U.S. Geological Survey Mineral Resourc…

lith-high lith-high lith-high
Service health Now:
Interface
Web Service, OGC Web Map Service 1.3.0
Keywords
Fees
none
Access constraints
none
Supported languages
No INSPIRE Extended Capabilities (including service language support) given. See INSPIRE Technical Guidance - View Services for more information.
Data provider

U.S. Geological Survey Mineral Resources Program (unverified)

Contact information:

Peter N. Schweitzer

U.S. Geological Survey Mineral Resources Program

mailing address:
Mail Stop 954 USGS National Center, 20192 Reston, USA

Email: 

Phone: 703-648-6533

Service metadata
No INSPIRE Extended Capabilities (including service metadata) given. See INSPIRE Technical Guidance - View Services for more information.

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Available map layers (13)

Tennessee_Geology (Tennessee_Geology)

Tennessee_Geology

Tennessee_Lithology (Tennessee_Lithology)

Tennessee_Lithology

Tennessee_Lithology (lith-high)

USGS Web Mapping Service: Lithologic map derived from the Tennessee State Geologic Map

Tennessee_Lithology (lith-low)

USGS Web Mapping Service: Lithologic map derived from the Tennessee State Geologic Map

Tennessee_Contacts (Tennessee_Contacts)

Tennessee_Contacts

Tennessee_Contacts (contacts-high)

USGS Web Mapping Service: Lithologic map contacts derived from the Tennessee State Geologic Map

Tennessee_Contacts (contacts-low)

USGS Web Mapping Service: Lithologic map contacts derived from the Tennessee State Geologic Map

Tennessee_Age (Tennessee_Age)

Tennessee_Age

Tennessee_Age (age-high)

USGS Web Mapping Service: Geologic age map derived from the Tennessee State Geologic Map

Tennessee_Age (age-low)

USGS Web Mapping Service: Geologic age map derived from the Tennessee State Geologic Map

Tennessee_Faults (Tennessee_Faults)

Tennessee_Faults

Tennessee_Faults (faults-high)

USGS Web Mapping Service: Faults derived from the Tennessee State Geologic Map

Tennessee_Faults (faults-low)

USGS Web Mapping Service: Faults derived from the Tennessee State Geologic Map

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