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Conichalcite, CaCu(AsO4)(OH), is a relatively common arsenate mineral related to duftite (PbCu(AsO4)(OH)). It is green, often botryoidal, and occurs in the oxidation zone of some metal deposits. It occurs with limonite, malachite, beudantite, adamite, cuproadamite, olivenite and smithsonite.
The analysis highlights Formation and Overview as prominent areas in the source structure around Conichalcite.
Source areas are shown by the number of related topics found in each part of the analysis. Use smaller areas too: they can reveal specialized angles and content gaps.
Smaller areas are not necessarily less important. They contain fewer connections in this analysis and can be useful for finding specialized angles or coverage gaps.
High-confidence facts extracted from structured source data. Use them as anchors for further research.
Browse the complete topic structure, not only the most central items. Less prominent entities and concepts can reveal missing angles, specialized context and useful research gaps. Each item opens a new analysis centered on that subject.
Deeper signals for content research, entity SEO and topical coverage. The plain-language headings explain what each technical view is useful for.
The extracted context around Conichalcite shows recurring relationship patterns in the source. For example, Conichalcite → Here, When Another extracted example is Conichalcite → δ = 0.023 – 0.046. Use these groups to spot repeated connection types before inspecting the individual relationships.
Use these terms to understand the vocabulary surrounding the topic, not as a checklist for keyword stuffing.
green occurs botryoidal oxidation malachite minerals cacu aso4 oh arsenate references series mineral often crystal crusts copper calciovolborthite arsenic vanadium
TTTA extracted 31 structured relationships around Conichalcite. Examples in this analysis include Conichalcite → Birefringence → δ = 0.023 – 0.046 and Conichalcite → Category → Arsenate minerals. The table shows each extracted connection, where it came from and its confidence.
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Conichalcite | Birefringence | δ = 0.023 – 0.046 | 1.00 | infobox |
| Conichalcite | Category | Arsenate minerals | 1.00 | infobox |
| Conichalcite | Cleavage | Absent | 1.00 | infobox |
| Conichalcite | Color | Grass-green to yellowish green, pistachio-green, emerald-green; may be zoned; light green to yellowish green in transmitted light. | 1.00 | infobox |
| Conichalcite | Crystal class | Disphenoidal (222) (same H-M symbol) | 1.00 | infobox |
| Conichalcite | Crystal habit | Crusts of acicular to almost fibrous crystals. Also as botryoidal masses and compact crusts. | 1.00 | infobox |
| Conichalcite | Crystal system | Orthorhombic | 1.00 | infobox |
| Conichalcite | Dana classification | 41.5.1.2 | 1.00 | infobox |
| Conichalcite | Diaphaneity | Translucent | 1.00 | infobox |
| Conichalcite | Dispersion | Strong r < v to r < v moderate | 1.00 | infobox |
| Conichalcite | Formula | CaCu(AsO4)(OH) | 1.00 | infobox |
| Conichalcite | Fracture | Uneven | 1.00 | infobox |
| Conichalcite | IMA symbol | Con | 1.00 | infobox |
| Conichalcite | Luster | Vitreous, greasy | 1.00 | infobox |
| Conichalcite | Mohs scale hardness | 4.5 | 1.00 | infobox |
| Conichalcite | Optical properties | Biaxial (+/−) | 1.00 | infobox |
| Conichalcite | Pleochroism | Visible | 1.00 | infobox |
| Conichalcite | Refractive index | nα = 1.778 – 1.800 nβ = 1.795 – 1.831 nγ = 1.801 – 1.846 | 1.00 | infobox |
| Conichalcite | Space group | P212121 | 1.00 | infobox |
| Conichalcite | Specific gravity | 4.3 | 1.00 | infobox |
| Conichalcite | Streak | Green | 1.00 | infobox |
| Conichalcite | Strunz classification | 8.BH.35 | 1.00 | infobox |
| Conichalcite | Tenacity | Brittle | 1.00 | infobox |
| Conichalcite | Twinning | Rare on {001} | 1.00 | infobox |
| Conichalcite | Unit cell | a = 7.39(1) Å, b = 9.23(1) Å, c = 5.83(1) Å; V = 397.66 ų; Z = 4 | 1.00 | infobox |
| Conichalcite | is a | arsenic rich end member of the series and calciovolborthite is the vanadium rich end member.Notable occurrences of conichalcite include Juab Co | 0.90 | text |
The concept neighborhoods around Conichalcite bring nearby vocabulary together. In this analysis, examples include Calciovolborthite, Mineral and References. Use the clusters to find adjacent concepts and terminology that may deserve separate research.
For Conichalcite, one of the stronger structural bridges in this analysis connects Conichalcite with Formation. Bridges highlight paths between different parts of the map and can reveal research angles that are easy to miss in a flat list.
TTTA analyzes the structure around Conichalcite to surface related topics, entities, relationships, concept neighborhoods and bridge connections. Use the map to explore areas such as Formation & Overview, including less central topics that may reveal useful research gaps. Automatically extracted connections are research leads rather than rewritten encyclopedia content.
Source: Wikipedia — Conichalcite · EN edition · Analysis: TopicsToTalkAbout