My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
PERMFILE111168
DRMS
>
Back File Migration
>
Permit File
>
200000
>
PERMFILE111168
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/24/2016 10:07:45 PM
Creation date
11/24/2007 8:19:13 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981013
IBM Index Class Name
Permit File
Doc Date
12/11/2001
Section_Exhibit Name
EXHIBIT 05 CULTURAL AND HISTORIC RESOURCE INFORMATION
Media Type
D
Archive
No
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
86
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
``,: <br />4"' <br />~, <br />i <br />I:: <br />~~~ <br />~: <br />~, <br /> <br />9 <br />Table 2 <br />Summary of Holocene Climatic Episodes <br />in Eastern North America' <br />Dateb Episode Inferred Climate <br />100 BP to Recent Dry or very dry <br />Present <br />400 to Neo-Boreal Generally cooler <br />100 BP <br />850 to Pacific Dry <br />400 BP <br />1260 to Neo-Atlantic Somewhat moister <br />850 BP <br />1680 to Scandic Somewhat moister <br />1260 BP <br />5060 to Sub-Boreal Initially moister condition followed <br />2760 HP by increased desiccation <br />8490 to Atlantic Drier and/or warmer; northward <br />5060 BP expansion <br />9300 to Boreal Gradual warming period; vegetation <br />8490 BP border moving northward and <br /> grasslands expanding eastward <br />10,030 to Sub-Boreal Gradual warming period <br />9300 BP <br />Before Late Glacial Temperatures a few degrees cooler; <br />10,030 BP gradual shift from boreal forests <br /> to grasslands indicating a <br /> drying/and/or warming trend <br />°Source: Wendland (1978) <br />bBP years before present, with a present baseline of AD 1950 <br />
The URL can be used to link to this page
Your browser does not support the video tag.