Black River Escarpment (Wisconsin): Difference between revisions

From Citizendium
Jump to navigation Jump to search
(first draft here)
 
(add reference)
Line 1: Line 1:
{{subpages}}
{{subpages}}
The '''Black River Escarpment''' is a geological feature in Eastern [[Wisconsin]].<ref name=Martin1965>
The '''Black River Escarpment''' is a geological feature in Eastern [[Wisconsin]].<ref name=UsgsHydrogeologicMichigan/><ref name=Martin1965>
{{cite book
{{cite book
| isbn=9780299034757
| isbn=9780299034757
Line 24: Line 24:
The escarpment marks the boundary between bedrock from [[Lower Magnesian]] [[limestone]] [[bedrock]] and earlier Black River limestone.
The escarpment marks the boundary between bedrock from [[Lower Magnesian]] [[limestone]] [[bedrock]] and earlier Black River limestone.
The escarpment emerges from [[Green Bay]], on [[Lake Michigan]].
The escarpment emerges from [[Green Bay]], on [[Lake Michigan]].
The escarpment's boundaries are not always visible to the untrained eye, but are makred by cliffs in some regions.
The escarpment's boundaries are not always visible to the untrained eye, but are marked by cliffs in some regions.


==References==
==References==
{{Reflist|refs=  
{{Reflist|refs=  
 
<ref name=UsgsHydrogeologicMichigan>
{{cite news       
{{cite news       
| url        =  
| url        = https://pubs.usgs.gov/of/2007/1236/pdf/OFR2007-1236.pdf
| title      =  
| title      = Summary of Hydrogeologic Conditions by County for the State of Michigan
| work        =  
| work        = [[United States Geological Service]]
| author      =  
| author      =  
| date        =  
| date        =  

Revision as of 23:00, 13 October 2023

This article is a stub and thus not approved.
Main Article
Discussion
Related Articles  [?]
Bibliography  [?]
External Links  [?]
Citable Version  [?]
 
This editable Main Article is under development and subject to a disclaimer.

The Black River Escarpment is a geological feature in Eastern Wisconsin.[1][2][3] The escarpment runs parallel to and between the Niagara Escarpment and the Magnesian Escarpment. The escarpment marks the boundary between bedrock from Lower Magnesian limestone bedrock and earlier Black River limestone. The escarpment emerges from Green Bay, on Lake Michigan. The escarpment's boundaries are not always visible to the untrained eye, but are marked by cliffs in some regions.

References