Tag: Calcium Carbonate

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Naturally Carbonated Water

Naturally Carbonated Water: Soda Springs Geyser, Soda Springs, Idaho, Courtesy & &copy Mary Heers, Photographer
Soda Springs Geyser, Soda Springs, Idaho

If you like drinking carbonated water as much as I do, you’ll be happy to hear you can drink as much as you’d like, -absolutely for free- just north of the Utah border in Soda Springs, Idaho.

Idan-Ha Mineral Water, Courtesy & &copy Mary Heers, Photographer
Idan-Ha Mineral Water
Courtesy & &copy Mary Heers, Photographer

Small Bubbling Soda Water Pool, Courtesy & &copy Mary Heers, Photographer Small Bubbling Soda Water Pool
Courtesy & &copy Mary Heers, Photographer

When settlers heading to California passed through this area on the Oregon Trail, they saw the many bubbling natural springs.

In 1838 Sarah White Smith, wrote in her diary, This is indeed a curiosity. The water is bubbling and foaming like boiling water.” But the water wasn’t hot.

She also wrote how delighted she was when she made bread with the water. “The bread was as light as any prepared with yeast.”

All this stirred up some fond memories I have of my high school science teacher who always made interesting things happen in the classroom. She put a pinch of sodium bicarbonate (commonly called baking soda) in a dish and added a couple tablespoons of water and vinegar. Voila! The dish began “bubbling and foaming like boiling water.”

For centuries something like this has been going on under the ground in Soda Springs. The carbonate rocks are mixing with slightly acidic water, sending CO2 bubbles to the surface .

By 1887, Soda Springs had grown to a bustling town. Some enterprising residents came up with a plan to capture the CO2 gas. They built giant drums over one of the springs and then built a five-mile pipeline to their bottling plant. There they mixed the gas with clear water from another spring and bottled it. The soda water was called “Idan-ha” and was shipped out on the railroad far and wide.

It won first place at the Chicago World’s Fair in 1893 and again in the World’s Fair in Paris in 1905.

A decade later, another group of businessmen went to work on a plan to build a mineral water swimming pool resort.

On Dec 2, 1937, drillers dug down to 315 ft. No luck. They went to dinner. Then they heard a gush of water shoot up outside the window. They said it was “roaring like a dragon.” The whole area was enveloped in water vapor and Main Street was flooded. It took them two weeks to cap it.

The water wasn’t warm, so the businessmen abandoned their plans for a swimming pool resort.

The town knew their geyser was accidental; it was man-made- but still a plume of water shooting 100 ft into the air was impressive to look at.

Engineers put a timer on the cap. Now the carbonated water shoots up for 8 minutes every hour on the hour.

You can watch it for free.

As for drinking the naturally carbonated water, the city has set aside three springs.

My guide drove me to his favorite site just outside of town We scrambled down a grassy hillside to a small bubbling pool about the size of a basketball. He whipped out a cup and dipped it in. I drank. It was cold and fizzy.

“Good as Perrier,” I said.

He smiled, “Now I like you.”

I liked him too. Even more, I loved drinking this tasty treasure bubbling up from the ground.

This is Mary Heers and I’m Wild About Utah

Credits:

Photos:
Images Courtesy & Copyright Mary Heers, Photographer
Featured Audio: Courtesy & Copyright © Friend Weller, Utah Public Radio upr.org
Text: Mary Heers, https://cca.usu.edu/files/awards/art-and-mary-heers-citation.pdf
Additional Reading: Lyle Bingham, https://bridgerlandaudubon.org/

Additional Reading

Wild About Utah, Mary Heers’ Postings

Price, Mike, Soda Springs, We Are East Idaho, EastIdahoNews.com LLC, September 9, 2019, https://www.eastidahonews.com/2019/09/we-are-east-idaho-soda-springs/

Hooper Springs Park, California National Historic Trail, Oregon National Historic Trail, National Park Service, US Department of the Interior, https://www.nps.gov/places/000/hooper-springs-park.htm

A man-made CO2 Geyser in Utah:
Weaver, Lance, Crystal Geyser, Grand County, Utah, Geosights, Utah Geological Survey (UGS), Utah Department of Natural Resources, January 2018, https://geology.utah.gov/map-pub/survey-notes/geosights/crystal-geyser/

Map on page 43 shows water from Soda Springs flows into the Bear River and the Great Salt Lake:
Dissolved-Mineral Inflow to Great Salt Lake and Chemical Characteristics of the Salt Lake Brine, United States Geological Survey (USGS) and The College of Mines and Mineral Industries, The University of Utah, 1963, https://ugspub.nr.utah.gov/publications/open_file_reports/ofr-485/Lake%20Brine%20Interpretive%20Reports/WRB%2003%20-%20Part%201%20-%20Hahl%20&%20Mitchell%20-%201963/Water%20Resources%20Bulletin%203%20Pt%201%201963.pdf

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Oolites

Click to view larger image of the Utah's Oolitic Sand, Photo Courtesy and Copyright Mark Larese-Casanova
Utah’s Oolitic Sand, Photo Courtesy and Copyright Mark Larese-Casanova

Hi, this is Mark Larese-Casanova from the Utah Master Naturalist Program at Utah State University Extension.

Imagine if prehistoric brine shrimp were responsible for one of the finest examples of architecture in Salt Lake City today.

Okay, so it may be a bit of a stretch, but let me explain. In a previous episode of Wild About Utah, I discussed the life cycle of brine shrimp and the important role that they play in the Great Salt Lake Ecosystem. Well, as the billions of brine shrimp feed on bacteria in Great Salt Lake, they excrete waste in the form of tiny fecal pellets. These pellets, along with sand grains and other bits of debris, eventually settle to the bottom of Great Salt Lake.

In shallow areas of the lake, where wind and waves routinely mix the water, these small particles gradually accumulate layers of calcium carbonate, forming an oolite (spelled o-o-l-i-t-e). This is very similar to how a pearl, also layers of calcium carbonate around a small particle, is formed within the shell of an oyster or mussel. The main difference, aside from a pearl being much larger, is that oolites are typically oblong, rather than round. The beaches on the west side of Antelope Island are a great place to find oolitic sand, which will look and feel as though you have a handful of tiny pearls.

Click to view larger image of the Utah's Oolitic Sandstone, Photo Courtesy and Copyright Mark Larese-Casanova
Utah’s Oolitic Sandstone
Photo Courtesy & Copyright
Mark Larese-Casanova

Around 50 million years ago, large fresh- and salt-water lakes covered parts of Utah, and in these areas, vast amounts of sediments, including oolites, were deposited. Over time, these oolites were compressed and cemented together into limestone.

A quarry near Ephraim in Sanpete County supplied oolitic limestone for the construction of the Governor’s Mansion in 1902 and the original Salt Lake City Public Library in 1905. The Library building, located at 15 South State Street, eventually housed the Hansen Planetarium and is now home to the O.C. Tanner flagship store. The building underwent an extensive restoration just a couple of years ago, and now serves as a shining example of neoclassical architecture in our capitol city.

The truth is, there are tens of millions of years separating oolitic limestone from our modern-day brine shrimp. So, we can’t exactly say that prehistoric brine shrimp were responsible for the existence of the O.C. Tanner building. But, it’s fun to imagine precious gems from around the world housed in a beautiful building constructed from the ‘pearls’ of Great Salt Lake.

Click to view larger image of the historic OC Tanner building made from oolitic sandstone (This building formerly housed the Salt Lake Library and Hansen Planetarium), Photo Courtesy and Copyright Mark Larese-Casanova
Historic OC Tanner Building
(formerly the Salt Lake Library
and later the Hansen Planetarium)
Photo Courtesy & Copyright
Mark Larese-Casanova

For Wild About Utah, I’m Mark Larese-Casanova.
Credits:

Images: Courtesy and copyright Mark Larese-Casanova

Text:     Mark Larese-Casanova, Utah Master Naturalist Program at Utah State University Extension.
Additional Reading:

Utah Geological Survey https://geology.utah.gov/utahgeo/rockmineral/collecting/oolitic.htm

Utah Division of Wildlife Resources, Great Salt Lake Ecosystem Program
https://wildlife.utah.gov/gsl/facts/oolitic_sand.php

Salt Lake Brine Shrimp, https://saltlakebrineshrimp.com/harvest/

Posted on

Oolites

Click to view larger image of the Utah's Oolitic Sand, Photo Courtesy and Copyright Mark Larese-Casanova
Utah’s Oolitic Sand, Photo Courtesy and Copyright Mark Larese-Casanova

Hi, this is Mark Larese-Casanova from the Utah Master Naturalist Program at Utah State University Extension.

Imagine if prehistoric brine shrimp were responsible for one of the finest examples of architecture in Salt Lake City today.

Okay, so it may be a bit of a stretch, but let me explain. In a previous episode of Wild About Utah, I discussed the life cycle of brine shrimp and the important role that they play in the Great Salt Lake Ecosystem. Well, as the billions of brine shrimp feed on bacteria in Great Salt Lake, they excrete waste in the form of tiny fecal pellets. These pellets, along with sand grains and other bits of debris, eventually settle to the bottom of Great Salt Lake.

In shallow areas of the lake, where wind and waves routinely mix the water, these small particles gradually accumulate layers of calcium carbonate, forming an oolite (spelled o-o-l-i-t-e). This is very similar to how a pearl, also layers of calcium carbonate around a small particle, is formed within the shell of an oyster or mussel. The main difference, aside from a pearl being much larger, is that oolites are typically oblong, rather than round. The beaches on the west side of Antelope Island are a great place to find oolitic sand, which will look and feel as though you have a handful of tiny pearls.

Click to view larger image of the Utah's Oolitic Sandstone, Photo Courtesy and Copyright Mark Larese-Casanova
Utah’s Oolitic Sandstone
Photo Courtesy & Copyright
Mark Larese-Casanova

Around 50 million years ago, large fresh- and salt-water lakes covered parts of Utah, and in these areas, vast amounts of sediments, including oolites, were deposited. Over time, these oolites were compressed and cemented together into limestone.

A quarry near Ephraim in Sanpete County supplied oolitic limestone for the construction of the Governor’s Mansion in 1902 and the original Salt Lake City Public Library in 1905. The Library building, located at 15 South State Street, eventually housed the Hansen Planetarium and is now home to the O.C. Tanner flagship store. The building underwent an extensive restoration just a couple of years ago, and now serves as a shining example of neoclassical architecture in our capitol city.

The truth is, there are tens of millions of years separating oolitic limestone from our modern-day brine shrimp. So, we can’t exactly say that prehistoric brine shrimp were responsible for the existence of the O.C. Tanner building. But, it’s fun to imagine precious gems from around the world housed in a beautiful building constructed from the ‘pearls’ of Great Salt Lake.

Click to view larger image of the historic OC Tanner building made from oolitic sandstone (This building formerly housed the Salt Lake Library and Hansen Planetarium), Photo Courtesy and Copyright Mark Larese-Casanova
Historic OC Tanner Building
(formerly the Salt Lake Library
and later the Hansen Planetarium)
Photo Courtesy & Copyright
Mark Larese-Casanova

For Wild About Utah, I’m Mark Larese-Casanova.
Credits:

Images: Courtesy and copyright Mark Larese-Casanova

Text:     Mark Larese-Casanova, Utah Master Naturalist Program at Utah State University Extension.
Additional Reading:

Utah Geological Survey https://geology.utah.gov/utahgeo/rockmineral/collecting/oolitic.htm

Utah Division of Wildlife Resources, Great Salt Lake Ecosystem Program
https://wildlife.utah.gov/gsl/facts/oolitic_sand.php

Salt Lake Brine Shrimp, https://saltlakebrineshrimp.com/harvest/

Posted on

Oolites

Utah’s Oolitic Sand, Photo Courtesy and Copyright Mark Larese-Casanova

Hi, this is Mark Larese-Casanova from the Utah Master Naturalist Program at Utah State University Extension.

Imagine if prehistoric brine shrimp were responsible for one of the finest examples of architecture in Salt Lake City today.

Okay, so it may be a bit of a stretch, but let me explain. In a previous episode of Wild About Utah, I discussed the life cycle of brine shrimp and the important role that they play in the Great Salt Lake Ecosystem. Well, as the billions of brine shrimp feed on bacteria in Great Salt Lake, they excrete waste in the form of tiny fecal pellets. These pellets, along with sand grains and other bits of debris, eventually settle to the bottom of Great Salt Lake.

In shallow areas of the lake, where wind and waves routinely mix the water, these small particles gradually accumulate layers of calcium carbonate, forming an oolite (spelled o-o-l-i-t-e). This is very similar to how a pearl, also layers of calcium carbonate around a small particle, is formed within the shell of an oyster or mussel. The main difference, aside from a pearl being much larger, is that oolites are typically oblong, rather than round. The beaches on the west side of Antelope Island are a great place to find oolitic sand, which will look and feel as though you have a handful of tiny pearls.

Utah’s Oolitic Sandstone
Photo Courtesy & Copyright
Mark Larese-Casanova

Around 50 million years ago, large fresh- and salt-water lakes covered parts of Utah, and in these areas, vast amounts of sediments, including oolites, were deposited. Over time, these oolites were compressed and cemented together into limestone.

A quarry near Ephraim in Sanpete County supplied oolitic limestone for the construction of the Governor’s Mansion in 1902 and the original Salt Lake City Public Library in 1905. The Library building, located at 15 South State Street, eventually housed the Hansen Planetarium and is now home to the O.C. Tanner flagship store. The building underwent an extensive restoration just a couple of years ago, and now serves as a shining example of neoclassical architecture in our capitol city.

The truth is, there are tens of millions of years separating oolitic limestone from our modern-day brine shrimp. So, we can’t exactly say that prehistoric brine shrimp were responsible for the existence of the O.C. Tanner building. But, it’s fun to imagine precious gems from around the world housed in a beautiful building constructed from the ‘pearls’ of Great Salt Lake.

Historic OC Tanner Building
(formerly the Salt Lake Library
and later the Hansen Planetarium)
Photo Courtesy & Copyright
Mark Larese-Casanova

For Wild About Utah, I’m Mark Larese-Casanova.
Credits:

Images: Courtesy and copyright Mark Larese-Casanova

Text:     Mark Larese-Casanova, Utah Master Naturalist Program at Utah State University Extension.
Additional Reading:

Utah Geological Survey https://geology.utah.gov/utahgeo/rockmineral/collecting/oolitic.htm

Utah Division of Wildlife Resources, Great Salt Lake Ecosystem Program
https://wildlife.utah.gov/gsl/facts/oolitic_sand.php

Salt Lake Brine Shrimp, https://saltlakebrineshrimp.com/harvest/