On May 3, 2003, the craggy rock face known as New Hampshire's Old Man of the Mountain tumbled to the ground in spectacular fashion. For a landmark that had been in the state's DNA for generations, its collapse was like a death in the family to some. The day after it fell, people left flowers at the base of Cannon Mountain in Franconia Notch State Park as a sort of funeral tribute, and plans were immediately launched to create a longer-lasting memorial. So what was so great about the Old Man of the Mountain, pre- and post-crumble? Read on for the stone-cold facts.

1. THANKS TO NATHANIEL HAWTHORNE, THE OLD MAN WAS ALSO KNOWN AS “THE GREAT STONE FACE.”

Although not explicitly named, it’s widely believed Hawthorne based his 1850 short story "The Great Stone Face"—which was set in an anonymous state that happens to look like New Hampshire—on the Old Man. At that time, the mountainous figure was already a tourist draw to the Granite State. Hawthorne described it as an “enormous giant, or a Titan,” with a “broad arch of the forehead,” a long-bridged nose, and having “vast lips.” Eventually Hawthorne’s nickname stuck, along with other loving titles like “Old Man” and “the Profile.”

2. THE "FACE" WAS ACTUALLY A SERIES OF LEDGES.

These granite cliff ledges, 40 feet tall and 25 feet wide, when viewed from the north at certain angles looked like a jagged face. Hawthorne corroborated this, writing in “The Great Stone Face”: “If the spectator approached too near, he lost the outline of the gigantic visage, and could discern only a heap of ponderous and gigantic rocks ... Retracing his steps, however, the wondrous features would again be seen; and the farther he withdrew from them, the more like a human face, with all its original divinity intact, did they appear."

3. HE COULD HAVE BEEN 12,000 YEARS OLD.

Public Domain, Wikimedia Commons

The Old Man was first discovered and recorded in 1805 by road surveyors Francis Whitcomb and Luke Brooks, which put the landmark at nearly 200 years old by the time it fell. But it likely first formed when water inside cracks in the granite bedrock froze and thawed following the retreat of glaciers about 12,000 years ago. (This freezing and thawing process was what hastened its eventual collapse.) According to geologist Brian Fowler in a research report by the Old Man of the Mountain Legacy Fund, the lower ledge—or chin—of the Old Man is assumed to have fallen first. Once that support was gone, the rest of the rock fell in formation.

4. CANNON MOUNTAIN WAS SO NAMED BECAUSE IT LOOKS LIKE ANTIQUE ARTILLERY.

The Old Man jutted from a cliff in Cannon Mountain in New Hampshire’s White Mountains, within Franconia Notch State Park. Originally named Profile Mountain, it took on a new name since its granite dome resembles a cannon from select vantage points. There are even three sub-peaks, nicknamed “The Cannon Balls.”

5. SOME OF THE STRONGEST SURFACE WINDS EVER IN THE U.S. WERE RECORDED ON TOP OF CANNON MOUNTAIN.

The gusts measured 199.5 mph on April 2, 1973. While impressive, they were likely even higher since 199.5 mph was the limit of what the researchers' instruments could record at the time. The highest surface wind gust in the U.S. still belongs in-state, though, with New Hampshire's Mount Washington recording 231 mph winds in 1934.

6. A SERIES OF TURNBUCKLES AND IRON TIES WERE PLACED WITHIN ITS FACE TO KEEP IT TOGETHER.

By 1916, as it became clear the Old Man might not live forever, the first efforts to protect the rock formation were made. By the 1920s, a crack in the Old Man’s "forehead" was clearly noticeable, and residents who were worried about its safety used chains, turnbuckles, and iron ties to keep the crack from separating. Many of those metal rods used to hold the Old Man together were still attached to the mountain years later.

7. THE STATE EVENTUALLY SPENT A SMALL FORTUNE TRYING TO SAVE IT.

Julius Hall, Public Domain, Wikimedia Commons

In 1957, the New Hampshire state legislature passed a $25,000 appropriation for the necessary repairs to slow the Old Man's deterioration. These steps included quick-drying cement and steel rods meant to fill in and fortify cracks. The rocky Band-Aids were maintained every summer.

8. THE CARETAKERS’ MAINTENANCE ROUTINES WERE METICULOUS.

One longtime caretaker, Niels Nielsen, took great pains to keep the Old Man clean since 1965. Nielsen would spray bleach on the rock face and in its cracks, then carefully remove moss and lichen in an effort to prevent cracks from spreading further. He would even clean out the Old Man’s ear with a garden hoe. When Nielsen retired, he passed the job on to his son, David. The face continued to be groomed until its collapse.

9. NIELS NIELSEN SAW THE OLD MAN AS A GIFT FROM GOD.

According to Yankee Magazine, Nielsen was rather enchanted by the rock formation. “I had sailed around the world as a merchant seaman, yet I had never seen anything like the Old Man," he said. "I don’t believe anyone can be up there and not feel the presence of God."

10. BUT EVEN NIELSEN KNEW IT MIGHT FALL SOME DAY.

Nielsen was asked by Yankee what would happen if the Old Man ever fell. “The Lord put him here, and the Lord will take him down," Nielsen replied. Research concluded its collapse was natural—that the freezing-thawing process and subsequent erosion over time caused its downfall.

11. YOU CAN STILL "SEE" THE OLD MAN.

Rob Gallagher, Public Domain, Wikimedia Commons

The image of the Old Man has lived on as a state emblem since 1945, appearing on highway signs, on the back of drivers licenses, and on the reverse of the state quarter. But residents weren’t done with honoring the now-deceased rock face. At Old Man of the Mountain Profile Plaza and Historic Site in Franconia, special viewfinders and steel “profilers” at vantage points near Profile Lake offer a glimpse of what the formation used to look like.

12. THERE’S EVEN AN OLD MAN OF THE MOUNTAIN FLOWER.

Old-Man-of-the-Mountain, or tetraneuris grandiflora, is found in the Intermountain Regions and Rocky Mountains in states like Wyoming, Montana, Utah, Colorado, and Idaho. It’s sometimes called an alpine sunflower and got its common name from the wooly hairs that cover its leaves.