Divide near Silver Bow in Silver Bow County, Montana — The American West (Mountains)

Plutons and the Humbug Spires

Photographed by Barry Swackhamer, July 11, 2021

1. Plutons and the Humbug Spires Marker

Caption: (top center) Humbug Spires, (bottom center) Map of plutons under discussion.

Inscription.

Plutons and the Humbug Spires. . This rest area lies near the southwest corner of the Boulder Batholith - a very large collection of igneous plutons. "Igneous" refers to rocks solidified from magma. "Plutons" harden from great blobs of magma that harden deep in the earth. , Plutons surround this rest area. The Big Hole Canyon Pluton makes up the south side of Fleecer Mountain to the west (the one that looks like Mount Fuji, though it isn't a volcano). The Climax Gulch Pluton rises on both sides of the highway here and to the north. The Butte Pluton, farther north, hosts the copper, gold, silver and molybdenum deposits of the Butte Mining District. The Butte Pluton has been mined almost continuously since 1864. , The Moose Creek Pluton, south and east of us, is now a labyrinth of pinnacles and fins called the Humbug Spires. The spires are what remain after millennia of weathering and erosion along fractures and joints. The result is a haven for hikers, rock climbers, and mountain lions. , (Side-bar on the right) , Geo-Facts: , . Plutons are one to twenty miles across. Batholiths are a hundred or more miles across. , . The Plutons around us formed more than three miles deep in the earth, between 70 and 80 million years ago. The dinosaurs living here would have seen nothing to show what was happening beneath their feet. , . The relentless forces of weathering, erosion, and plate tectonics brought the plutons to the surface over millions of years. The rocks above the plutons were slowly disintegrated and carried away. Their remains are now spread all the way to the Atlantic and Pacific oceans. , Geo-Activity: , . Pick up a rock and look at it very closely. Igneous rocks are made of interlocking crystals. The particles in the rocks are commonly angular. Sedimentary rocks are commonly made of roundish particles that are cemented together. Rub the rock with you fingers. Does it break apart? Try to imagine how long it would take for wind, and water to turn the rock into sand and carry it to the sea.

This rest area lies near the southwest corner of the Boulder Batholith - a very large collection of igneous plutons. "Igneous" refers to rocks solidified from magma. "Plutons" harden from great blobs of magma that harden deep in the earth.
Plutons surround this rest area. The Big Hole Canyon Pluton makes up the south side of Fleecer Mountain to the west (the one that looks like Mount Fuji, though it isn't a volcano). The Climax Gulch Pluton rises on both sides of the highway here and to the north. The Butte Pluton, farther north, hosts the copper, gold, silver and molybdenum deposits of the Butte Mining District. The Butte Pluton has been mined almost continuously since 1864.
The Moose Creek Pluton, south and east of us, is now a labyrinth of pinnacles and fins called the Humbug Spires. The spires are what remain after millennia of weathering and erosion along fractures and joints. The result is a haven for hikers, rock climbers, and mountain lions.

(Side-bar on the right)
Geo-Facts:
• Plutons are one to twenty miles across. Batholiths are a hundred or more miles across.
• The Plutons around us formed

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more than three miles deep in the earth, between 70 and 80 million years ago. The dinosaurs living here would have seen nothing to show what was happening beneath their feet.
• The relentless forces of weathering, erosion, and plate tectonics brought the plutons to the surface over millions of years. The rocks above the plutons were slowly disintegrated and carried away. Their remains are now spread all the way to the Atlantic and Pacific oceans.

Geo-Activity:
• Pick up a rock and look at it very closely. Igneous rocks are made of interlocking crystals. The particles in the rocks are commonly angular. Sedimentary rocks are commonly made of roundish particles that are cemented together. Rub the rock with you fingers. Does it break apart? Try to imagine how long it would take for wind, and water to turn the rock into sand and carry it to the sea.

Erected by Montana Department of Transportation.

Topics. This historical marker is listed in this topic list: Natural Features. A significant historical year for this entry is 1864.

Location. 45° 50.087′ N, 112° 41.038′ W. Marker is near Silver Bow, Montana, in Silver Bow County.

Photographed by Barry Swackhamer, July 11, 2021

2. Plutons and the Humbug Spires Marker

It is in Divide. It is on Interstate 15 at milepost 111 near Divide Creek Road. The marker is in the North Bound Feely Rest Stop. Touch for map. Touch for directions.

Regionally, this marker is in andspecifically outhwest Montana, in Gold West Country, in Mining Country. It is also in the American Mountain West

and in the Lewis & Clark Corridor.

Globally, it is in North America,

the Rocky Mountains,

the Western Hemisphere,

the Western World,

and the Anglosphere.

Historically, it finds itself in what was once Rupert’s Land

and also the Louisiana Purchase.

Other nearby markers. At least 8 other markers are within 14 miles of this marker, measured as the crow flies: Keep Watching The Skies! (a few steps from this marker); Pay Gold (approx. 12 miles away); Spanish-American War Veterans Memorial (approx. 12½ miles away); Milwaukee Depot (approx. 13.4 miles away); History of the ’M’ (approx. 13.7 miles away); Galbraith Residence (approx. 13.7 miles away); Socialist Hall (approx. 13.7 miles away); Paul Clark Home (approx. 13.8 miles away).

Credits. This page was last revised on February 16, 2023. It was originally submitted on September 1, 2021, by Barry Swackhamer of Brentwood, California. This page has been viewed 1,080 times since then and 150 times this year. Photos: 1, 2. submitted on September 1, 2021, by Barry Swackhamer of Brentwood, California.