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New Geologic Map of Vermont Unveiled

New Geologic Map of Vermont Unveiled

MONTPELIER, Vt. – A new bedrock geologic map of the state was unveiled in a ceremony at the Vermont State House today, bringing a critical tool to land managers involved in natural resource planning and environmental assessment. 

The event, hosted by Gov. Peter Shumlin, included the Secretary of the Agency of Natural Resources Deb Markowitz; Peter Lyttle of the U.S. Geological Survey; Laurence Becker, Vermont Agency of Natural Resources; and Char Mehrtens of the University of Vermont. These three organizations were the main collaborators to produce this updated, highly detailed map.  The state’s last map of this kind was produced in 1961, with the first geologic map of the state being produced 150 years ago. 

“Through the balanced work of all the partners, Vermonters now have a comprehensive map that will help us better understand and plan for issues like groundwater, energy, hazards, infrastructure development, and environmental protection for years to come,” Gov. Shumlin said. “Such up to date information is crucial to the State when addressing the economic and environmental concerns of citizens, lawmakers, government, business, and local communities.” 

Geologic maps enable resource managers and land management agencies to identify and protect aquifers, evaluate resources and land use, and prepare for natural hazards, such as earthquakes and land subsidence, for example.  Geologic maps are also critical tools for choosing safe sites for solid and hazardous waste disposal and for protecting sensitive ecosystems. 

Understanding where different rock types are located provides important clues about where groundwater and mineral resources exist. The map provides a template for future studies in a variety of disciplines — not only geologic, tectonic and hydrologic studies, but also economic and environmental evaluations. 

“It was an incredible tour de force to bring this level of detail to the new bedrock map on account of the many intense geologic events that have left their mark on the state of Vermont over the eons,” said USGS Director Marcia McNutt from the bureau’s headquarters in Reston, Va. “Without the steadfast and enduring partnership of the USGS, the Vermont Geological Survey, and the University of Vermont, this achievement would not have been possible.” 

Vermont’s new map shows an uncommon level of detail for state geologic maps. Mapped rock units are based on lithology, or rock type, rather than traditional rock formations that may include multiple rock types.  This map identifies more than 486 different types of rock throughout the state of Vermont, a design feature intended to facilitate use by multiple disciplines. During the project, scientists also discovered many fault lines, advancing understanding about how and where water travels through the underground rock formations and providing clues about where underground aquifers — an important source for potable fresh water — may be located. 

“The Vermont map is the visual presentation used to communicate data, ideas and interpretations. New map patterns developed through years of field and laboratory studies led to recognition of terranes from different geologic settings. Most importantly, understanding these settings gives us predictive capabilities for the sub-surface including areas where rocks are covered by glacial deposits,” said Laurence Becker, the 13th Vermont State Geologist.  “The bedrock geology, in conjunction with the overlying glacial deposits, form the geologic system crucial to understanding economic and environmental issues that face our state.” 

Vermont’s new geologic map substantially builds upon the state’s previous geologic map – created in 1961– by incorporating the theory of plate tectonics, which had not yet been developed 50 years ago. The Green Mountains form the backbone of Vermont. Their geologic history, spanning more than 1.4 billion years, attests to a complex series of plate tectonic events including the formation of corals reefs, ocean basins and volcanic arcs punctuated by periods of Appalachian mountain building. 

“The new bedrock geologic map of Vermont changes the way we look at the geologic history of the state because we can now see relationships between rock types and structures that were obscured on the old map,” said Char Mehrtens, contributing author of the map and professor of Geology at UVM.  “The level of detail provided by the new map is also a huge help to geoscience educators because we can now design student projects to utilize the three dimensional information it contains.  The significance of this map can’t be understated; it places us in the national conversation about the origin and evolution of mountain belts, particularly because the National Science Foundation-funded Earth Scope project will be working in New England starting in 2013.  The new bedrock map sets the stage for collaborative studies of University of Vermont geologists with their national and international colleagues.” 

The process for creating a geologic map for an entire state is very field intensive, and The Bedrock Geologic Map of Vermont has been in development since the 1980s.  The authors who originated this project and brought it to fruition include Nicholas M. Ratcliffe, USGS; Rolfe S. Stanley*, UVM; Marjorie H. Gale, VGS; Peter J. Thompson, VGS; and Gregory J. Walsh, USGS. 

Other contributors included Norman L. Hatch, Jr.*, USGS; Douglas W. Rankin, USGS; Barry L. Doolan, UVM; Jonathan Kim, VGS; Charlotte J. Mehrtens, UVM; John N. Aleinikoff, USGS; and J. Gregory McHone, Wesleyan University.  Linda M. Masonic, USGS, was responsible for the cartography. 

The Bedrock Geologic Map of Vermont covers 246 7.5-minute quadrangles at a scale of 1:100,000 where one inch equals about 1.6 miles.  The map consists of three oversize sheets (52 x 76 inches), and displays the state’s geology in an 8.5-foot tall map. Printed copies of the map will be available for sale by the USGS and by the Vermont Geological Survey. The map is also available online in a variety of formats through the USGS and the Vermont Geological Survey website.

* Deceased

USGS Newsroom

More information

Parameter Value Description
Magnitude mb The magnitude for the event.
Longitude ° East Decimal degrees longitude. Negative values for western longitudes.
Latitude ° North Decimal degrees latitude. Negative values for southern latitudes.
Depth km Depth of the event in kilometers.
Place Textual description of named geographic region near to the event. This may be a city name, or a Flinn-Engdahl Region name.
Time 1970-01-01 00:00:00 Time when the event occurred. UTC/GMT
Updated 1970-01-01 00:00:00 Time when the event was most recently updated. UTC/GMT
Timezone offset Timezone offset from UTC in minutes at the event epicenter.
Felt The total number of felt reports
CDI The maximum reported intensity for the event.
MMI The maximum estimated instrumental intensity for the event.
Alert Level The alert level from the PAGER earthquake impact scale. Green, Yellow, Orange or Red.
Review Status Indicates whether the event has been reviewed by a human.
Tsunami This flag is set to "1" for large events in oceanic regions and "0" otherwise. The existence or value of this flag does not indicate if a tsunami actually did or will exist.
SIG A number describing how significant the event is. Larger numbers indicate a more significant event.
Network The ID of a data contributor. Identifies the network considered to be the preferred source of information for this event.
Sources A comma-separated list of network contributors.
Number of Stations Used The total number of Number of seismic stations which reported P- and S-arrival times for this earthquake.
Horizontal Distance Horizontal distance from the epicenter to the nearest station (in degrees).
Root Mean Square sec The root-mean-square (RMS) travel time residual, in sec, using all weights.
Azimuthal Gap The largest azimuthal gap between azimuthally adjacent stations (in degrees).
Magnitude Type The method or algorithm used to calculate the preferred magnitude for the event.
Event Type Type of seismic event.
Event ID Id of event.
Event Code An identifying code assigned by, and unique from, the corresponding source for the event.
Event IDS A comma-separated list of event ids that are associated to an event.

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