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Why rockhounds from across the country keep making the drive to Franklin, New Jersey

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Zinc ore under ultraviolet black light from the Precambrian of New Jersey, USA. (public display, Orton Geology Museum, Ohio State University, Columbus, Ohio, USA) Green fluorescence = willemite Black = zincite and franklinite Significant zinc ore bodies in the Franklin Marble of Mesoproterozoic age have been mined in northern New Jersey, USA for many decades. Zinc ores from the Sterling Hill and Franklin areas of New Jersey are dominated by red zincite (ZnO - zinc oxide) and black franklinite ((Zn,Fe)Fe2O4 - zinc iron oxide). The New Jersey zincite-franklinite bodies are traditionally considered as skarn deposits - the result of contact metamorphism of Cambro-Ordovician limestones by igneous intrusions. Elsewhere, igneous intrusion of limestones does result in the formation of odd mineral suites by contact metamorphism. However, these zinc ores do not appear to be skarn deposits. Their exact origin is still debated in the literature, but published research suggests that the zinc ore bodies were originally Zn-rich metalliferous sediments deposited in the margin of a marine basin. The marine basin was subsequently metamorphosed by subduction during the Grenville Orogeny (1.03-1.08 billion years ago) and became enclosed in marble host rocks by inverse diapirism. In addition to their economic geologic significance, the rocks and minerals from the Franklin and Sterling Hill zinc orebodies of New Jersey are famous for their gorgeous fluorescent colors under ultraviolet (UV) light. In addition to franklinite and zincite, which don't fluoresce, many rocks from the New Jersey zinc mines are rich in calcite (CaCO3 - calcium carbonate), plus some willemite (Zn2SiO4 - zinc silicate), both of which fluoresce. Under normal light, the calcite is whitish-grayish in color. Under UV light, manganiferous calcite will fluoresce an intense orangish-red color. Willemite varies considerably in normal light, but is usually light brown to peachy-colored in New Jersey zinc ores. Under UV light, willemite will always have an intense greenish fluorescence. Why do some minerals fluoresce under UV light? When short-wavelength UV radiation, long-wavelength UV radiation, or x-rays bombard atoms, electron excitation occurs. But the electrons do not remain in an energetically excited state. They quickly give off energy and resume their normal energy levels. If the electron energy release is in the visible spectrum of light, a mineral glows, or fluoresces. Locality: unrecorded/undisclosed site at or near Franklin, Sussex County, northern New Jersey, USA

Franklin’s rocks glow in the dark

About an hour from New York City, tucked into Sussex County at the edge of the Appalachians, Franklin sits on one of the most mineral-rich patches of ground on the planet. The rocks here don’t just look unusual.

Under ultraviolet light, they explode into colors. This isn’t a special exhibit or a trick of the light.

It’s the geology. And you can take a piece of it home.

New Jersey Zinc Company's mines at Franklin, New Jersey (Sussex County).

From iron furnace to zinc mining boomtown

Franklin started as a village called Franklin Furnace in the 1600s, where early settlers smelted iron along the Wallkill River. Zinc changed everything.

By the early 1800s, commercial mining had begun, and by 1897, a string of small companies merged into the New Jersey Zinc Company. Workers came from Russia, England, Hungary and Poland to fill the mines.

The town officially became the Borough of Franklin in the early 1900s, built almost entirely around what was underground.

Willemite , Franklinite , Rhodonite Locality: Sterling Mine, Sterling Hill , Ogdensburg , Franklin Mining District, Sussex County, New Jersey , USA ( Locality at mindat.org ) Size: 16.4 x 10.0 x 8.4 cm. At 1600 grams, this is a fairly good-sized, impressively hefty specimen. This piece features fat willemite crystals to 7 cm tall, with a few franklinites perched upon them. They are ensconced in calcite (fluorescent red) and rhodonite matrix. The specimen was long on display in the Paterson Museum, which only let it trade out as part of an exchange for some extremely rare and valuable New Jersey specimens from the 1800s...or this never would have left the museum. A superb specimen. Ex. George Elling Collection.

More than 350 minerals and 19 found nowhere else on Earth

Scientists have confirmed more than 350 different mineral species in the Franklin area. About 19 of them exist nowhere else on the planet.

The ore body also holds franklinite, willemite and zincite, the three minerals that drove a century of zinc mining.

Researchers rank this area among the most complex mineral sites in the world, not just in the United States.

That density of rare minerals in a single location is what makes the geology here so different from anywhere else.

Franklinite rock is a type of oxide minerals. They glow under the UV light. Franklinite rocks under UV lights. We see rocks everywhere we walk in the park or at our neighbors or our own yard, but we hardly notice that some of them glow under UV lights. New Jersey

Franklinite was named after Benjamin Franklin himself

In 1819, French geologist Pierre Berthier first described a black, shiny mineral with sharp crystal formations pulled from these mines. He named it franklinite in honor of Benjamin Franklin.

For more than a century, it served as New Jersey’s main source of zinc. The state didn’t let that history fade.

In 2023, New Jersey made franklinite its official state mineral, more than 200 years after Berthier first put a name to it.

This shows how willemite in natural light and how it fluoresces in ultraviolet light. The rock is from Franklin, New Jersey, US. It is on display at the Gem and Mineral Museum in Franklin, North Carolina, U.S.

How Franklin got its official glowing rocks title

On Sept. 13, 1968, New Jersey passed a resolution declaring Franklin the Fluorescent Mineral Capital of the World. The title recognized something no other place could match.

More than 90 different minerals in the area fluoresce under ultraviolet light, and no other town in the country carries that distinction. The resolution made official what rockhounds and geologists had known for decades.

The rocks under Franklin do something the rocks under everywhere else simply don’t.

Franklinite-willemite-calcite rock fluorescing (Franklin Marble, Mesoproterozoic, 1.03-1.08 Ga; zinc mine in northern New Jersey, USA) 4

Step into the darkroom and watch the walls come alive

The Franklin Mineral Museum opened in 1964, founded by the Franklin Kiwanis Club.

Inside, a darkroom lets you stand in front of rock specimens and watch them shift from dull gray to vivid pinks, greens and oranges the moment the ultraviolet lamps come on.

The museum also holds exhibits on fossils, petrified wood and Native American artifacts, plus a mine replica that shows what the underground work actually looked like.

It’s one of the best public displays of fluorescent minerals anywhere.

Franklinite-willemite-calcite rock fluorescing (Franklin Marble, Mesoproterozoic, 1.03-1.08 Ga; zinc mine in northern New Jersey, USA) 2

A 32-foot wall of glowing rock lights up the main hall

Welsh Hall holds more than 5,000 specimens from around the world. The Local Minerals Room shows off species found only in Franklin.

Walk into the Fossil Room and you’ll find dinosaur eggs, shells and petrified wood. A 32-foot wall of fluorescent rocks runs along one side, and when the room goes dark, it lights up in layers of color.

A separate room holds stone tools made by the Lenni Lenape people who lived on this land long before the mining began.

Gloved hand holding a raw vein quartz pebble, freshly unearthed at a sunny quarry. Sparkling natural mineral specimen with earthy textures, a geological find

Dig the Buckwheat Dump and keep what you find

Behind the museum sits a three-acre pile of mine waste rock called the Buckwheat Dump, named after a farm field that once stood there. The pile is open to visitors whenever the museum is.

Bring gloves and dig. Collectors have pulled specimens worth hundreds of dollars from the same ground everyone else walks past. Whatever you find goes home with you.

The site has been open to rockhounds for decades, and there’s still plenty left to discover.

Mineral illuminated with UV light, green willemite, red calcite

Willemite, calcite and four colors in a single rock

Not all the colors are the same. Willemite glows bright apple green under ultraviolet light.

Calcite from Franklin glows deep red. Hardystonite shines purple-blue, and clinohedrite gives off a soft orange.

Some single rocks contain four or more colors layered into one piece. The effect isn’t from paint or treatment.

It comes straight from the mineral chemistry locked inside the rock. That’s why the darkroom displays hit so differently here than at any other museum.

The visitor center for the Sterling Hill Mining Museum in Ogdensburg, New Jersey . Formerly the mine superintendent's office.

Go underground at Sterling Hill Mine

Three miles away in Ogdensburg, the Sterling Hill Mine takes you into the real thing. Guides hand out hard hats before you walk into tunnels the miners actually worked.

The mine reached 2,675 feet below the surface at its deepest point. Many of the guides are former miners, and they don’t read from scripts.

They talk about working these tunnels from memory.

Life-size mining displays line the route, but the guides’ stories are what stay with you after you come back up.

Fluorescent rocks of sterling hill mine glowing veins of light

The Rainbow Tunnel turns the mine walls into a light show

Deep inside Sterling Hill, there’s a section called the Rainbow Tunnel where the walls run thick with glowing ore. The guide cuts the lights and switches on ultraviolet lamps.

Reds, greens and yellows break across the rock in every direction. There’s no paint, no projection, no setup.

The color comes from the minerals in the walls, the same minerals that drew miners and scientists here for over a hundred years. First-time visitors tend to go quiet the moment it happens.

Access to the main shaft from the adit at the Sterling Hill Mining Museum in Ogdensburg, New Jersey .

The old mine replica inside a historic engine house

Back at the museum, the mine replica sits inside the former Taylor mine engine house, listed on the New Jersey State Historic Site Register. The New Jersey Zinc Company originally built it as a training space.

Now it lets you see what underground mining looked like without going below ground. Old candle hats, air pressure drills and other tools line the displays.

The inside stays cool, the way a working mine does, and the layout gives you a clear picture of what the men who dug this town out of the earth actually dealt with every day.

Demonstrace luminiscence (fosforescence a fluorescence) některých minerálů při nasvícení UV zářením. Den otevřených dveří v depozitářích Přírodovědeckého muzeu v Praze v Horních Počernicích.

Visit the Franklin Mineral Museum in Franklin, New Jersey

You can dig the Buckwheat Dump and walk the museum exhibits all in one visit.

The Franklin Mineral Museum at 32 Evans St. opens seasonally from early April through late November. Admission covers both the museum and dump access.

A gift shop sells ultraviolet lights if you want to check your finds on the spot.

Call ahead or check the official website for current hours and pricing before you go, since seasonal schedules can shift.

This article was created with AI assistance and human editing.

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Currently residing in the "Sunset State" with his wife and 8 pound Pomeranian. Leo is a lover of all things travel related outside and inside the United States. Leo has been to every continent and continues to push to reach his goals of visiting every country someday. Learn more about Leo on Muck Rack.

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