The reason for the abandonment is believed to have been the collapse of a slide which had blocked the Fraser River, forming a lake reaching upstream many miles, such that the location at Keatley Creek was near the shoreline (it is today on a benchland high above the river's canyon).
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It was not just from her account that Teit drew drawings upon which Lillooet's rebuilt si7xten was built, but also from his knowledge of underground houses in the Thompson and Bonaparte valleys - in his day, many people still lived in them.
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Quiggly towns and smaller groups of quiggly holes are common features of the landscape in certain areas of southern British Columbia, notably from the Fraser Canyon near Lillooet across the Thompson River valley and down the Okanagan Valley.
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