Quick answer. Around a hundred and fifteen records coded GLM-0001 upwards, in two distinct families. The larger is specimen sets - rocks and minerals in sets of forty and fifty, metallic ores, alloys, metals, with identification charts. The smaller is astronomy and earth models - an elementary planetarium, a solar system simulator and an illuminated globe. For the specimen sets, one thing decides whether the money was well spent, and it is not the number of specimens: a set is only as good as its key. Fifty labelled rocks with an identification sheet and a numbered tray is a teaching resource. Fifty unlabelled rocks in a box is a box of stones, and that is what a set becomes within two years if the key is lost. Everything below follows from that.
Specimen sets fail in a specific and predictable way. The specimens are handed round, put back in the wrong compartments, a few are dropped or taken home, the printed sheet is mislaid, and what remains is a tray of unidentified pieces that nobody is confident enough to teach from. Four things prevent it, and all four should be on the order:
A rock and mineral set is bought to teach identification, and it is worth being clear about what identification from a hand specimen actually involves - because that determines what else you need to buy.
What can be determined by hand and eye: colour and lustre, whether the mineral is translucent or opaque, crystal form where it is visible, cleavage and fracture, relative hardness, streak, apparent density by feel, grain size and texture in a rock, and whether it is layered, crystalline or fragmental. That is enough to identify a large number of common minerals and to classify rocks as igneous, sedimentary or metamorphic - which is the school and college syllabus.
What cannot: precise composition, and the distinction between minerals that look alike but differ chemically. Those need instruments, and a teaching laboratory should not pretend otherwise.
So the specimen set needs a small kit beside it, and it is routinely forgotten:
Tell us if you want that kit quoted with the set; we would rather send it than have the set used as a display.
The metallic ores, alloys and metals sets are often bought as if they were more rock sets, and they are doing something different and more interesting. Used together they teach extraction and use as a sequence:
Laid out as a row - ore, metal, alloy - for two or three familiar metals, that is one of the best single demonstrations in a chemistry or materials syllabus, and it needs no apparatus at all. Buy the three sets together if you buy them, because the sequence is the lesson and no one set shows it.
For the metallography that follows this subject at a higher level - how the structure of a metal is revealed and examined - see metallurgical equipment.
The physiographic relief globes, relief maps and landform models sit in our meteorology and earth science listing, along with the fossil collections and the legal questions those raise.
Related ranges: meteorology and earth science for landforms, relief globes and fossils, educational charts, science teaching equipment for the general school science range, metallurgical equipment, and microscopes and slides where thin sections are examined. The full educational kit and educational lab equipment categories list the rest.
Not necessarily, and the count is the least important thing about it. A set of forty with numbered compartments, a laminated key, a spare key in the cupboard and replaceable specimens will still be teaching in twenty years. A set of fifty loose in a box with one paper sheet will be a tray of unidentified stones within two. Compare the trays and the documentation before comparing the counts.
A hand lens above all, because grain size and crystal form are often invisible to the unaided eye; then a streak plate, a set of hardness references, dilute acid in a dropper bottle for carbonates, and a magnet. Without them a set can be looked at but not worked with. Ask us to quote the kit alongside the set - it costs little and it is what turns a display into a practical.
They can get a long way: colour, lustre, transparency, crystal form, cleavage and fracture, relative hardness, streak, density by feel, and the texture that classifies a rock as igneous, sedimentary or metamorphic. What they cannot do is determine composition, or separate minerals that look alike but differ chemically - that needs instruments. A course that is clear about the boundary teaches better science than one that implies the eye is enough.
Because the sequence is the lesson. An ore is usually unrecognisable as the metal it contains; the extracted metal is where chemistry becomes visible; the alloy is what is actually used, and raises the question of why almost nothing is made of a pure metal. Laid out as a row for two or three familiar metals it is one of the best demonstrations available with no apparatus at all - and no single set shows it.
No desk model can be to scale in both planet size and orbital distance - at true relative scale the planets would be invisible specks. Ask what a particular model is to scale in, tell the class, and the model becomes useful rather than misleading. What these models do teach well is relative motion: day and night, seasons, lunar phases and why eclipses are rare, which is the part students find hardest.
An illuminated globe, because it is the only honest way to show that every flat world map distorts something - area, shape, distance or direction - and the globe-against-wall-map comparison is worth a whole lesson. After that, a rock and mineral set with its identification kit, which supports both geography and chemistry teaching.
Ray Export is a manufacturer and exporter of laboratory, scientific and educational equipment based at Plot No. 449, HSIIDC Industrial Area, Saha, Ambala, Haryana 133104, India. Enquiries: [email protected], +91-9817319615.
Written by Palak Mall, Senior Content Writer. Technically reviewed by Arvind Kumar, Lab Equipment Specialist, 12+ years in laboratory and testing instrumentation. Last updated: 17 October 2026.
Notes on this listing, published rather than hidden: the product names carry the padding phrase "For Earth Science Lab", which has truncated several of them where it overflowed the field, and the names also repeat the words "Set Of" and "Set" twice in several records ("Set Of Rocks And Minerals Set OF 50"); both are being corrected. The code sequence skips GLM-0002, which suggests a record was removed or reassigned and needs a database check rather than a guess - and a GLM- code also appears inside our high school physics listing, which is a separate fault we have flagged. Specimen counts, specimen sizes, what each set contains, what accompanies it and the scale of the astronomy models will all be confirmed in writing on the quotation. Verify them before tender submission, and treat dilute acid supplied for carbonate testing as a laboratory chemical with your own institution's rules applying.
This Collection contains 20 Types of Basic Stones.The Stones include Some of the following Bauxite, Boron, Calcite, Chalcopyrite, Dolomite, Feldspar, Gabbro, Granite, Graphite, Gypsum, Hematite, Lime Stone, Magnetite, Marble, Pegmatite, Pumice, Quartz, Slate, Soap Stone & Sulphur etc.
The Mohs scale of mineral hardness characterizes the scratch resistance of various minerals through the ability of a harder material to scratch a softer material. This Collection contains 9 Minerals represents the scale of Hardness Talc (H=1), Gypsum (H=2), Calcite (H=3), Fluorite (H=4), Apatite (H=5), Orthoclase (H=6), Quartz (H=7), Topaz (H=8) & Corundum (H=9)
Fracture represents a mineral break other than along a cleavage or parting plane. Breaks may occur in any direction but are usually around some imperfection in the mineral. This collection contains 10 Minerals having Property of Even, Uneven, Conchoidal, Subconchoidal, Splintery & Hackly fracture.
Cleavage is the tendency of minerals to break along preferred directions. Some minerals tend to have one direction of cleavage. This collection contains 10 Minerals having Property of Basal, Cubic, Octahedral, Sinusoidal, Rhombohedral & Prismatic cleavage.
The streak is the color of the mineral in powdered form.Streak shows the true color of the mineral.In large solid form, trace minerals can change the color appearance of a mineral by reflecting the light in a certain way. This collection contains 10 Minerals having Property of Light Blue, White, Colour Less, Brown Grey, Black, Yellow Grey, Reddish, Brown, Greenish Black & Brown Gold Streak.
Luster is the property of minerals that indicates how much the surface of a mineral reflects light. The luster of a mineral is affected by the brilliance of the light used to observe the mineral surface. This collection contains 10 Minerals having Property of Metallic, Adamantine, Viteous, Resinous, Greasy, Pearly, Shining, Sub metallic, Dull & Metallic Luster.
Tenacity is the characteristic that describes how the particles of a mineral hold together or resist separation. The chart below gives the list of terms used to describe tenacity and a description of each term. This collection contains 10 Minerals having Property of Brittleness, Sectile, Malleability, Flexibility, Elastic, Softness, Tensile & Fragility Tenacity.
Specific Gravity of a mineral is a comparison or ratio of the weight of the mineral to the weight of an equal amount of water.
Colour is the first thing someone notices when they view a mineral. Color is also one of the big reasons that attract people to minerals.
The Feel of a mineral can sometimes help identify it.Some minerals are greasy to the touch, others are smooth, and others have a rough feel.This Collection contains 10 Minerals having Thin, Greasy, Fiberous, Heavy, Smooth, Greasy, Rough, Oily, Sandy & Grained Feel Property.