5114 33RD AVE W 2018-01-02 MF Import

I Novack Property 99-11-10 1 510 Place Everett, Wa. The site generally slopes from the southwest to the northeast portion of the site. The elevation of the property within this area ranges from and elevation of 414 feet along the southwest portion of the site to an elevation of 402 within the northeast portion of the site. A steep bank is located along the west side of the property. The bank within this side of the site slopes down at almost a 100% slope down to adjoining properties that have been developed as single family residences. Vegetation on the site consists mainly of grasses and blackberry bushes. There are some deciduous and evergreen trees located along the west side of the property along the top on the steep bank. 3.2 Site Geology The site lies in a physiographic region known as the Puget Sound Lowland. The Puget Sound Lowland consists of a linear depression which trends in a north -south direction between the Olympic Mountains to the west and the Cascade Mountains to the east. The Lowland contains the majority of the Puget Sound Area. During the recent geologic past, within the last 1 million years, the topography of the Puget Sound Lowland Was altered by a series of glacial events originating out of the Canadian Rockies and the Northern Cascade Mountains. The most recent of these glacial events has been named the Vashon Stade and covered most of the Puget Sound Lowland with up to 3,000 feet of glacial ice from approximately 15,000 to 10,000 years ago. This glacial event altered the topography of the Puget Sound Lowland to resemble its current configuration of today. 4 GES, Inc.