Fact-checked by Grok 2 weeks ago

Howlite

Howlite is a calcium with the Ca₂B₅SiO₉(OH)₅, belonging to the inoborate group, and typically appears as white or colorless porcelaneous nodules, masses, or veins marked by gray, black, or brown intersecting patterns resembling . Named after Canadian and Henry How (1828–1879), who first identified and described the mineral in 1868 from specimens collected in , howlite was initially termed silicoborocalcite before being renamed by in 1868. It crystallizes in the monoclinic system, though it rarely forms distinct crystals and instead occurs in compact, massive habits. Physically, howlite has a Mohs of 3.5 in its massive form (up to 6.5 for rare ), a specific of 2.58–2.62, and a sub-vitreous to dull luster, with perfect cleavage in and a white streak. It is translucent to opaque, soluble in , and exhibits weak under light, appearing orange or bluish-white. Howlite forms in evaporitic environments through the alteration of boron-rich or in arid or semi-arid conditions, often associated with other borates like and , as well as and in sedimentary deposits. Notable occurrences include the region in , ; the Kramer District in California's ; and deposits in , , and . Due to its attractive veining and relatively low cost, howlite is primarily valued as an ornamental stone for carvings, cabochons, beads, and decorative objects, and it is frequently dyed blue or green to imitate in jewelry. Its softness limits industrial applications, though it has minor historical use in small sculptures.

Properties

Chemical Composition

Howlite is a classified within the inoborates group, specifically as an ino-triborate borosilicate, characterized by its chain-like structures. Its ideal is \ce{Ca2B5SiO9(OH)5}, representing a calcium borosilicate where calcium cations are balanced by a complex polyanion consisting of silicate and borate tetrahedra along with hydroxyl groups. This composition accounts for approximately 13.8% boron by weight, underscoring its significance as a boron-bearing mineral. The of howlite is monoclinic, belonging to the P2_1/c with four formula units per (Z = 4). parameters are typically a = 12.82 , b = 9.351 , c = 8.608 , and β ≈ 104.8°. In this arrangement, calcium atoms are coordinated by eight oxygen and hydroxyl atoms, forming distorted polyhedra that link the together. Boron plays a central role in howlite's structure by forming tetrahedral coordination polyhedra, such as isolated \ce{BO4} and \ce{BO3(OH)} units, which integrate with tetrahedra to create colemanite-like chains and silicoborate spirals. These boron-centered chains run parallel and are interconnected via shared oxygen atoms and involving the hydroxyl groups, resulting in a layered-like that imparts stability to the . While the ideal formula predominates, some specimens exhibit minor substitutions, including sodium and as common impurities replacing calcium or altering site occupancies, though magnesium or iron substitutions are not typically reported in standard analyses.

Physical Characteristics

Howlite is typically or colorless, often exhibiting gray, black, or brown veining that gives it a marbled appearance resembling or other stones. This veining occurs naturally in its nodular formations, contributing to its distinctive aesthetic. In terms of durability, howlite registers 3.5 on the Mohs hardness scale in massive form (up to 6.5 for rare crystals). Its specific gravity ranges from 2.58 to 2.62, making it lightweight compared to many other minerals. The mineral displays a luster that varies from dull to sub-vitreous or porcelaneous, with a conchoidal to uneven and no distinct . It produces a streak and is generally opaque to translucent, though rare crystalline forms may show greater . Howlite commonly forms in compact nodular or massive habits, often with a chalky, earthy texture attributed to its composition, and it has a of approximately 1.59 to 1.60. It is soluble in hydrochloric acid, forming a gelatinous silica residue, and exhibits weak under light, appearing orange or bluish-white. These traits make it easy to handle but prone to absorption, influencing its use in polished forms.

Formation and Occurrence

Geological Formation

Howlite is a secondary that primarily forms in deposits through the reaction of boron-rich hydrothermal solutions with calcium-bearing host rocks such as or . These solutions, often derived from volcanic or geothermal activity leaching from surrounding bedrock, infiltrate and interact with the carbonates under evaporative conditions in arid, closed-basin lacustrine or environments, leading to the precipitation of howlite as nodules, veins, or masses. The formation process is typically diagenetic, occurring contemporaneously with the of minerals like and , where howlite develops from silica- and -enriched gels or brines in unconsolidated sediments. Host rocks commonly include evaporitic sequences of clays, marls, and limestones, as well as altered volcanic tuffs or basalts in boron-enriched settings; in some cases, it appears in contact metamorphic zones or altered ultramafic rocks where boron mobilization enhances . Formation conditions involve low temperatures, generally under 100°C, in concentrated, alkaline brines driven by and fluid circulation along faults or fractures. Howlite shares paragenesis with other borates such as and , often forming in alternating layers or replacing primary borates during burial diagenesis in these environments, reflecting sequential based on evolving chemistry and silica availability. Its nodular or cauliflower-like further indicates in low-energy, stable depositional settings.

Major Deposits

The type locality for howlite is near , , where it was discovered in 1868 within and deposits formed in evaporative environments. Significant deposits occur in the same region, including Iona on , where howlite forms nodules embedded in anhydrite matrices along ancient sequences from the Windsor Sea. In the United States, a key deposit is at Tick Canyon in , part of a borate-rich sequence where howlite nodules are found alongside other in volcanic and sedimentary beds. Another notable site is the East Kramer borate area near , in the , yielding large nodules from open-pit operations historically focused on extraction. Mexico hosts deposits in Baja California, including areas near the border region, where howlite occurs in evaporite settings similar to those in California. Other occurrences include the Pobrdje mine in Serbia's Jarandol Basin, with minor howlite associated with colemanite in boron-bearing layers. Howlite is commonly associated with gypsum, anhydrite, and calcite in these evaporite deposit matrices, occasionally with serpentine in altered zones. Mining primarily involves open-pit methods to extract nodules from gypsum quarries or borate operations, with Canada serving as the historical main source of commercial production.

History

Discovery

Howlite was first noted in the early as unusual white nodules occurring within deposits in , , where they were regarded by miners as impurities disrupting the quality of the extracted material, though no formal scientific identification was made at the time. These nodules, often as large as a man's fist, were encountered during gypsum quarrying operations that began in the 1820s near . The mineral was formally discovered in 1868 by Canadian chemist, geologist, and mineralogist Henry How (1828–1879), a at in , who was alerted to the specimens by local gypsum miners at a on the Clifton Estate in Brookville. How initially mistook the compact, white, cauliflower-like nodules for a novel boron-containing compound and named it silicoborocalcite based on his preliminary observations. Through chemical tests, including qualitative analysis for via coloration and quantitative assays revealing significant content alongside calcium and silica, How confirmed its unique borosilicate composition, distinguishing it from known minerals. How's findings were published in the in 1868, marking the first scientific description of the . Shortly thereafter, American geologist renamed it howlite in honor of its discoverer, solidifying its recognition as a distinct species within the group by the early . This transition elevated the local curiosity from a mining nuisance to a formally accepted borosilicate in geological .

Etymology and Early Uses

The mineral derives its name from Canadian chemist, geologist, and Henry How (1828–1879), who first described it in 1868. It was initially classified as silicoborocalcite based on its borate composition, but American James D. soon renamed it howlite to honor How's analytical contributions to its identification. In the late , howlite attracted scientific interest in due to its content, contributing to studies of regional deposits and geology. Although no large-scale extraction attempts materialized—given howlite's limited abundance compared to other borates like —its presence advanced understanding of local . By the late , howlite had evolved from a curiosity for mineral collectors to an ornamental material, with specimens from being carved into small decorative items, cabochons, and early jewelry elements for their porcelain-like appearance and ease of working. In the early , additional specimens from deposits expanded its availability for such uses. This shift reflected growing appreciation for its aesthetic qualities beyond scientific analysis.

Uses

Jewelry Applications

Howlite is commonly fashioned into beads, cabochons, carvings, and tumbled stones for use in necklaces, earrings, bracelets, and other adornments, leveraging its uniform white color and veined patterns for aesthetic appeal. Its porous structure allows howlite to readily absorb dyes, enabling it to imitate more valuable gemstones such as turquoise with blue-green hues, lapis lazuli with deep blue tones, or malachite with green variations; this dyeing process involves soaking the stone in pigment solutions followed by heating to set the color. Due to its relative softness (Mohs hardness of 3–3.5), howlite requires careful handling in jewelry to prevent scratching or chipping, and it should avoid prolonged water exposure or acidic substances, as it is partially soluble in dilute acids; cleaning is best done with a soft cloth and mild soapy water, followed by immediate drying and occasional polishing to maintain luster. Undyed howlite typically retails for $0.30–$1 per , making it an inexpensive option that gains popularity in and Native American-inspired designs, where its affordability supports elaborate and carvings without compromising style. Originally employed in the primarily as an imitation for and other stones, howlite transitioned by the 2000s into a widely accepted affordable alternative in mainstream jewelry, valued for its versatility rather than solely as a simulant.

Other Applications

Howlite is frequently carved into small sculptures, bookends, and figurines that highlight its distinctive white color and gray veining, making it a popular choice for decorative home accents such as coasters, wind chimes, bowls, and vases. It is also used in architectural elements like countertops and tiles for its marble-like appearance. These objects leverage the mineral's porcelain-like texture and relative ease of , though its softness limits it to finer, non-structural pieces. Its also allows for occasional to enhance aesthetic appeal in decorative items. In metaphysical and spiritual practices, howlite is valued for its purported calming properties, believed to absorb negative emotions like , reduce stress and anxiety, and alleviate by soothing the mind and . It is commonly incorporated into aids, such as grids or tumbled stones placed under pillows for restful sleep, and is associated with enhancing focus, emotional healing, and spiritual awareness, particularly linked to the . Though primarily ornamental, howlite has minor industrial applications due to its content and physical properties. It has served as a source for extraction to produce and other compounds through processes like solvent extraction from calcium . Culturally, howlite features in modern Native American crafts, where it is shaped into small sculptures, sacred objects, and beads. In contemporary products, it appears in items like tumbled stones, , and diffusers, capitalizing on its soothing reputation. Mining of howlite, particularly from low-impact deposits in , —the primary commercial source—employs environmentally friendly practices that minimize habitat disruption and adhere to sustainable extraction standards. These operations focus on selective excavation of evaporite deposits, supporting ongoing availability without significant ecological harm.

Identification and Varieties

Distinguishing Features

Howlite is readily identifiable in its natural state by its characteristic spiderweb-like veining patterns consisting of gray to black inclusions, which form within compact nodules and distinguish it from other white minerals. These threadlike impurities, often resembling erratic webs, are a hallmark of howlite's massive habit and result from associated mineral inclusions during formation. Practical field tests confirm howlite's softness, with a Mohs of 3.5, allowing it to be scratched by a penny (approximately Mohs 3) but not by a (Mohs 5.5). Due to its relatively high thermal conductivity compared to synthetics like , natural howlite feels noticeably cool to the touch when held in the hand. A key diagnostic chemical test involves exposing howlite to dilute (HCl), where it may exhibit mild fizzing if calcium carbonate impurities are present, though pure specimens dissolve slowly without , forming a gelatinous silica residue. Under longwave (UV) light, howlite displays weak white to bluish-white , providing another authentication trait, particularly in nodular samples. Advanced identification relies on spectroscopic methods, such as (XRF) analysis, which reveals distinct peaks alongside calcium and , confirming howlite's borosilicate composition (Ca₂B₅SiO₉(OH)₅). This elemental signature sets it apart from similar borates formed in environments.

Treatments and Imitations

Howlite, due to its natural , readily absorbs dyes and resins, making it susceptible to various treatments that enhance its appearance and durability for commercial use. Common treatments include dyeing with synthetic colors to mimic more valuable gems, such as ; this process often involves cobalt-based dyes to achieve a hue, allowing howlite to be marketed as an affordable alternative. Additionally, stabilization with colorless resins is applied to improve and prevent crumbling, as untreated howlite has a Mohs hardness of only 3.5, rendering it prone to wear in jewelry. Imitation materials frequently substitute for howlite in the market, including , which shares similar white coloration and veining but possesses greater (3.5-5) and a sticky when licked due to its magnesium composition. White serves as another low-cost fake, offering a comparable marbled look but with higher and lack of , while plastic replicas, often molded and dyed, exhibit uniformity and lightness that natural stones lack. Detection methods for treated or imitation howlite include testing for dye bleeding by immersing the stone in hot water, where synthetic colors may leach out, revealing the treatment; under ultraviolet (UV) light, uneven fluorescence or a lack of natural glow can indicate artificial coloration in dyed specimens. Density tests further distinguish fakes, as genuine howlite has a specific gravity of 2.5-2.6, while plastics register lower (around 1.3-1.5) and feel unnaturally light. Ethical concerns in the gem trade center on disclosure requirements, with organizations like the emphasizing that non-disclosure of treatments or mislabeling as " howlite" deceives consumers and undermines market integrity; such practices are prevalent. The use of howlite imitations surged in the amid turquoise scarcity, as major deposits like those in the Southwest depleted, prompting manufacturers—particularly in —to dye and stabilize howlite and similar stones to meet demand for affordable jewelry components during that era.

References

  1. [1]
    Howlite: Mineral information, data and localities.
    Howlite ; Hardness: 6½ ; Specific Gravity: 2.62 ; Crystal System: Monoclinic ; Name: First described as silicoborocalcite by Henry How (11 July 1828, London, ...
  2. [2]
    [PDF] Borate minerals from the Kramer district, Mohave Desert, California
    The development of the borate deposits of the Kramer dis trict, in the Mohave Desert, Calif., received a strong impulse in 1926 by the discovery there of'a ...
  3. [3]
    Howlite Gem Guide and Properties Chart - Gemstones.com
    Howlite is a basic calcium silico-borate that is used for ornamental and decorative objects. It is whitish or cream in color often with gray or brown veining.
  4. [4]
  5. [5]
    Howlite Mineral Data - Mineralogy Database
    Howlite's chemical formula is Ca2B5SiO9(OH)5. It is colorless or white, translucent, with a density of 2.58, and a hardness of 2.5-3.5. It is found in arid ...
  6. [6]
    [PDF] crystal structure of the calcium silicoborate, howlite
    These two structural features link through o(4) oxygen atoms, which are common to the silicate tetrahedra and borate tetrahedra of two colemanite-like chains.
  7. [7]
    Howlite | Properties, Formation, Occurrence - Geology Science
    May 13, 2023 · Magnesite is composed of magnesium carbonate (MgCO3), while howlite is a calcium borosilicate hydroxide. Magnesite is sourced from various ...
  8. [8]
    Howlite gemstone information - Gemdat.org
    It often forms in nodules which resemble cauliflower heads. The nodules are opaque, white with gray or black veins, often showing web-like pattern.
  9. [9]
    Howlite Gemstone: Properties, Meanings, Value & More
    ### Summary of Howlite Jewelry Applications
  10. [10]
    Howlite – Mineral and Healing Properties - Kidz Rocks
    May 1, 2025 · Because of its porous texture, howlite can be easily dyed to imitate other minerals, especially turquoise because of the superficial similarity ...
  11. [11]
    None
    ### Summary of Borate Formation from https://saltworkconsultants.com/downloads/57%20Borates.pdf
  12. [12]
    Contributions of arid climate and hydrothermal fluid flow on ...
    May 23, 2025 · Howlite forms fine-grained milky to white aggregates, nodular masses or wormlike bodies within clay-rich groundmass. It forms along the ...2 Geological Setting · 4.1 Depositional... · 5.1 Depositional...<|control11|><|separator|>
  13. [13]
    [PDF] HOWLITE AND UTEXITE FROM THE CARBONIFEROUS GYPSUM ...
    The howlite is believed to have been formed from a gel; the formation of the borates was contempo- ran€ous with the precipitation of calcium sulphate. Borate ...
  14. [14]
    [PDF] Geology of the Monte Blanco Borate Deposits, Furnace Creek Wash ...
    The howlite commonly occurs as a white mineral that has a satiny micaceous sheen on fresh surfaces. It has roughly columnar structure developed ...
  15. [15]
    [PDF] Howlite Ca2B5SiO9(OH)5
    Distribution: In Canada, near Windsor; at Wentworth; large crystals on the shore of Bras. D'Or Lake, 2.5 km south of Iona, Cape Breton Island, Nova Scotia.
  16. [16]
    The Mineralogy of Nova Scotia - Howlite
    Howlite has since been found throughout the deposits that were formed by the Windsor Sea. It has been reported from Cape Breton (Dingwall and Iona), ...<|control11|><|separator|>
  17. [17]
    None
    Nothing is retrieved...<|control11|><|separator|>
  18. [18]
    Canada's Boron One to refurbish Pobrdje colemanite mine in Serbia
    May 7, 2025 · The boron bearing minerals found at Pobrdje include primarily colemanite with minor howlite. The Piskanja Project is a boron deposit with a ...Missing: Boronik | Show results with:Boronik
  19. [19]
  20. [20]
    [PDF] Data of Geochemistry - USGS Publications Warehouse
    This is the sixth edition of 'Data of Geochemistry', covering topics like chemical elements, Earth's composition, and marine evaporites.<|separator|>
  21. [21]
  22. [22]
    Howlite Value, Price, and Jewelry Information
    Jul 1, 2018 · Howlite is frequently dyed blue to resemble turquoise, and it makes a most convincing simulant. The white material is relatively unexciting in ...
  23. [23]
    Turquoise Howlite : Properties, Formation, Uses, Locations
    Jul 1, 2024 · Ornamental Use: In addition to jewelry making, Turquoise Howlite is also popular for ornamental use in sculptures, carvings, and decorative ...
  24. [24]
    How to Care for Howlite? - Rock Identifier
    Howlite should not be submerged in water or exposed to intense light and heat due to the risk of structural weakening, discoloration, and possible damage.Missing: instructions solubility
  25. [25]
    Howlite Gemstone Information: Your Essential Guide
    ### Summary of Howlite Uses Beyond Jewelry
  26. [26]
    Process for the preparation of boric acid from colemanite and/or ...
    In that method treats minerals containing calcium borate, such as colemanite and howlite, are treated to recover useful boron compounds from said minerals.
  27. [27]
  28. [28]
    Gemstone - Howlite, its Meaning, History and Uses - MYKU
    Howlite is believed to open attunement and prepare the mind to receive wisdom. Howlite absords your anger and any that is directed toward you. Howlite ...
  29. [29]
  30. [30]
    Howlite
    Longwave UV (365nm) colors: Orange , Bluish White ,. Shortwave UV (254nm) colors: Orange , Bluish White ,. Do you have a photo of this mineral you would like ...
  31. [31]
    Dyed Howlite and Magnesite - The Turquoise Impostors
    Most likely it is one of two other minerals, howlite or magnesite, that have been skillfully dyed to colors so similar to turquoise that it fools almost ...
  32. [32]
  33. [33]
    Howlite, Imitation Turquoise, dyed treatment. - Jie Hong Gem
    Sep 23, 2022 · Howlite, white color with gray or black veining, is a natural gemstone that promotes peace and clarity. Ideal for stress relief, ...
  34. [34]
    Complete Buyer's Guide for Howlite Gemstone
    Aug 5, 2020 · Howlite is a borate mineral found in the evaporite deposits. This versatile gemstone has the texture of unglazed porcelain and is usually found in irregularly ...
  35. [35]
  36. [36]
    Magnesite VS Howlite - How to Tell Them Apart - Rock Seeker
    When tested, magnesite will show a RI of 1.509-1.700, and howlite will show 1.583-1.608. Hydrochloric Acid Test. For this test, you'll need a couple of spare ...
  37. [37]
    Fake Turquoise ID - is it Howlite, Magnesite, plastic, resin, or real?!
    A few simple ways to identify fake Turquoise pieces, one of the most faked stones sold online today. Is it Turquoise, Magnesite, Howlite, resin, or plastic?Missing: marble | Show results with:marble
  38. [38]
  39. [39]
  40. [40]
  41. [41]
    An Introduction to Gem Treatments - GIA
    A guide describing frequently encountered gem treatment processes, their detection, and special care tips for treated gems.Surface Coating · Fracture Or Cavity Filling · Heat Treatment
  42. [42]
    Turquoise vs Howlite: Key Differences, Identification & Buying Tips
    Apr 9, 2025 · ... Egypt, El Salvador, Equatorial Guinea, Estonia, Falkland Islands, Faroe ... Many jewelry pieces labeled as turquoise are actually dyed howlite.
  43. [43]
    Magnesite, Howlite & Turquoise
    Aug 20, 2021 · Especially in the 60s to 90s of the last century large quantities of these fake turquoises were offered. After the deposits dried up, genuine ...
  44. [44]
    Turquoise History - Durango Silver Company
    Chinese manufacturers found Magnisite, Howlite and a few other types of white chalk and began dying them and then stabilizing them with plastic resins to make ...
  45. [45]
    The Best Turquoise Is More Valuable Than Diamonds | HowStuffWorks
    only about 100 pounds was mined before the deposit completely ran out in the 1970s.