Dream Quartz

Host: SiO2 · Mohs 7 · Trigonal · Crown Chakra

The stone of dream quartz: meaning, mineralogy, and somatic practice.

IntuitionSleep & InsomniaSpiritual ConnectionSelf-Awareness

This page documents traditional and cultural uses of dream quartz alongside emerging research on tactile grounding objects. Crystalis does not claim that dream quartz treats, cures, or prevents any medical condition. For mental health concerns, consult a qualified professional.

Crystalis Editorial · 40+ Years · Herndon, VA · 12 peer-reviewed sources

Origins: Colombia

Quick actions

Move from reference into practice

Save Field Note Try the 3-Minute Reset Take Sacred Match Build My Bracelet Try a Power Vial

Crystalis

Materia Medica

Dream Quartz

The Lucid Dreamer

IntuitionSleep & InsomniaSpiritual Connection

Crystalis

Protocol

The Phantom Gate

Trigonal quartz hosting phantom inclusions of epidote, chlorite, or actinolite — previous crystal faces preserved inside the current one like memories the stone grew around rather than erased.

5 min

1
Hold the dream quartz and look into it carefully. Find the phantom — the ghost crystal visible inside the current crystal. This phantom is a previous termination face that was coated with a thin layer of epidote, chlorite, or actinolite, and then the quartz resumed growing over it. The stone did not shed its past. It grew around it. The earlier face is still there, perfectly preserved inside the later growth.
2
Lie down if possible, or recline. Place the dream quartz on your forehead, between and slightly above the eyebrows. The trigonal quartz host is hardness 7 — firm, cool. The phantom inclusions inside may appear green (chlorite), yellow-green (epidote), or fibrous (actinolite). Close your eyes. The weight of the stone creates a focal point of gentle pressure.
3
Breathe slowly — in for six counts, out for eight. Let the exhale be longer than the inhale. On each inhale, imagine looking into the crystal and seeing the phantom layer. On each exhale, ask: What earlier version of myself is preserved inside my current form? Not as nostalgia. As geology. A layer that growth enclosed but did not erase.
4
Shift attention from the forehead to the body. Scan downward from crown to feet without rushing. The phantom inside dream quartz is visible because the coating mineral has a different refractive index than the surrounding quartz. The earlier self is visible because it reflects light differently than the current self. Notice where in your body an earlier version of you is still reflecting.

Continue in the full protocol below.

tap to flip for protocol

Some minds are not disorganized. They are imagistic. Meaning comes as atmosphere, layered symbol, inner scenery.

Dream quartz honors that mode. Clear quartz hosts green epidote or chlorite-like inclusions in veils, clouds, and internal gardens, keeping lucidity and dream-sense in the same body. The structure never disappears. It simply shares the room with image.

There are truths that want to be seen before they are translated.

What Your Body Knows

Nervous system states

At first contact, dream quartz presents a regulated shell with unsettled interior weather. That visual arrangement is why it speaks so directly to states where the body looks functional from the outside while carrying diffuse activation underneath.

In one common presentation, the nervous system is operating in mixed state: ventral enough to keep going, sympathetic enough to keep scanning. The person appears composed, but imagery intensifies at night, during showers, or in the pause just before sleep. Dream quartz gives that drifting material a container the eyes can track. Internal inclusions suspend rather than spill. The body reads the pattern as motion held inside structure.

It also works clearly with grief states that do not arrive as crying. Some bodies grieve visually instead of verbally. They produce symbols, fragments, old scenes, and dream saturation. Because dream quartz shows depth without collapse, it can serve as an orienting object during those image-heavy periods.

Another use appears in gentle dissociation, when awareness goes misty rather than absent. The clear quartz host provides edge definition. The green interior keeps the object from feeling sterile. That combination helps attention return without force. Dream quartz finds its primary use in bodies carrying layered imagery that needs containment more than interpretation.

sympathetic

Hyper-aroused states, racing thoughts, anxiety spirals, decision paralysis from overthinking

Mechanism of engagement: The phantom interior creates a visual focal point that naturally draws the eye inward and deeper. This "looking through layers" effect parallels the cognitive process of examining thoughts without attachment; a somatic analog to depth work. - Polyvagal context: Supports movement from sympathetic activation (fight/flight) toward ventral vagal engagement (social, reflective) by providing a visual anchoring stimulus that is complex enough to hold attention but non-threatening.

Nervous system mapping based on polyvagal theory (Porges, S.W. The Polyvagal Theory. Norton, 2011).

The Earth Made This

Formation: How Dream Quartz Becomes Dream Quartz

Dream quartz is a trade name for quartz containing green epidote inclusions, typically from Colombia. The epidote crystals were trapped within the quartz during growth, creating green phantoms, wisps, or clusters visible through the clear or translucent quartz host. Epidote forms at temperatures of 200-600°C in metamorphic and hydrothermal environments, and its presence as an inclusion in quartz indicates these conditions were present during the quartz's growth.

The green color of the epidote comes from iron (Fe³⁺) in the crystal structure. The trade name was coined by crystal dealers to describe the dreamy, underwater garden appearance created by the suspended green inclusions.

Material facts

What the stone is made of

Mineralogy: Macrocrystalline quartz with green epidote inclusions. Chemical formula: SiO₂ (host) with Ca₂(Al,Fe³⁺)₃(SiO₄)₃(OH) (epidote inclusions). Crystal system: trigonal (quartz host). Mohs hardness: 7. Specific gravity: 2.65. Color: clear quartz with green epidote inclusions creating internal green phantoms, veils, or clusters. Luster: vitreous (quartz surfaces); inclusions may appear vitreous to silky. Habit: prismatic. Not a distinct mineral species; a trade name for quartz with epidote inclusions. From Colombia.

Deeper geology

Inside this material, the host is ordinary quartz and the visual drama comes from what the quartz enclosed while it grew. Dream quartz is a trade name used for clear to milky macrocrystalline quartz that contains green epidote, chlorite, or other mist-like inclusions, most often in hydrothermal pockets where silica-rich fluids circulated through fractured rock. The quartz host crystallizes in the trigonal system, building from SiO2 tetrahedra linked into a continuous framework. Given open space, it extends as prisms terminated by rhombohedra. Given crowding, it thickens around earlier growth and traps whatever the fluid still carries. What emerges is a crystal body that reads like suspended weather.

The inclusion story matters. Epidote commonly forms in metamorphic and hydrothermal settings rich in calcium, aluminum, and iron. If those minerals are present before quartz growth finishes, the quartz can overtake them. Instead of dissolving the earlier phase, it entombs it. That is why dream quartz often shows plumes, green clouds, phantom ridges, or landscape-like patches rather than neat crystals floating in empty space. The quartz formed later, but the interior scene records a longer sequence of events. In many specimens from Colombia and Brazil, this sequence likely involved repeated pulses of fluid, slight changes in temperature, and short pauses in growth that let inclusion bands settle before the next silica layer sealed them in.

Its physical framework remains straightforward even when the interior looks surreal. The host keeps quartz hardness at Mohs 7, vitreous luster, and specific gravity near 2.65. Any softness the eye perceives belongs to pattern, not structure. The crystal system is still trigonal. The chemistry is still silica-dominant. Only the growth history makes the stone appear dreamlike. In the hand, that split between stable host and drifting interior gives the body a small somatic lesson: containment does not require emptiness. A vessel can stay coherent while holding weather, memory, and motion inside it.

Mineralogy

Mineral specs

Chemical Formula

Host: SiO2

Crystal System

Trigonal

Mohs Hardness

Specific Gravity

2.65

Luster

Vitreous (quartz surfaces); inclusions may appear vitreous to silky

Color

Green-White

Crystal system diagram represents the general trigonal classification. Diagram created by Crystalis for educational reference.

Traditional Knowledge

Lore and culture around Dream Quartz

Science grounds the page. Tradition, lore, and remembered use make it readable as lived knowledge.

Ancient/Classical: Epidote as a distinct mineral was not recognized until 1801, when Rene Just Hauy named it from the Greek "epidosis" (increase/addition), referring to the base of the prism being longer on one side. Quartz with green inclusions would have been collected as curiosities alongside other included quartzes throughout antiquity, but without specific cultural identity. 19th century: Epidote became a recognized mineral species. Specimen collectors prized included quartz from Alpine localities in Switzerland and Austria. Late 20th century: The trade name "Dream Quartz" emerged in the crystal healing and metaphysical community, likely coined by dealers marketing Colombian epidote-included quartz in the 1990s-2000s. The name references the phantom-like internal landscapes said to resemble dreamscapes. 21st century: Dream Quartz has become a significant category in the collector and metaphysical mineral market, with Colombian specimens particularly valued for their clarity and vivid green phantoms.

Unknown

Ancient/Classical

Epidote as a distinct mineral was not recognized until 1801, when Rene Just Hauy named it from the Greek "epidosis" (increase/addition), referring to the base of the prism being longer on one side. Quartz with green inclusions would have been collected as curiosities alongside other included quartzes throughout antiquity, but without specific cultural identity. - 19th century: Epidote became a recognized mineral species. Specimen collectors prized included quartz from Alpine localities in Switzerland and Austria. - Late 20th century: The trade name "Dream Quartz" emerged in the crystal healing and metaphysical community, likely coined by dealers marketing Colombian epidote-included quartz in the 1990s-2000s. The name references the phantom-like internal landscapes said to resemble dreamsca

Sacred Match Notes

When this stone becomes the right door

Sacred Match prescribes Dream Quartz when you report:

Dream saturation

Symbol-heavy grief

Foggy but functional

Nighttime image surges

Holding more than saying

Sacred Match prescribes through physiological diagnosis, not preference. It queries the nervous system: current sensation, protective mechanism, and the biological need masked by both. When that triangulation reveals a body containing large amounts of unspoken visual material without discharge, Dream Quartz enters the protocol. The prescription is based on structure. Clear quartz provides order. Interior inclusions preserve movement inside that order. The body often responds to that combination before language can explain it.

Dream saturation -> image overflow at rest -> seeking contained recall

Symbol-heavy grief -> feeling translated into picture -> seeking witness without force

Foggy but functional -> edges intact, center diffuse -> seeking coherence

Nighttime image surges -> activation after dark -> seeking a visual anchor

Holding more than saying -> expression stalled in the throat -> seeking interior permission The protocol is chosen for fit, not romance. It looks for the clearest material mirror of the body's current pattern and then uses that mirror to support a more stable response.

3-Minute Reset

The Phantom Gate

Trigonal quartz hosting phantom inclusions of epidote, chlorite, or actinolite — previous crystal faces preserved inside the current one like memories the stone grew around rather than erased.

5 min protocol

1
Hold the dream quartz and look into it carefully. Find the phantom — the ghost crystal visible inside the current crystal. This phantom is a previous termination face that was coated with a thin layer of epidote, chlorite, or actinolite, and then the quartz resumed growing over it. The stone did not shed its past. It grew around it. The earlier face is still there, perfectly preserved inside the later growth.
1 min
2
Lie down if possible, or recline. Place the dream quartz on your forehead, between and slightly above the eyebrows. The trigonal quartz host is hardness 7 — firm, cool. The phantom inclusions inside may appear green (chlorite), yellow-green (epidote), or fibrous (actinolite). Close your eyes. The weight of the stone creates a focal point of gentle pressure.
1 min
3
Breathe slowly — in for six counts, out for eight. Let the exhale be longer than the inhale. On each inhale, imagine looking into the crystal and seeing the phantom layer. On each exhale, ask: What earlier version of myself is preserved inside my current form? Not as nostalgia. As geology. A layer that growth enclosed but did not erase.
1 min
4
Shift attention from the forehead to the body. Scan downward from crown to feet without rushing. The phantom inside dream quartz is visible because the coating mineral has a different refractive index than the surrounding quartz. The earlier self is visible because it reflects light differently than the current self. Notice where in your body an earlier version of you is still reflecting.
1 min
5
Remove the stone from your forehead. Sit up slowly. Hold the dream quartz at eye level and look at the phantom one more time. It is not trapped. It is housed. The crystal chose to keep growing rather than fracture along the coated surface. Place the stone down. The phantom you carry is housed, not trapped.
1 min

The #1 Question

Can Dream Quartz go in water?

SAFE for brief rinsing. Quartz is stable in water. However, if epidote or actinolite inclusions are exposed at surface fractures, prolonged soaking is not recommended -- epidote is generally stable but actinolite (an amphibole) should not be subjected to extended water immersion.

Mineral Distinction

What sets Dream Quartz apart

Dealers routinely sell dream quartz under a long list of poetic names, but the buyer should treat it as inclusion quartz and identify the host first. The fastest test is hardness and structure. The outer crystal should behave like quartz: it should resist a steel knife, show vitreous luster, and usually present trigonal prism geometry if left unpolished. If the green material scratches too easily or coats the surface in a chalky layer, the piece may be chrysocolla, dyed quartz, or another copper mineral rather than true inclusion quartz.

What separates dream quartz from garden quartz is mostly trade language, not mineral species. The more useful distinction is between included quartz and surface-stained quartz. A loupe gives the confirming step. In true dream quartz, the green forms sit within the silica body at different depths, often with phantom zoning or plume-like distribution. In dyed or coated material, the color pools in fractures or lies right on the surface. Epidote inclusion identification is what supports the premium, and selling generic green included quartz as dream quartz without verifying the inclusion type is labeling by hope rather than evidence.

Care and Maintenance

How to care for Dream Quartz

Water: SAFE for brief rinsing. Quartz is stable in water. However, if epidote or actinolite inclusions are exposed at surface fractures, prolonged soaking is not recommended .

epidote is generally stable but actinolite (an amphibole) should not be subjected to extended water immersion. Sun/light safety: SAFE. Neither quartz nor epidote/actinolite are photosensitive.

Color will not fade with light exposure. Heat safety: MODERATE CAUTION. Sudden temperature changes can cause internal fracturing along inclusion boundaries due to differential thermal expansion between quartz (alpha = 7.

1 x 10^-6 /K) and epidote (alpha = ~5. 5 x 10^-6 /K). Do not subject to rapid heating or cooling.

Chemical safety: Avoid hydrofluoric acid (dissolves quartz). Dilute acids will not significantly affect quartz but may etch epidote over time. Fiber hazard note: Actinolite is an amphibole mineral.

In its fibrous form (asbestiform actinolite), it is a regulated asbestos mineral. The prismatic inclusions within Dream Quartz are encapsulated in quartz and pose NO inhalation risk . they are fully sealed within the crystal.

However, if a specimen is broken or cut, avoid inhaling any dust. This is a precautionary note, not a general hazard for intact specimens. Ultrasonic cleaning: Use with caution.

Internal inclusion boundaries may be stressed by ultrasonic vibration.

Crystal companions

What pairs well with Dream Quartz

Epidote Anchor. Pair dream quartz with black tourmaline when the inner image stream feels richer than the outer boundary. Dream quartz already holds green inclusion matter inside clear structure, so black tourmaline gives that softness a perimeter. Place dream quartz on the sternum and keep black tourmaline in the front pocket during journaling. One supports symbolic material. The other keeps the room simple.

Lucid Lens. Pair it with amethyst for dream recall, image work, and quieter sleep transitions. Amethyst contributes mental cooling while dream quartz keeps the visual language intact. Set dream quartz on the nightstand and tuck amethyst under the pillow corner. The placement matters because one stone stays visible and one works closer to the head.

Interior Landscape. Pair it with garden quartz if the intention is to work with layered memory rather than single insight. Dream quartz tends to read as mist, plume, or green weather. Garden quartz often looks more architectural, with inclusions resembling terrain. Place both on a desk, dream quartz to the left and garden quartz to the right, so the eye moves from atmosphere to landform.

Clear Signal. Add clear quartz when the dream material is present but hard to translate. Clear quartz functions as an amplifier without changing the basic chemistry of the host family. Lay a clear quartz point just above dream quartz in a small grid on the bedside table. Best when the goal is to remember rather than interpret.

In Practice

How Dream Quartz is used

- Primary indication: Hyper-aroused states, racing thoughts, anxiety spirals, decision paralysis from overthinking - Mechanism of engagement: The phantom interior creates a visual focal point that naturally draws the eye inward and deeper. This "looking through layers" effect parallels the cognitive process of examining thoughts without attachment. a somatic analog to depth work. - Polyvagal context: Supports movement from sympathetic activation (fight/flight) toward ventral vagal engagement (social, reflective) by providing a visual anchoring stimulus that is complex enough to hold attention but non-threatening.

- During reflective journaling or meditation practices focused on inner landscape exploration - When processing layered or complex emotional material (the phantom layers mirror psychological layering) - Transition work. moving between life phases, integrating old patterns with new growth - Evening wind-down practices when the nervous system needs help shifting from active to receptive

- During dissociative states or depersonalization episodes. the "dreamy" quality could reinforce disconnection from present-moment reality - When grounding and strong earth-connection are needed (use denser, more opaque stones instead) - In acute crisis situations requiring immediate nervous system stabilization (too subtle for acute activation)

Verification

Authenticity

Dream quartz: green epidote inclusions should be INSIDE the quartz (Mohs 7). The green phantoms, wisps, or clouds should be visible through the transparent host. If green is only on the surface, it is coating.

Specific gravity 2. 65. Colombian provenance is standard for the trade name.

Temperature

Natural Dream Quartz should usually feel cooler than plastic or resin on first touch and warm more slowly in the hand.

Scratch logic

Use 7 on the Mohs scale as the check, not internet myths. A real specimen should behave in line with the hardness listed above.

Surface and luster

Look for a vitreous (quartz surfaces); inclusions may appear vitreous to silky surface quality rather than a painted or plastic shine.

Weight and density

The listed specific gravity is 2.65. If a specimen feels unusually light for its size, it may deserve a second look.

Geographic Origins

Where Dream Quartz forms in the world

Colombia: Eastern Cordillera, Boyaca and Cundinamarca departments (primary source of commercial "Dream Quartz") Brazil: Minas Gerais, Bahia (epidote-included quartz) Switzerland: Central Alps . Aar Massif, Gotthard Massif, Graubunden (Alpine fissure veins with epidote + quartz) Pakistan: Northern Areas, Gilgit-Baltistan (epidote phantoms in quartz) Austria: Tyrol, Salzburg (Alpine fissure epidote-quartz) India: Karnataka, Tamil Nadu (metamorphic-hosted quartz with epidote)

The Colombian localities, which produce many specimens marketed as Dream Quartz, are situated in the Eastern Cordillera geological province . the same tectonic belt that hosts world-famous emerald deposits. The region's complex geological history includes Cretaceous sedimentary basin formation, subsequent Andean orogenesis, and extensive hydrothermal fluid circulation through shale and limestone sequences. These fluids, rich in silica, calcium, aluminum, and iron, precipitated quartz with epidote-actinolite inclusions in extensional fractures and fault zones. The geological setting shares characteristics with Alpine-type fissure veins found in Switzerland, where similar epidote-bearing quartz assemblages occur in metamorphic cavities (Leon et al., 2023, doi:10.1111/ter.12668; Weisenberger & Bucher, 2010, doi:10.1111/j.1525-1314.2010.00895.x).

FAQ

Frequently asked

What is Dream Quartz?

Dream Quartz is classified as a 75.1.3.1. Chemical formula: - **Host:** SiO2 (silicon dioxide). Crystal system: **Quartz host:** Trigonal (hexagonal scalenohedral, class 32).

Can Dream Quartz go in water?

Can Dream Quartz go in the sun?

SAFE. Neither quartz nor epidote/actinolite are photosensitive. Color will not fade with light exposure.

What crystal system is Dream Quartz?

Dream Quartz crystallizes in the **Quartz host:** Trigonal (hexagonal scalenohedral, class 32).

What is the chemical formula of Dream Quartz?

The chemical formula of Dream Quartz is - **Host:** SiO2 (silicon dioxide).

Where is Dream Quartz found?

- Colombia: Eastern Cordillera, Boyaca and Cundinamarca departments (primary source of commercial "Dream Quartz") - Brazil: Minas Gerais, Bahia (epidote-included quartz) - Switzerland: Central Alps -- Aar Massif, Gotthard Massif, Graubunden (Alpine fissure veins with epidote + quartz) - Pakistan: Northern Areas, Gilgit-Baltistan (epidote phantoms in quartz) - Austria: Tyrol, Salzburg (Alpine fissure epidote-quartz) - India: Karnataka, Tamil Nadu (metamorphic-hosted quartz with epidote) ---

How does Dream Quartz form?

Dream Quartz forms in hydrothermal vein systems where quartz crystals grow in open cavities (fissures, vugs) within metamorphic or metasomatic rock. The distinctive phantom-like green inclusions arise from episodic changes in the hydrothermal fluid chemistry during crystal growth. Quartz grows during one phase of fluid circulation, then a pause or shift in conditions allows epidote and/or actinolite to nucleate on the crystal surface. When quartz growth resumes, it encapsulates these mineral coa

References

Sources and citations

Ren, Y. F., Chen, D. L., Kelsey, D. E., Gong, X. K., Liu, L. et al. (2018). Metamorphic evolution of a newly identified Mesoproterozoic oceanic slice in the Yuka terrane and its implications for a multi‐cyclic orogenic history of the North Qaidam<scp>UHPM</scp>belt. Journal of Metamorphic Geology. [SCI]
DOI: 10.1111/jmg.12300
Torres Sánchez, Sonia Alejandra, Augustsson, Carita, Barboza Gudiño, José Rafael, Jenchen, Uwe, Ramírez Fernández, Juan Alonso et al. (2015). Magmatic source and metamorphic grade of metavolcanic rocks from the Granjeno Schist: was northeastern Mexico a part of Pangaea?. Geological Journal. [SCI]
DOI: 10.1002/gj.2702
Kurosawa, Masanori, Ishii, Satoshi, Sasa, Kimikazu. (2010). Trace‐element compositions of single fluid inclusions in the Kofu granite, Japan: Implications for compositions of granite‐derived fluids. Island Arc. [SCI]
DOI: 10.1111/j.1440-1738.2009.00702.x
Wang, Yu, Qiu, Kun‐Feng, Müller, Axel, Hou, Zhao‐Liang, Zhu, Zhi‐Hai et al. (2021). Machine Learning Prediction of Quartz Forming‐Environments. Journal of Geophysical Research: Solid Earth. [SCI]
DOI: 10.1029/2021JB021925
Bernardis, Sarah, Newman, Bonna K., Di Sabatino, Marisa, Fakra, Sirine C., Bertoni, Mariana I. et al. (2011). Synchrotron‐based microprobe investigation of impurities in raw quartz‐bearing and carbon‐bearing feedstock materials for photovoltaic applications. Progress in Photovoltaics: Research and Applications. [SCI]
DOI: 10.1002/pip.1126
Manalo, Pearlyn C., Subang, Leo L., Imai, Akira, de los Santos, Mervin C., Takahashi, Ryohei et al. (2019). Geochemistry and Fluid Inclusions Analysis of Vein Quartz in the Multiple Hydrothermal Systems of Mankayan Mineral District, Philippines. Resource Geology. [SCI]
DOI: 10.1111/rge.12214
Giuntoli, Francesco, Viola, Giulio, Sørensen, Bjørn Eske. (2022). Deformation Mechanisms of Blueschist Facies Continental Metasediments May Offer Insights Into Deep Episodic Tremor and Slow Slip Events. Journal of Geophysical Research: Solid Earth. [SCI]
DOI: 10.1029/2022JB024265
León, Santiago, Jiménez‐Rodríguez, Sebastián, Piraquive, Alejandro, Florez‐Amaya, Sandra, Muñoz‐Rocha, Jimmy et al. (2023). Sediment provenance signal of the discontinuous retroarc topography in the northern Andes during the Early Cretaceous. Terra Nova. [SCI]
DOI: 10.1111/ter.12668
Papeschi, Samuele, Musumeci, Giovanni, Massonne, Hans‐Joachim, Mazzarini, Francesco, Ryan, Eric James et al. (2020). High‐<i>P</i> (<i>P</i> = 1.5–1.8 GPa) blueschist from Elba: Implications for underthrusting and exhumation of continental units in the Northern Apennines. Journal of Metamorphic Geology. [SCI]
DOI: 10.1111/jmg.12530
Yoshida, Takumi, Taguchi, Tomoki, Ueda, Hayato, Horie, Kenji, Satish‐Kumar, M. (2020). Early Carboniferous HP metamorphism in the Hida Gaien Belt, Japan: Implications for the Palaeozoic tectonic history of proto‐Japan. Journal of Metamorphic Geology. [SCI]
DOI: 10.1111/jmg.12564
WEISENBERGER, T., BUCHER, K. (2010). Zeolites in fissures of granites and gneisses of the Central Alps. Journal of Metamorphic Geology. [SCI]
DOI: 10.1111/j.1525-1314.2010.00895.x
Cartwright, I., Buick, I. S. (2000). Fluid generation, vein formation and the degree of fluid–rock interaction during decompression of high‐pressure terranes: the Schistes Lustrés, Alpine Corsica, France. Journal of Metamorphic Geology. [SCI]
DOI: 10.1046/j.1525-1314.2000.00280.x

Closing Notes

Dream Quartz

Green epidote inclusions trapped inside quartz during growth. Green phantoms and wisps sealed inside transparency. The science documents how one mineral preserves another by growing around it.

The practice asks what dreams look like when they are mineral inclusions frozen in a crystal body.

Field Notes