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Data release for Evidence of glacial activity during MIS 4 in the Rocky Mountains, Colorado, USA

Dates

Publication Date
Start Date
2015
End Date
2021

Citation

Honke, J.S., Pigati, J.S., and Daniels, J.M., 2021, Data release for Evidence of glacial activity during MIS 4 in the Rocky Mountains, Colorado, USA: U.S. Geological Survey data release, https://doi.org/10.5066/P9OQL78N.

Summary

The Ziegler Reservoir fossil site near Snowmass Village, Colorado (USA) provides a rare opportunity to examine environmental conditions in the Rocky Mountains during marine isotope stage (MIS) 4 (71–57 ka). Although recognized as a global-scale cold event, MIS 4 is typically absent from Rocky Mountain glacial chronologies because the geologic evidence was either covered or destroyed during the subsequent, and larger, MIS 2 (Pinedale; 29–14 ka) glaciation. The Ziegler Reservoir site is perched on a ridge above Pinedale glacial limits, which allowed for the preservation of a long-lived sequence of predominantly eolian sediments that spans from late MIS 6 (ca. 140 ka) through early MIS 3 (ca. 55 ka). Sediments dating to MIS 4 exhibit [...]

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Attached Files

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0_Data_Dictionary_MIS4_study.csv 12.59 KB text/csv
1a_Sample_Information_ZR_Samples_MIS4_study.csv 820 Bytes text/csv
1b_Sample_Information_Provenance_Samples_MIS4_study.csv 1.56 KB text/csv
2a_Particle_Size_Data_MIS4_study.csv 1.13 KB text/csv
2b_Particle_Size_Data_Silt_Subsets_MIS4_study.csv 1.45 KB text/csv
3a_Mineralogy_Data_MIS4_study.csv 5.05 KB text/csv
3b_Mineralogy_Ranges_MIS4_study.csv 551 Bytes text/csv
3c_Mineralogy_Averages_MIS4_study.csv 225 Bytes text/csv
3d_Clay_Mineralogy_Data_MIS4_study.csv 1.15 KB text/csv
4_Elemental_Data_MIS4_study.csv 32.53 KB text/csv

Purpose

These data were used to determine if there is evidence of glaciation in the Rocky Mountains during MIS 4..

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Communities

  • USGS Data Release Products

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Provenance

Additional Information

Identifiers

Type Scheme Key
DOI https://www.sciencebase.gov/vocab/category/item/identifier doi:10.5066/P9OQL78N

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