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(For further information on spectrsocopy, see:
http://speclab.cr.usgs.gov)
TITLE: White_Crust LV30 (Epsomite?) DESCRIPT
DOCUMENTATION_FORMAT: Mixture
SAMPLE_ID: LV30
MIXTURE_TYPE: Intimate
MIXTURE: Epsomite + possible other salts
FORMULA: MgSO4.7H2O
FORMULA_HTML: MgSO4.7H2O
COLLECTION_LOCALITY: Arkansaa river Site 3 km south of Leadville, Colorado, USA
ORIGINAL_DONOR: Gregg Swayze
COLLECTION_LATITUDE: Not Available # degrees and decimal minutes (N or S)
COLLECTION_LONGITUDE: Not Available # degrees and decimal minutes (W or E)
DATUM: Not Available # coordinate datum
CURRENT_SAMPLE_LOCATION: USGS Denver Spectroscopy Laboratory, Denver, Colorado
ULTIMATE_SAMPLE_LOCATION: USGS Denver Spectroscopy Laboratory, Denver, Colorado
SAMPLE_DESCRIPTION:
White Crust (Epsomite?) Arkansas River Site Leadville LV30. This crust formed about saturated fluvial mine tailings rich in pyrite. Apparently water saturated with salts wicked up through permeable fine-grained sand and formed the white salt crust at the surface when the liquid evaporated. It may be possible that the epsomite is mixed with other salts and trace metals may substitute for Mg (e.g. As etc). This type of salt deposit is typical of acid mine drainage and when dissolved by rain or other precipitation causes a quick release of metals into streams.
END_SAMPLE_DESCRIPTION.
XRD_ANALYSIS:
none
END_XRD_ANALYSIS.
COMPOSITIONAL_ANALYSIS_TYPE: NONE # XRF, EM(WDS), ICP(Trace),WChem
COMPOSITION_TRACE: None
COMPOSITION_DISCUSSION:
none
END_COMPOSITION_DISCUSSION.
MICROSCOPIC_EXAMINATION:
none
END_MICROSCOPIC_EXAMINATION.
SPECTROSCOPIC_DISCUSSION:
The spectral features closely resemble those of epsomite in standard GDS149. The presence of a band at 1.6237 and 2.207 may be diagnostic of epsomite and perhaps other salts.
END_SPECTROSCOPIC_DISCUSSION.
SPECTRAL_PURITY: 1c2_3_4_ # 1= 0.2-3, 2= 1.5-6, 3= 6-25, 4= 20-150 microns
| LIB_SPECTRA_HED: | where | Wave Range | Av_Rs_Pwr | Comment |
|---|---|---|---|---|
| LIB_SPECTRA: | splib05a r 9029 | 0.2-3.0µm | 200 | g.s.= |
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