Wild About Utah Archives - Page 71 of 145

March 30, 2020January 24, 2021

Hope

It feels odd to be denning in the spring. Our usual season to escape back into the out of doors has shifted radically for society at-large. It is odd because all the world around us is still warming, flying a little further each day, and here we are, humanity, digging in. It is for the best, for our own survival, but it is still not easy to go against the natural grain.

Hunkering down has affected us all, myself included. At first I was angry with frustration, as I’m sure you were too. I wanted something or someone to blame, to witness and call wrong. I struggled to find meaning in any of it; I struggled to hear anything but fear. It took me a while to come to remind myself that this frustration, this search for orientation, is the human way; it is natural to feel as we do in the omnipresence of the unknown.

What I discovered though is that this perspective, natural as it may be, is harmful if lived too long. My search was a dangerous one: for some externality of blame in an effort to begin to wrest back seeming control. When this is the path you choose to take, you find, as I did, that your anger is not quenched, but instead stoked. My focus was consumed by a blackness; it burned into my eye like a mariner’s missing star.

How then does one change course towards hope, and if not acceptance, then duty, empathy, and discipline for our fellow man? How do we get through such times?

The Greek philosopher Heraclitus said that “For God all things are good and right and just, but for man some things are right and others are not.” When I do not understand the world, the world I love so dearly, I think of these ancient words. I am reminded of this wisdom as I find myself unconsciously passing judgement upon the things I cannot control, and it stops me. In this wisdom I am reminded that, while there may be something to fear, there is no righteousness to my anger. True righteousness instead stems from the lessons of spring; the lessons of hope: of living on with tenacity, industry, and love, even in the face, however distant, of winter.

The righteousness of hope is found, too, in our choice to harness our actions with humble intention in light of what is happening in the world and the toll that is being taken. And just as fear is begotten in the meandering anger of blame, hope lives in our individual conscious actions. Only together can our actions create constellations for others to follow: cosmos among the chaos, shining brighter than the void’s pull. That we will all choose to do what is right, though it will not be easy, even in the face of doubt and fear, gives me hope.

So from the crocuses, the robins, and the fresh mud of our beautiful Utah spring, don’t forget that the world is still good and continues to be every day, even if sometimes it does not feel like it. Remind yourself of the lessons of spring by opening your window, listening to the birds, smelling deep the thawing air, and choosing to den in these times, fulfilling the spring lessons of tenacity, industry, and love. Choose to fix yourself as another orienting light of hope for those who still only see the night, or those who do not look up at all, for the world is good, it is everywhere, and we will always be of it. Here is to the persistence of life and hope found in us all this spring.

I’m Patrick Kelly, and I’m Wild About Utah.

Hope-Credits:

Images: Image Courtesy Pixabay
Audio: Contains audio Courtesy & Copyright Kevin Colver
Text: Patrick Kelly, Director of Education, Stokes Nature Center, https://logannature.org
Included Links: Lyle Bingham, Webmaster, WildAboutUtah.org

Hope-Additional Reading

Campbell, Joseph, Moyers, Bill, The Power of Myth, Bantum Books, Knopf Doubleday Publishing, Excerpt Courtesy Google Books, Heraclitus said: For God all things are good and right and just, but for man some things are right and others are not.

March 23, 2020March 25, 2020

Jack’s Nuthatches In Three Varieties

Inverted woodpecker, a phrase I use to describe the feeding habits of the amazing nut hatch family. I first became aware of this lovely little songbird growing up in Michigan, where the white-breasted nut hatch was common fare in the north woods. Their little laughing notes were most welcome as I sat on my deer stand where I would watch them search bark crevices for yummy morsels of grubs, insect eggs or seeds they had wedged in for tomorrow’s snack.

Jack's Nuthatches In Three Varieties: Red Breasted Nuthatch Courtesy US FWS Dave Menke, Photographer — Red Breasted Nuthatch
Courtesy US FWS
Dave Menke, Photographer

Now having lived many years in Utah, it is the red-breasted nut hatch that has replaced this eastern cousin for the most part. Their “yank, yank, yank” vocalizations light up my life whenever and wherever they occur. They prefer conifers but will gladly substitute a deciduous tree, especially those with more furrowed bark. Where there is food or water, infrequently a white-breasted will appear, especially in our higher elevations, although I’ve had them join the red-breasted at our feeder during winter months – a rare treat.

Jack's Nuthatches In Three Varieties: Pygmy nuthatch, Sitta pygmaea, Courtesy US FWS Lee Karney, Photographer — Pygmy nuthatch
Sitta pygmaea
Courtesy US FWS
Lee Karney, Photographer

If one spends much time in our Ponderosa pine forests in central and southern Utah, another family member can be found. Unlike the other two more solitary species, these tiny pygmies occur in small flocks and are very chatty. Highly social, the pygmy nut hatch appear to enjoy a food frolic as they fly from tree to tree for feeding and social interaction. Thus, Utah’s blessed with all three North American species of nut hatch.

If you observe them as they search the main stem of a tree, my inverted woodpecker title will be justified. Rather than moving from top to bottom of the tree facing up as do the woodpeckers, the nut hatch prefers head down from top to bottom. They also like hanging upside down on a horizontal limb. Why? Evolution keeps us mysteries well-guarded. I conjecture partitioning might be part of the answer: a phenomenon where bird species will utilize different parts of the tree to avoid competing for resources with other species.

As with all of life, I pay attention to how our shifting climate has been observed or predicted to affect their populations and distribution. As long as there are conifers breeding season, nut hatches are content. They can be found in dry Ponderosa pine foothills, in moist boreal bogs, around tree line in the mountains, and even in planted Christmas tree plantations. Audubon’s seven-year generated climate model shows an overall northward drift of the species’ range with more disruption and range loss in summer than in winter. The nut hatch is a habitat generalist in winter, so summertime climate is the chief concern going forward. However, whether the species adapts in the decades ahead will be determined in large part by the conifer forest health in a changing climate. The projection for species range change from 2000 to 2080 is 19% of summer 2000 range remaining stable and 58% of winter range projected to be stable. It’s my plan to follow them wherever they may go.

Wild about Utah is brought to you in part by our listeners and the Moab area travel council, whose support of tourism events and recreation in Grand county promotes and protects the natural beauty for visitors from across the state of Utah. Information available online at discovermoab.com

This is Jack Green, reading and getting wilder about Utah as days pass.

Credits:

Pictures: Courtesy US FWS, David Brenzinski, Photographer
Contains Sound: Courtesy Kevin Colver
Text: Jack Greene, Bridgerland Audubon Society //Utah State University Sustainability

Additional Reading:

White-breasted Nuthatch, All About Birds, Cornell Lab of Ornithology, https://www.allaboutbirds.org/guide/White-breasted_Nuthatch/id

Red-breasted Nuthatch, All About Birds, Cornell Lab of Ornithology, https://www.allaboutbirds.org/guide/Red-breasted_Nuthatch/id

Pygmy Nuthatch, All About Birds, Cornell Lab of Ornithology, https://www.allaboutbirds.org/guide/Pygmy_Nuthatch/id

Red-breasted Nuthatch, Sitta canadensis, eBird, Cornell Lab of Ornithology, https://ebird.org/species/rebnut

March 16, 2020May 18, 2020

Imaginary Wanderings

I’ve fancied a certain type of wandering lately—to grab my pack and boots and walk the lines of Utah’s political border—a trail made not of dirt and stone, but of imaginary lines of latitude and longitude. But, as of yet, I haven’t found the time or resources to do so beyond my own imagination and the 3 or 4 minutes I have with you now. Come join me in a stroll around Utah, at least the way I’ve imagined it.

Walking north out of Logan, I’ll wander through the grid-patterned neighborhoods that pepper the flanks of the Bear River Range, the still-snowy peaks that serve as sentinels over my daily commute and the adventure on which I embark now. They serve another, greater purpose, too, though. Without the Bear Rivers, the Rocky Mountains would be otherwise dissected. The snowy peaks I adore and which now pass in slow motion over my right shoulder form the only range of mountains that connect the northern and southern Rockies. Though they only measure about 70 miles in length, they provide a critical ecological thoroughfare from the south end of Cache Valley, Utah, north to Soda Springs, Idaho.

I won’t follow them that far, though. I’ll turn left (west) at the Idaho border toward the Great Basin.

I’m technically already there. We all are if we live along the Wasatch Front. And there are just a few minor ranges—the Clarkston Range, Blue Spring Hills, and the northern fingerling ridges of the Promontory Mountains—to wander across before reaching the Great Basin proper.

My favorite hidden gem of this often-overlooked portion of Utah are the Raft River Mountains. Like the mighty Uintas to the east, the Raft Rivers run East-to-West. So, despite being a stone’s throw from the Great Salt Lake, the tributaries running off their northern flanks drain not into the Great Basin and the Great Salt Lake, but north onto the Snake River Plain toward the Columbia River and, eventually, the Pacific Ocean.

The Tri Corners Landmark is a simple granite pillar sticking 3 or 4 feet out of the sand amongst wind-whipped sage brush. It’s easy to miss, but marks some interesting irregularities. Utah’s political border is not, in fact, made up of straight lines. According to cartographer Dave Cook, surveyors who created the state’s initial boundaries hastily covered ground with their crude survey instruments. They were paid by the mile, so they were more interested in finishing quickly than correcting any errors they made along the way.

The border wiggles at least four times by my calculations—one of which comprises two right angles—as it wanders across ridgelines and through the dusty draws of the basin and range mountains toward the Mojave Desert of southwest Utah.

Imaginary Wanderings: The wrinkled topography if the Colorado Plateau Courtesy & Copyright Josh Boling, Photographer — The wrinkled topography if the Colorado Plateau
Courtesy & Copyright Josh Boling, Photographer

I won’t be there for long, though. The border only runs for roughly 50 miles along the two legs of the right triangle that constitutes Utah’s allotment of the Mojave Desert before it climbs up onto the Colorado plateau. Ed Abbey famously compared the wrinkled topography of Utah, particularly his beloved canyon country of the Colorado Plateau, to the two largest of our states. “Alaska is our biggest, buggiest, boggiest state,” Abbey wrote. “Texas remains our largest unfrozen state. But mountainous Utah, if ironed out flat, would take up more space on a map than either.” Ropes, technical climbing and canyoneering gear, and a fair amount of fortitude would be required here.

The eastern border we share with Colorado is a varied expanse of high desert plateaus, rugged cliffs, out-of-place riparian zones, and a few spectacular snow-capped mountain ranges leading through some of the most beautiful and gloriously desolate places on the planet. The Book Cliffs, Dinosaur National Monument, and the La Sal Mountains come to mind.

A short walk distance-wise would require heaps of route finding across the Green River’s Flaming Gorge and along the northern toes of the Uinta Mountains. Here is perhaps the greatest of Utah’s geologic juxtapositions. Low basins adjacent the Intermountain West’s highest peaks.

Imaginary Wanderings: A view of the high Uintas from their northern foothills Courtesy & Copyright Josh Boling, Photographer — A view of the high Uintas from their northern foothills Courtesy & Copyright Josh Boling, Photographer

I’ll take my first right turn at the western edge of the Uinta foothills. Here I might skip the formalities of a longitudinal walk—stick my thumb out instead, and make a bee-line for Bear Lake, Logan Canyon, and home: the walks I’ve already known for some time.

Perhaps you’re inspired now to know parts of this walk better yourself.

I’m Josh Boling, and I’m Wild About Utah!

Credits:

Imaginary Wanderings:
Photos: Courtesy and Copyright Josh Boling, Photographer
Audio: Includes audio from
Text: Josh Boling, 2020, Edith Bowen Laboratory School, Utah State University

Sources & Additional Reading

Boling, Josh, Why I Teach Outside, Wild About Utah, November 11, 2019, https://wildaboututah.org/why-i-teach-outside/

Kiffel-Alcheh, Utah, National Geographic Kids, https://kids.nationalgeographic.com/explore/states/utah/

The Geography of Utah, NSTATE LLC, https://www.netstate.com/states/geography/ut_geography.htm

Fisher, Albert L, Physical Geography of Utah, History to Go, Utah Division of State History, https://historytogo.utah.gov/physical-geography-utah/

March 2, 2020July 2, 2024

Logan River’s Evolving Geomorphology

Logan River’s geomorphology, or landform, has changed very little over the past 150 years in the mountain canyons. But where the river leaves the mountains and drops down onto Cache Valley’s floor, its geomorphology has changed dramatically.

A river’s geomorphology is how it interacts with its environment, how it changes and moves over time, how it picks up sediment and debris when its flowing fast then releases the sediments downstream where the river slows and spreads over open-flat landscapes.

Logan Rivers evolving geomorphology: Logan River’s Evolving Geomorphology: Father and son enjoying a day of fishing on the reservoir behind First dam in the mouth of Logan Canyon Courtesy & Copyright Shauna Leavitt, Photographer — Father and son enjoying a day of fishing on the reservoir behind First dam in the mouth of Logan Canyon
Courtesy & Copyright Shauna Leavitt, Photographer

The route of Logan River is noteworthy. Peter Wilcock, department head of Watershed Sciences in the Quinney College of Natural Resources explains, Logan River cuts through a large amount of the Bear River mountain range [in northeastern Utah and southeastern Idaho] and is by far the biggest drainage from the range.

The river’s size has made a mark on the mountain. When all the tributaries and springs come together, the result is the fast-flowing river with great force for erosion. If you compare Logan Canyon with other canyons coming out of the Bear River Range such as Green Canyon or Providence Canyon you can see Logan Canyon is close to 600 feet lower than all the other canyons. The volume and force of Logan River cut through the beach material that ancient Lake Bonneville left behind, the other drainages have been too small to cut through the ancient short line.

In the early 1800s, the lower part of Logan River flowed freely, meandering and spreading across the Cache Valley floor. As it entered the valley, the river would form into an alluvial fan spreading like fingers over the valley floor and meeting the natural functions of a river to transport water, sediments and nutrients.

As each decade passed an increasing number of buildings, roads and complex infrastructures were built to keep up with the growing population. And to protect this infrastructure, people attempted to restrict the movements of the river. In many places, the river was straightened or channelized even as its water was re-routed for irrigation.

The dams placed along the river and at the mouth of Logan Canyon slowed the river before it reached the valley floor. As a result, a large percentage of the sediments which would have dropped on the valley floor, are now captured behind the river’s dams and fill the reservoirs.

Frank Howe, chairman of the Logan River Task Force, explains how this impacts the river’s geomorphology, “Water released from the dams is free of deposits; the river is now “hungry” – hungry for new sediments. It’s now capable of picking up large amounts of sediments which causes erosion problems miles below the dams.”

The Logan River Task Force, consisting of representatives from Utah State University, Logan City, Cache County, State and Federal Agencies, six non-profit organizations, corporations and interested citizens came together to find solutions to the erosion problem and other river issues. To address these issues, they prepared a “long-term plan for the Logan River to balance ecological and social values and capture what Cache Valley community wants the river to become. “

Rivers, by nature, are dynamic. They move back and forth especially where the slope is gentle. Over time, this meandering movement delivers fine sediments, across the river’s floodplains creating rich soils diverse in vegetation and wildlife. By changing the river’s geomorphology, we’ve altered the rivers dynamics, as well as how and where it delivers sediments.

Fortunately, parts of the Logan River’s geomorphology can be restored. River restoration will be the topic of our fourth and final segment for the Logan River series on Wild About Utah.

This is Shauna Leavitt and I’m wild about Utah.

Logan River’s Evolving Geomorphology-Credits:
Photos: Courtesy & Copyright ©
Audio: Courtesy & Copyright © Friend Weller, Utah Public Radio
Text: Shauna Leavitt, Utah Cooperative Fish and Wildlife Research Unit, Quinney College of Natural Resources, Utah State University
Co-Authored by: Frank Howe, chairman of the Logan River Task Force, adjunct associate professor, and university liaison for Utah Division of Wildlife Resources.

Logan River’s Evolving Geomorphology-Additional Reading

Leavitt, Shauna, A Short History of the Logan River, Wild About Utah, November 4, 2019, https://wildaboututah.org/short-history-of-logan-river/

Leavitt, Shauna, The Ecology in and around the Logan River, Wild About Utah, December 2, 2019, https://wildaboututah.org/the-ecology-in-and-around-the-logan-river/

Williams, Edmond J, Geomorphic Features and History of the Lower Part of Logan Canyon, Utah, Thesis, MS Science 2964, Donald R. Olsen Chair, Department of Geology, Utah State University, https://digitalcommons.usu.edu/etd/6644/

James P. Evans, James P. McCalpinl, David C. Holmes, Geologic Map of the Logan 7.5′ Quadrangle, Cache County, Utah, Department of Geology, Utah State University, Utah Geological Survey, Utah Department of Natural Resources, 1996, https://ugspub.nr.utah.gov/publications/misc_pubs/mp-96-1.pdf

Hylland, Rebecca, What are Igneous, Sedimentary & Metamorphic Rocks?, Glad You Asked, Utah Geological Survey, https://geology.utah.gov/map-pub/survey-notes/glad-you-asked/igneous-sedimentary-metamorphic-rocks/

Map of the Deltas formed in Lake Bonneville by the Logan River, U.S. Geological Survey, ca. 1890, Held in the Utah State University, Merrill-Cazier Library, Special Collections and Archives
https://digital.lib.usu.edu/digital/collection/Bear/id/109/