Hemlock-Canadice UMP – NYS Dept. of Environmental Conservation

Hemlock-Canadice UMP – NYS Dept. of Environmental Conservation.

USGS Scientific Investigations Report 2012-5282: Hydrogeology of the Susquehanna River Valley-Fill Aquifer System and Adjacent Areas in Eastern Broome and Southeastern Chenango Counties, New York

USGS Scientific Investigations Report 2012-5282: Hydrogeology of the Susquehanna River Valley-Fill Aquifer System and Adjacent Areas in Eastern Broome and Southeastern Chenango Counties, New York.

Prepared in cooperation with New York State Department of Environmental Conservation

Hydrogeology of the Susquehanna River Valley-Fill Aquifer System and Adjacent Areas in Eastern Broome and Southeastern Chenango Counties, New York

By Paul M. Heisig

Thumbnail of and link to report PDF (3.56 MB)Abstract

The hydrogeology of the valley-fill aquifer system along a 32-mile reach of the Susquehanna River valley and adjacent areas was evaluated in eastern Broome and southeastern Chenango Counties, New York. The surficial geology, inferred ice-marginal positions, and distribution of stratified-drift aquifers were mapped from existing data. Ice-marginal positions, which represent pauses in the retreat of glacial ice from the region, favored the accumulation of coarse-grained deposits whereas more steady or rapid ice retreat between these positions favored deposition of fine-grained lacustrine deposits with limited coarse-grained deposits at depth. Unconfined aquifers with thick saturated coarse-grained deposits are the most favorable settings for water-resource development, and three several-mile-long sections of valley were identified (mostly in Broome County) as potentially favorable: (1) the southernmost valley section, which extends from the New York–Pennsylvania border to about 1 mile north of South Windsor, (2) the valley section that rounds the west side of the umlaufberg (an isolated bedrock hill within a valley) north of Windsor, and (3) the east–west valley section at the Broome County–Chenango County border from Nineveh to East of Bettsburg (including the lower reach of the Cornell Brook valley). Fine-grained lacustrine deposits form extensive confining units between the unconfined areas, and the water-resource potential of confined aquifers is largely untested.

Recharge, or replenishment, of these aquifers is dependent not only on infiltration of precipitation directly on unconfined aquifers, but perhaps more so from precipitation that falls in adjacent upland areas. Surface runoff and shallow groundwater from the valley walls flow downslope and recharge valley aquifers. Tributary streams that drain upland areas lose flow as they enter main valleys on permeable alluvial fans. This infiltrating water also recharges valley aquifers.

Current (2012) use of water resources in the area is primarily through domestic wells, most of which are completed in fractured bedrock in upland areas. A few villages in the Susquehanna River valley have supply wells that draw water from beneath alluvial fans and near the Susquehanna River, which is a large potential source of water from induced infiltration.

First posted February 20, 2013

  • Appendix 1 XLS (864 kB)
    Well data for Susquehanna River valley and adjacent uplands, eastern Broome and southeastern Chenango Counties, New York.
  • Plate 1 html
    Hydrogeology of the Susquehanna valley-fill aquifer system and adjacent areas in eastern Broome and southeastern Chenango Counties, New York

For additional information contact:
Director
U.S. Geological Survey
New York Water Science Center
425 Jordan Road
Troy, NY 12180
(518) 285-5600
http://ny.water.usgs.gov

COMMENTS
What the USGS are saying is that these three regions/locations are prime for “developers” (AKA drillers) to sink MAJOR water wells to supply frack operations. This paper relates to what I heard a Senior SRBS scientist present last year, that SRBC was quite concerned that as gas drilling moved North from PA it would be getting to the “headwaters regions (low water volume) of the Susq and other rivers and thus they anticipated more emphasis by the drillers to use groundwater for their fracking uses.
This directly goes to the issue of impacts on water quantity of residential and public water wells; that is what will a big mother of a “comercial” well by a driller do to the QUANTITY of water available from your private well.  In other words, will your water well dry up?
This is an issue that is NOT adressed at all in NYS draft regs OR the rdSGEIS – only pre-drill baseline testing of wells near(1000ft) a proposed well pad need be tested by the driller for QUALITY.
The potential impact on private property values is clear; mitigation by drilling a private well deeper would probably work, although I dont know enoug hydrology to float a boat, so to speak.
————————————
“Unconfined aquifers with thick saturated coarse-grained deposits are the most favorable settings for water-resource development, and three several-mile-long sections of valley were identified (mostly in Broome County) as potentially favorable: (1) the southernmost valley section, which extends from the New York–Pennsylvania border to about 1 mile north of South Windsor, (2) the valley section that rounds the west side of the umlaufberg (an isolated bedrock hill within a valley) north of Windsor, and (3) the east–west valley section at the Broome County–Chenango County border from Nineveh to East of Bettsburg (including the lower reach of the Cornell Brook valley).”
————————————
Finally, this water source/quantity issue will apply equally to regions further north of the NY/PA border, and one hope USGS is studying such; remember, drilling a bit north likely wont be marcellus but rather the deeper Utica Shale.
S
Stan Scobie, Binghamton, NY, 607-669-4683

Putting Local Aquifer Protections in Place in New York. Rachel Treichler

Sienna poll on hydrofracking in NY 1/2013

SNY0313 Crosstabs.xlsx.

There is tremendous stability over time in the overall result for support/oppose fracking
Support:  39%
Oppose:  43%
Upstate support:  39%
Oppose:              49%
(beyond margin of error)
=====================
Income <50K:
Support:  36%
Oppose:   46%
——————–
Income <$100K:
Support: 33%
Oppose:  51%
——————–
Income  $100K+:
Support:  47%
Oppose:   35%
(all beyond margin of error)
========================
So…Upstate : don’t like, higher income folks: like.
Hmm.
S
Stan Scobie, Binghamton, NY, 607-669-4683

New York Compulsory Integration

New York Compulsory Integration.

A Critical Review of the Compulsory Integration Requirement

in New York Environmental Conservation Law

Title 9 of Article 23

William C. Fischer

Various Pipeline Maps

Bill Huston’s Blog (Binghamton NY): Various Pipeline Maps.

Roundtable on Lenpape Resources Lawsuit & Gas Industry Intimidation tactics | Shaleshock Media

http://shaleshockmedia.org/2013/02/24/roundtable-on-lenpape-resources/

Hill and Hollow Unit Management Plan

Hill and Hollow Unit Management Plan.

Draft Unit Management Plan for Taylor Valley

  • I just received notification of a March  public meeting in Truxton to discuss the Draft Unit Management Plan for Taylor Valley.  I think it will be important to flood that meeting with concerned citizens from the area.

    Dear Taylor Valley Unit Management Area Stakeholder,

    A draft Unit Management Plan (UMP) has been developed for the Taylor Valley Unit Management Area, which includes Baker School House, Donahue Woods, Gee Brook, Hoxie Gorge, and Taylor Valley State Forests along with Papish Pond Multiple-Use Area. The UMP process, for this Unit began with a public meeting at the McGraw Central School’s cafeteria in February 2010. This meeting was used to gather input from the public with regards to the future management of the Unit.  Input from this meeting along with a long-range vision, the principles of ecosystem management, and the current use were used to develop management activities in the UMP.

    There is a meeting scheduled to gather feedback from the public on two draft UMPs (Taylor Valley and Hill and Hollow). I look forward to receiving feedback from you at the upcoming meeting. The following announcement contains details about the meeting:

      DEC Seeks Public Feedback on Two Draft Unit Management Plans (UMPs): Hill & Hollow and Taylor Valley

    WHEN: Monday, March 11, 2013, from 6:30 to 9:00 p.m.

    WHERE: Homer Central School District’s Hartnet Elementary School Gymnasium located on Academy Street in Truxton, NY.

    WHAT: To receive public feedback on the Draft Hill & Hollow and Draft Taylor Valley UMPs.  Copies of the plans are posted on the DEC’s website at: http://www.dec.ny.gov/lands/4979.html .The plans are also available, for public review, at local libraries and DEC offices. Copies of the UMPs are available on compact discs from the Cortland DEC office and may be requested by calling (607)753-3095 ext. 217.

    The meeting will begin with an open house format, to allow the public to meet informally with staff, discuss their concerns and provide written comments. Beginning at 7 p.m., staff will briefly present highlights of the two UMPs.  Following the presentation, the public will be able to provide verbal comments about the UMPs. Those unable to attend the meeting may submit comments (until April 11, 2013) by mail to: DEC, Division of Lands and Forests, 1285 Fisher Avenue, Cortland, NY  13045 or  by email to hcdedric@gw.dec.state.ny.us  for the Taylor Valley UMP and  to mlzubal@gw.dec.state.ny.us forthe Hill and Hollow UMP.

     

    WHY: The Draft UMPs have been developed to address management activities on State lands. The Hill & Hollow UMP contains Morgan Hill and Kettlebail State Forests as well as Labrador Hollow Unique Area. The Taylor Valley UMP includes: Taylor Valley, Hoxie Gorge, Baker School House, Donahue Woods and Gee Brook State Forests as well as Papish Pond Multiple-Use Area.

    Henry C. Dedrick Jr.
    Senior Forester, Region 7
    NYS DEC, Division of Lands & Forests
    1285 Fisher Ave.
    Cortland, NY 13045
    Phone: (607)753-3095 ext. 218
    1-800-388-8244 ext. 218
    Fax:      (607)753-8532
    e-mail:   hcdedric@gw.dec.state.ny.us

     

    The following   action by the DEC  is proposed in  the January  2013 Draft Taylor Valley Unit Management Plan (http://www.dec.ny.gov/docs/regions_pdf/tayvy1.pdf ).   Is the DEC anticipating a reversal of the decision not to allow surface activity associated with drilling in our state forests?     The final paragraph of page 60 says the following:

     

    “This prohibition is subject to change if the Draft Supplemental Generic Environmental Statements regarding Well Permit Issuance for Horizontal Drilling and High-Volume Fracturing to Develop the Marcellus Shale and Other Low-Permeability Gas Reservoirs is amended during finalization processes.”

    Here’s a more extended quote from the Draft Unit Management Plan:

    b. Consider future requests for oil and gas leasing using an open public process while protecting natural and recreational resources. Prior to leasing lands in this Unit, an open public process must be followed. This process includes coordination with the Division of Mineral Resources to determine: areas that can be leased with full rights granted (100% surface entry and no special conditions required); areas that may require special environmental and safety conditions; and areas that may be leased with no surface-disturbance/entry conditions (non-drilling clause). The following is a summary of the leasing process of State Forest lands:

    Receive requests to nominate specific lands within the Unit for leasing of mineral rights, from interested parties.

    Conduct tract assessments of nominated properties to determine where lands are able to support or accommodate related surface disturbance associated with oil and gas exploration, development, and extraction. Factors considered during the tract assessment process include the proximity to sensitive resources of the Unit. These resources include, but are not limited to certain management strategies, wetland, riparian zones, steep slopes, recreational trails and areas, unique ecological communities, habitat of rare and endangered species, archeological and cultural sites and scenic vistas and view sheds.

    o Apply a hierarchical approach that classifies areas of each State Forest into four categories as part of a tract assessment to be conducted prior to leasing.

    § Category A ‐ Compatible with well pad, road, and utility development. These areas can be considered the least sensitive to surface disturbance and should be considered first for well pad development to limit the overall impact of development. Examples of Category A areas include open fields, conifer plantations, and even-aged management areas.

    § Category B ‐ Uneven-age Management Areas with one well pad per State Forest. These areas are being managed for species that require large blocks of un-fragmented (diameters of temporary openings in the canopy shall be no larger than 2.5 times the height of surrounding trees) forests.

    § Category C ‐ 250-foot stream and designated recreational trail buffers. Not compatible with well pad development; may be compatible with road and utility development.

    § Category D – Infrastructure Exclusion areas. Not compatible with well pad, road, or utility development. These include: ponds, wetlands, spring seeps, and vernal pools with appropriate 250-foot buffers; slopes greater than 15 percent; archeological and cultural concerns; and areas being managed as Natural Areas.

    o Prohibit surface disturbance associated with high-volume hydraulic fracturing. This prohibition is subject to change if the Draft Supplemental Generic Environmental Statements regarding Well Permit Issuance for Horizontal Drilling and High-Volume Fracturing to Develop the Marcellus Shale and Other Low-Permeability Gas Reservoirs is amended during finalization processes.

    Is it a coincidence that there has been heavy logging in the state forest next to my home for the past two summers? Well-pad sized sections have been clear-cut or significantly thinned in Kennedy State Forest, and pipeline-width corridors have been cleared of debris.   It could be coincidence,  but this logging activity was well ahead of scheduled logging in the management plan for Kennedy State Forest  (according to conversations I had with the forester).    The clearing areas are congruent with the Department’s 2008(?) published maps of “Areas compatible with drilling. ”  Now the Draft Unit Management Plan  for Taylor Valley  shows that the DEC is planning for a possible reversal of the prohibition against surface activity associated with hvhf.  Has the DEC planned to allow drilling in the state forests all along  -despite claims to the contrary in the revised SGEIS?

    STATE FORESTS IN PA UNDER HYDROFRACKING

    U.S. Geological Survey: Natural Gas Fracking Is Destroying Pennsylvania Forests – Natural Gas Watch.org.

  • Full Report:  https://docs.google.com/viewer?url=http%3A%2F%2Fwww.naturalgaswatch.org%2Fwp-content%2Fuploads%2F2012%2F10%2FUSGS-fracking-landuse-report.pdf

Taylor Valley Unit Management Plan

Taylor Valley Unit Management Plan.

I just received notification of a March  public meeting in Truxton to discuss the Draft Unit Management Plan for Taylor Valley.  I think it will be important to flood that meeting with concerned citizens from the area.

 

The following   action by the DEC  is proposed in  the January  2013 Draft Taylor Valley Unit Management Plan (http://www.dec.ny.gov/docs/regions_pdf/tayvy1.pdf ).   Is the DEC anticipating a reversal of the decision not to allow surface activity associated with drilling in our state forests?     The final paragraph of page 60 says the following:

 

“This prohibition is subject to change if the Draft Supplemental Generic Environmental Statements regarding Well Permit Issuance for Horizontal Drilling and High-Volume Fracturing to Develop the Marcellus Shale and Other Low-Permeability Gas Reservoirs is amended during finalization processes.”

 

Here’s a more extended quote from the Draft Unit Management Plan:

 

b. Consider future requests for oil and gas leasing using an open public process while protecting natural and recreational resources. Prior to leasing lands in this Unit, an open public process must be followed. This process includes coordination with the Division of Mineral Resources to determine: areas that can be leased with full rights granted (100% surface entry and no special conditions required); areas that may require special environmental and safety conditions; and areas that may be leased with no surface-disturbance/entry conditions (non-drilling clause). The following is a summary of the leasing process of State Forest lands:

Receive requests to nominate specific lands within the Unit for leasing of mineral rights, from interested parties.

Conduct tract assessments of nominated properties to determine where lands are able to support or accommodate related surface disturbance associated with oil and gas exploration, development, and extraction. Factors considered during the tract assessment process include the proximity to sensitive resources of the Unit. These resources include, but are not limited to certain management strategies, wetland, riparian zones, steep slopes, recreational trails and areas, unique ecological communities, habitat of rare and endangered species, archeological and cultural sites and scenic vistas and view sheds.

o Apply a hierarchical approach that classifies areas of each State Forest into four categories as part of a tract assessment to be conducted prior to leasing.

§ Category A ‐ Compatible with well pad, road, and utility development. These areas can be considered the least sensitive to surface disturbance and should be considered first for well pad development to limit the overall impact of development. Examples of Category A areas include open fields, conifer plantations, and even-aged management areas.

§ Category B ‐ Uneven-age Management Areas with one well pad per State Forest. These areas are being managed for species that require large blocks of un-fragmented (diameters of temporary openings in the canopy shall be no larger than 2.5 times the height of surrounding trees) forests.

§ Category C ‐ 250-foot stream and designated recreational trail buffers. Not compatible with well pad development; may be compatible with road and utility development.

§ Category D – Infrastructure Exclusion areas. Not compatible with well pad, road, or utility development. These include: ponds, wetlands, spring seeps, and vernal pools with appropriate 250-foot buffers; slopes greater than 15 percent; archeological and cultural concerns; and areas being managed as Natural Areas.

o Prohibit surface disturbance associated with high-volume hydraulic fracturing. This prohibition is subject to change if the Draft Supplemental Generic Environmental Statements regarding Well Permit Issuance for Horizontal Drilling and High-Volume Fracturing to Develop the Marcellus Shale and Other Low-Permeability Gas Reservoirs is amended during finalization processes.

 

 

Is it a coincidence that there has been heavy logging in the state forest next to my home for the past two summers? Well-pad sized sections have been clear-cut or significantly thinned in Kennedy State Forest, and pipeline-width corridors have been cleared of debris.   It could be coincidence,  but this logging activity was well ahead of scheduled logging in the management plan for Kennedy State Forest  (according to conversations I had with the forester).    The clearing areas are congruent with the Department’s 2008(?) published maps of “Areas compatible with drilling. ”  Now the Draft Unit Management Plan  for Taylor Valley  shows that the DEC is planning for a possible reversal of the prohibition against surface activity associated with hvhf.  Has the DEC planned to allow drilling in the state forests all along  -despite claims to the contrary in the revised SGEIS?

BA

Schools and Gas Drilling

And Claire Barnett of the Healthy Schools Network joins Jeff Jones to discuss schools and gas drilling Interview at about 38 minutes into the program:

Capitol Pressroom, Feb. 1, 2013 http://www.wcny.org/thecapitolpressroomorg/wp-content/uploads/FEB012013.MP3

Healthyschools.org