← Back to Gem Knowledge

GEM KNOWLEDGE · LABORATORY NOTES

Magma Chalcedony

An Indonesian material that Soul Body Gems obtained as raw stone, introduced to clients, and submitted for testing in 2020. “Magma Chalcedony” is its market name.

Finding: Sample 9148 (#5), completed July 16, 2020, showed orange quartz/chalcedony colored by arsenic sulfides identified as orpiment/realgar. The gray zones were mainly quartz with minor aluminum, calcium and sodium; the researcher suggested former plagioclase phenocrysts in volcanic rock followed by hydrothermal alteration.

Our history: Soul Body Gems recalls being first to obtain the raw material, sell it, and commission testing for the market. This is our account of sourcing history; the analytical report establishes the specimen findings, not a market-wide priority claim.

Handling: The report detects arsenic-bearing minerals in the orange areas. Avoid making dust or ingesting material, and wash hands after handling rough pieces.

View the original report

Select a page to enlarge it. 3 pages; findings are summarized in accessible text above.

Report images © Soul Body Gems, Alexander Falster and the Maine Mineral & Gem Museum. Please acknowledge all three when referring to these results. Findings apply to the specimen examined.

Understanding the report figures

Use this guide alongside the written findings and the original report transcript. It explains the purpose of each analytical figure and preserves the laboratory’s own figure labels. The interpretations apply to the tested specimen; signals alone do not establish the identity of every similar-looking stone.

  • Electron microscope image: This view shows small-scale regions selected for analysis. Its brightness contrast helps distinguish regions with different compositions; it is not a photograph of their natural colors. Numbered spots connect this view to the analyses listed in the report.

    Laboratory figure caption: Fig. 1: Backscattered electron image (Indonesian stones, orange area)

  • Elemental spectrum: The peaks record characteristic X-ray signals from elements in the analyzed spot or area. This is an analysis of that location, not automatically of the entire specimen. Any mineral identification or uncertainty named in the laboratory caption is retained below.

    Laboratory figure caption: Fig. 2: Energy dispersive spectrum of spot 1 in Fig. 1. (quartz).

  • Elemental spectrum: The peaks record characteristic X-ray signals from elements in the analyzed spot or area. This is an analysis of that location, not automatically of the entire specimen. Any mineral identification or uncertainty named in the laboratory caption is retained below.

    Laboratory figure caption: Fig. 3: Energy dispersive spectrum of spot 2 in Fig. 1. (orpiment/realgar).

  • Electron microscope image: This view shows small-scale regions selected for analysis. Its brightness contrast helps distinguish regions with different compositions; it is not a photograph of their natural colors. Numbered spots connect this view to the analyses listed in the report.

    Laboratory figure caption: Fig. 4: Backscattered electron image (Indonesian stones, from the botryoidal surfaces from a cavity)

  • Elemental spectrum: The peaks record characteristic X-ray signals from elements in the analyzed spot or area. This is an analysis of that location, not automatically of the entire specimen. Any mineral identification or uncertainty named in the laboratory caption is retained below.

    Laboratory figure caption: Fig. 5: Energy dispersive spectrum of spot 1 in Fig. 4. (quartz).

  • Electron microscope image: This view shows small-scale regions selected for analysis. Its brightness contrast helps distinguish regions with different compositions; it is not a photograph of their natural colors. Numbered spots connect this view to the analyses listed in the report.

    Laboratory figure caption: Fig. 6: Backscattered electron image (Indonesian stones, from the gray area)

  • Elemental spectrum: The peaks record characteristic X-ray signals from elements in the analyzed spot or area. This is an analysis of that location, not automatically of the entire specimen. Any mineral identification or uncertainty named in the laboratory caption is retained below.

    Laboratory figure caption: Fig. 7: Energy dispersive spectrum of spot 1 in Fig. 7. (quartz with possible indication of remnant plagioclase).

Read the original laboratory report as text

The following text and tables are transcribed from the original laboratory document. Figure captions identify the report images; the laboratory interpretations and limitations are preserved.

Laboratory report 1

Analytical Result Report

Sample id: 9148 (#5 Indonesian stones)

Submitted by: K. Bitner

Date submitted: July 13, 2020

Date completed: July 16, 2020

Operating conditions: JEOL JSM-6400 operated at 25 kV acceleration potential, 15 mm working distance, 15 degrees sample tilt, coated with 250 Å carbon. Using the X-ray fluorescence attachment with 35kv potental in conjunction with the EDS system.

Fig. 1: Backscattered electron image (Indonesian stones, orange area)

Fig. 2: Energy dispersive spectrum of spot 1 in Fig. 1. (quartz).

Fig. 3: Energy dispersive spectrum of spot 2 in Fig. 1. (orpiment/realgar).

Fig. 4: Backscattered electron image (Indonesian stones, from the botryoidal surfaces from a cavity)

Fig. 5: Energy dispersive spectrum of spot 1 in Fig. 4. (quartz).

Fig. 6: Backscattered electron image (Indonesian stones, from the gray area)

Fig. 7: Energy dispersive spectrum of spot 1 in Fig. 7. (quartz with possible indication of remnant plagioclase).

Summary of findings: This is really interesting! The orange areas are essentially quartz (chalcedony) (Figs. 1,2,4, and 5) with orpiment/realgar as coloring agents! (Figs 1 and 3). The gray areas are mainly quartz with minor aluminum, calcium and sodium. It appears that there were initially phenocrysts of plagioclase present (Figs. 6 and 7), likely in a volcanic rock that than underwent hydrothermal overprinting and deposition of a low temperature arsenic sulfide assemblage. XRF analyses of the gray area only indicates 79 ppm arsenic as well as 8500ppm iron, 4500 ppm potassium, 1 et. % calcium and 0.7 wt. % sodium.

The orange areas contain 1650 ppm arsenic, 4600 ppm iron and 250 ppm calcium.

Date: July 16 ,2020 Signature

Report acknowledgment: These analytical results and report materials are the property of Soul Body Gems, Alexander Falster, and the Maine Mineral & Gem Museum. Any use or mention of these results requires full acknowledgment of all three.

← Back to Gem Knowledge

Results shown here apply to the specimens identified in the reports. A trade name or visual resemblance alone does not establish the composition of another piece.