Conondont biostratigraphy and thermal color alteration indices of the upper St. Charles and lower Garden City formations, Bear River Range, northern Utah and southeastern Idaho

Homeless programs often rely on landlord engagement for successful implementation. However, there is very little research that examines landlord perspectives related to homelessness. Better understanding landlords’ opinions and attitudes regarding those experiencing homelessness can inform program development and policy in the efforts to prevent and mitigate homelessness in the U.S. A 49-question survey was created and administered by social work faculty and students to landlords and property managers throughout the Bear River Region of northern Utah (N = 134). The survey contained a variety of questions that assessed landlord attitudes and knowledge toward those experiencing homelessness as well as their comfortability in renting to these individuals. Results revealed that landlords would like to help solve homelessness in their community, but they do not know where to start. Additionally, results showed that landlords’ willingness to rent to individuals experiencing homelessness is dependent on contextual factors, such as having more information regarding the individual, their income, past rental history, and other factors. Finally, results showed that landlords had biases toward specific groups of individuals experiencing homelessness (e.g., landlords felt more comfortable renting to those with physical disabilities than those with substance misuse histories). Results are discussed in context of program, policy, and research implications.

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Complementary seasonal bias in records of Holocene paleoclimate, Bear River Range, Southeast Idaho

Quaternary International ◽

10.1016/j.quaint.2015.01.149 ◽

2015 ◽

Vol 387 ◽

pp. 138

Author(s):

Zachary Lundeen ◽

Andrea Brunelle

Keyword(s):

Holocene Paleoclimate ◽

Bear River Range ◽

Bear River

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Vegetation on Soils Derived from Dolomite and Quartzite in the Bear River Range, Utah: A Comparative Study

Bulletin of the Torrey Botanical Club ◽

10.2307/2996018 ◽

1984 ◽

Vol 111 (2) ◽

pp. 179 ◽

Cited By ~ 4

Author(s):

Elizabeth E. Neely ◽

Mary E. Barkworth

Keyword(s):

Comparative Study ◽

Bear River Range ◽

Bear River

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Ricks Spring

Geosites ◽

10.31711/geosites.v1i1.64 ◽

2019 ◽

Vol 1 ◽

pp. 1-6

Author(s):

Lawrence Spangler

Keyword(s):

Cold Weather ◽

National Forest ◽

Karst Springs ◽

Standing Water ◽

Bear River Range ◽

Small Pool ◽

Bear River ◽

Cache County ◽

The City

Ricks Spring is one of several major karst springs that discharge along the Logan River in the Bear River Range in Cache County, Utah. The spring is located along U.S. Highway 89 in Logan Canyon about 17 miles (27.4 kilometers) northeast of (up-canyon from) the city of Logan, at mile marker 477. It lies within Uinta-Wasatch-Cache National Forest at an elevation of 5880 feet (1792 meters). Situated at the base of a hillside, the spring is one of the largest and most scenic along the Logan River (figure 1). Water from the spring flows out of a large alcove, under Highway 89, and into the Logan River, about 150 feet (45 meters) from the spring. Pullouts on both sides of the highway provide parking for visitors to the spring, and a boardwalk crosses the spring run, which allows access to the rise pool in the alcove. Several signs at the spring provide information about its history and hydrology. Ricks Spring typically flows during the spring, summer, and fall months, but can have periods of no flow during the winter months, particularly during extended periods of cold weather. During these times, the water in the rise pit recedes to a small pool of standing water that can contain fish, which presumably originate from the nearby Logan River. During the last 10 years, cave divers have explored the conduit that feeds the spring for about 2300 feet (700 meters) into the mountainside.

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Evidence for a Shallow Early or Middle Wisconsin-Age Lake in the Bonneville Basin, Utah

Quaternary Research ◽

10.1016/0033-5894(87)90081-0 ◽

1987 ◽

Vol 27 (3) ◽

pp. 248-262 ◽

Cited By ~ 32

Author(s):

Charles G. Oviatt ◽

William D. McCoy ◽

Richard G. Reider

Keyword(s):

Oxygen Isotope ◽

Stage Ii ◽

Fine Grained ◽

Northern Utah ◽

Bear River ◽

Buried Soil ◽

Bonneville Basin ◽

Lacustrine Facies

AbstractRelatively complete stratigraphic records of the Bonneville cycle and of at least one and probably two earlier lacustrine are exposed along the Bear River below Cutler Dam in northern Utah between altitudes of 1290 and 1365 m. In most exposures the unconformity between the Bonneville Alloformation and the underlying unit, herein named the Cutler Dam Alloformation, is marked by slight erosional relief and by a weakly to moderately developed buried soil, herein named the Fielding Geosol. In truncated profiles, the Fielding Geosol reaches a maximum of stage II carbonate morphology. Wood from near the base of the Cutler Dam Alloformation yielded a 14C date of >36,000 yr B.P. (Beta-9845). Alloisoleucine/isoleucine (aIle/Ile) ratios of Sphaerium shells from the Cutler Dam beds average 0.15 ± 0.01 in the total hydrolysate, which is significantly greater than the average for Sphaerium shells of Bonneville age elsewhere in the basin. Therefore, the Cutler Dam Alloformation is older than 36,000 yr B.P., but much younger than deposits of the Little Valley lake cycle (140,000 yr B.P.?) which bear shells having significantly higher aIle/Ile ratios. The Cutler Dam Alloformation along the Bear River may be broadly correlative with marine oxygen-isotope stages 4 or 3. Fine-grained, fossiliferous, marginal-lacustrine facies of the Cutler Dam Alloformation are exposed at altitudes near 1340 m, and are probably the highest exposures of sediments deposited in the early or middle Wisconsin lake in the Bonneville basin.

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