Ellensburg Interbed). We didn’t see much in the way of basaltic bedrock that got carried down. I’ll try and get a cross section picture posted soon.

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