My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
10-23-2002 Council Agenda
>
City Council Packets
>
2000-2009
>
2002
>
10-23-2002 Council Agenda
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
5/9/2012 1:38:19 PM
Creation date
5/9/2012 1:31:05 PM
Metadata
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
113
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
View images
View plain text
All soil samples obtained were brought: to our laborato <br />for examination and classification. They will be retained for <br />o period of at least 90 cloys from date of issue of this report <br />after which they will be discarded unless we are otherwise not- <br />ified. <br />Drawing No 1 is a site plan showing the test hole loco <br />tions in relation to the outline of the proposed building. Detc <br />iled soil descriptions along with a plot of the standard pene- <br />tration test blows per foot are given on the Borehole Log shee s, <br />Drawings No.2 and 3„ The capital letters in parentheses folio <br />ing the regular soil descriptions are the appropriate group <br />symbols of the Unified Soil Classification System. A chart <br />explaining this system is appended. <br />All elevations in this report are to geodetic datum, an <br />were obtained using the bench mark noted on the site plan. <br />SITE AND GEOLOGY <br />The properly slopes from the south down to a creek whic <br />traverses the north side of the site <br />Geologically, the site lies just north of a fork of 'two <br />deep, major pre-glacial river channels. According to informati�' <br />published by the State of Minnesota Geological Survey, the uppc <br />most bedrock stratum under the property is believed to be St, <br />Peter sandstone and probably occurs at a depth of 130 to 140 <br />feet below present grade. The lower portions of these channels <br />were probably filled in with glacial outwash sands and gra•. 1s <br />These were subsequently covered by clayey glacial till related <br />o the Qes Main -s i_c^ - cansin <br />SUBTERRANEAN <br />ENGINEERING INC. <br />MINNEAPOLIS. <br />
The URL can be used to link to this page
Your browser does not support the video tag.