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Precariously balanced rock data from northern New York and Vermont, USA

Dates

Publication Date
Start Date
2022-08-01
End Date
2022-08-08

Citation

McPhillips, D., and Pratt, T.L., 2024. Precariously balanced rock data from northern New York and Vermont, USA: U.S. Geological Survey data release, https://doi.org/10.5066/P1H74TGF.

Summary

This work describes observations of boulders and their pedestals at five sites in New York and Vermont, which are used to calculate scaling factors for the 2023 time-independent National Seismic Hazard Model site-specific hazard curves (Petersen, M.D., Shumway, A.M., Powers, P.M., Field, E.H., Moschetti, M.P., Jaiswal, K.S., Milner, K.R., Rezaeian, S., Frankel, A.D., Llenos, A.L. and Michael, A.J., 2024. The 2023 US 50-State National Seismic Hazard Model: Overview and implications. Earthquake Spectra, 40(1), pp.5-88). This approach represents the current best-practice for validating hazard curves using precariously balanced rocks (e.g., Rood, A.H., Rood, D.H., Stirling, M.W., Madugo, C.M., Abrahamson, N.A., Wilcken, K.M., Gonzalez, [...]

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results_preferredGeometry.csv 608 Bytes text/csv
results_conservativeGeometry.csv 632 Bytes text/csv
miniseed_azureMtn.zip 5.08 MB application/zip
miniseed_blueRidgeRd.zip 3.69 MB application/zip
miniseed_littleSawyerMtn.zip 4.74 MB application/zip
miniseed_mtElmore.zip 8.45 MB application/zip
miniseed_westfield.zip 3.27 MB application/zip
adkpbr_azure_utm_centroid.txt 42.73 MB text/plain
adkpbr_blueridge_utm_centroid.txt 75.09 MB text/plain
adkpbr_elmore_utm_centroid.txt 71.12 MB text/plain
adkpbr_sawyer_utm_centroid.txt 39.25 MB text/plain
adkpbr_westfield_utm_centroid.txt 117.24 MB text/plain
figure_captions.txt 610 Bytes text/plain
figure_azureMtn.pdf 157.12 MB application/pdf
figure_blueRidgeRd.pdf 198.15 MB application/pdf
figure_mtElmore.pdf 152.87 MB application/pdf
figure_Westfield.pdf 126.07 MB application/pdf
figure_littleSawyerMtn.pdf 169.88 MB application/pdf
results_hazardResults.csv 387 Bytes text/csv

Purpose

Although recordings of historic seismicity are a fundamental part seismic hazard models, the duration of the record is generally short relative to the return times of damaging earthquakes. Geologic data can provide important constraints over longer timescales. This is true in the eastern U.S., where crustal strain rates are low (and earthquake return times are long), but few Quaternary-active faults have been mapped, even in areas of relatively high seismicity, such as northern New York and Vermont. As a result, there have been few geologic constraints applied to the National Seismic Hazard Model in this region (Thompson Jobe, J., A. Hatem, R. Gold, C. DuRoss, N. Reitman, R. Briggs, and C. Collett (2022). Revised Earthquake Geology Inputs for the Central and Eastern United States and Southeast Canada for the 2023 National Seismic Hazard Model, Seismol. Res. Lett. 93, 3100–3120, doi: 10.1785/0220220162). The precariously balanced rocks described here may be used to validate the hazard model with geologic constraints.

Rights

This work is marked with Creative Commons Zero v1.0 Universal (https://creativecommons.org/publicdomain/zero/1.0/).

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DOI https://www.sciencebase.gov/vocab/category/item/identifier doi:10.5066/P1H74TGF

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