Are We Drying Up?

by Skip Via
skip@westvalleynaturalists.org

Editor’s note: In an earlier post on our website (Water Water Everywhere?) I discussed the nature of our valley water resources. Our groundwater comes from two sources–the shallow, unconfined aquifers that are replenished by precipitation, and the deeper confined aquifer from which Kalispell’s municipal water and most of the water used for irrigation in the valley is drawn. None of our water comes from reservoirs. (Whitefish gets its municipal water from Whitefish Lake.) A review of that article might provide good context for this article.

The intent of this article is intended to stimulate thought, not to advocate for a specific viewpoint. To that end, some assumptions, disclaimers and caveats:

  • I’m not a hydrologist, climatologist, or a geologist–just an interested observer;
  • Weather can change quickly in these parts;
  • Weather and climate are not the same thing;
  • I don’t know the answers to the questions I am posing.

It’s not difficult to see what a critical force water has been in the geographical and habitation history of our valley. If we didn’t have access to abundant water resources, both above and below ground, we would not be the agricultural center that we are now. And if it weren’t for glaciers, snowpack, and rushing rivers and streams, the landscape around here would look a lot different. There probably wouldn’t even be a place level enough with sufficient soil to farm at all.

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Hydrology Snapshot, July 2023

by Skip Via
skip@westvalleynaturalists.org

My intention with this post is to begin a regular documentation of the local effects that hydrological issues have on life here in the valley.

This post from last month–Water Water Everywhere?–discusses some of the hydrological factors involved in how we access water resources for drinking and agriculture here in the valley, including a discussion of the water table and the Deep Aquifer, from which most of our water is drawn. The distinction between the water table and the Deep Aquifer is important. Rainfall, which can alter the local water table either by its presence or absence, does not affect the amount of water in the Deep Aquifer. Please refer to that article for more information.

Here’s a quick Flathead Valley hydrology snapshot from July 4, 2023:

Rainfall YTD5” (avg 9.72”)
Flathead Lake Level12” below 23-year median,
9” below full pool
Valley Sreamflow60% below average
Snowpack86% of average
SnowmeltFastest in 30 years
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Indigenous Place Names

by Skip Via
skip@westvalleynaturalists.org

If an enterprise or place name here in the valley doesn’t begin with “Glacier,” there’s a good chance that it begins with “Flathead.” We live in Flathead County, in the Flathead Valley drained by the Flathead River. There’s Flathead Valley Community College, Flathead High School, Flathead National Forest, Flathead Lake, the Flathead Beacon…

But where exactly does that name come from, and what does it mean? There’s a clue in the Flathead County Seal, but there is much more to the story.

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Aurora Borealis in the Flathead

by Denise Silva (text and images)
Denise.Silva@aicpa-cima.com

The Aurora Borealis is often referred to as the Northern Lights because we see it to our north. But this is a bit of a misnomer, as the “lights” are also seen in the Southern Hemisphere, where they are referred to as the Aurora Australis. In fact, not only does Earth have auroral displays, but auroras can be seen on images of other celestial bodies, such as Jupiter, Saturn and Mars.

Aurora over Kalispell
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West Valley Geology Tour

by Skip Via
skip@westvalleynaturalists.org

Welcome to a virtual tour of some of the Flathead Valley’s prominent (and some not so prominent) geological features, courtesy of Google Earth.

This tour is a companion piece to several articles that have appeared elsewhere on our website:

This inspiration for this project came largely from the work of Dr. Lex Blood, professor emeritus, Flathead Valley Community College, for his extensive (and clearly heartfelt) efforts to make the geological history of the valley accessible to everyone. Thank you, Lex.

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Water Water Everywhere?

by Skip Via
skip@westvalleynaturalists.org

To take a virtual tour of the West Valley area, click here.

It’s easy to take water for granted here in the valley. We’re surrounded by water, with numerous streams and rivers, lakes and ponds of various sizes, and seasonal runoff from snow and rain that typically replenish the surface water that we see.

The water we drink and irrigate with here in the West Valley comes from underground aquifers–layers of permeable rocks or sediments that are saturated with water. Our shallower surface aquifers are fed by groundwater that enters the aquifers mostly through seasonal precipitation or snowmelt.

The Flathead Valley also sits directly atop a large, deep aquifer referred to in studies, appropriately enough, as The Deep Aquifer. It’s from this aquifer that our municipal water is drawn. Farms and homes also tap into the Deep Aquifer via wells for irrigation or daily use. (The city of Whitefish does not draw water from the Deep Aquifer. They draw their municipal water from Whitefish Lake and surrounding streams. See Editor’s Note, below, for clarification.)

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NMFA Firefighting Images

by Skip Via and Barbara Boorman
skip@westvalleynaturalists.org

Editor’s note: Images provided by Barbara Boorman as an accompaniment to her article about fighting wildfires. Captions are transcribed from the reverse side of the photo. To read Barbara and Pat’s history of firefighting in the Flathead Valley, click here.

Lillian Neas Boorman and Bertha Boorman on tower of Blacktail Lookout, Sec. 18 T 26N. R 21 W. 7/30/1935
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Schools of West Valley

By Jeanine Buettner
nammy@montanasky.com

West Valley School was opened in 1961. But what was schooling in the valley like before that?

Stillwater School

Stillwater School first opened on January 21, 1899. The first building was a small log cabin on the Henry Bird place on the corner of Clark Drive and Stillwater Road. All eight grades were taught here with just one teacher.

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The Ashley Creek Ditch

by Jeanine and Kevin Buettner
nammy@montanasky.com
and Skip Via
skip@westvalleynaturalists.org

Editor’s Note (November 2024): For some images of a few remaining vestiges of the Ashley Creek Ditch, head over to Ashley Creek Ditch Revisited on this web site.

The Ashley Creek Ditch was an irrigation system developed in the early 1900s to supply water from Ashley Creek to farms in the west valley area of the Flathead. The Ditch was not a county or state project; rather, it was paid for and maintained by the families that used the water. It’s no longer there, having been dismantled in the late 1970s due to changing agricultural practices and the increasing availability of tapping directly into the aquifers for irrigation. But its story is a prime example of the ingenuity and work ethic that early settlers in the area shared.

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Glaciers, Faults, and Tectonics

by Skip Via
skip@westvalleyaturalists.org

To take a virtual tour of the West Valley area, click here

Here in the Flathead Valley, we’re fortunate to be able to enjoy a richly varied landscape—craggy mountains, rolling hills, swift rivers and meandering streams lined with brightly colored stones, a sprawling valley floor punctuated with the occasional boulder or with massive rock outcroppings displaying multiple bands of colors and textures, clearwater lakes fed by springs or seasonal precipitation, wetlands that provide shelter and food for our avian residents. It’s a rare day that I’m not struck by the immense beauty of our valley.

But do you ever wonder how it got this way?

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West Valley Bee and Bee

by Skip Via
skip@westvalleynaturalists.org

There are two common recommendations for maintaining and increasing the population of native bee species: plant native plants and provide a bee house of some kind so that the insects can overwinter or deposit their eggs and have a safe place for their larvae until the spring when they emerge. This article describes an attempt to do these as complementary processes.

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West Valley Pioneer: Edmond Levi Kelley

by Jeanine Buettner
nammy@montanasky.com

Edmond Kelley was born in Wyoming County, Pennsylvania, on April 18, 1860 and was educated and lived in Pennsylvania until coming to Montana in 1885, first locating in Butte and then moving to the Flathead Valley in 1887. He spent his first night in Somers. He was told that the valley farther up had some value as a range for cattle but of no value for farming. The next day he walked to the site that would later become Demersville.

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