DOCSLIB.ORG

Highway Frontage | 21 Acres Sec 26, T40S, R21E, Bluff UT 84512

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Highway Frontage | 21 Acres Sec 26, T40S, R21E, Bluff UT 84512 Highway Frontage | 21 Acres Sec 26, T40S, R21E, Bluff UT 84512 O F F E R I N G M E M O R A N D U M Highway Frontage | 21 Acres CONTENTS 01 Executive Summary Offering Summary 5 Zoning Summary 6 Development Summary 8 Location Summary 9 02 Property Description Aerial Map 15 Parcel Map 17 03 Demographics Demographics 22 Demographic Charts 24 Exclusively Marketed by: Trenton Bright Cole Waterfall Daniel Davis Paul Pursell Associate Broker Sales Agent Sales Agent Director of Commercial Real Estate Lic: 7961776-AB00 Lic: 7839895-SA00 Lic: 11123399-SA00 Lic: 9894235-AB00 (435) 820-6801 (385) 347-2457 (435) 650-4294 (801) 300-2466 [email protected] [email protected] [email protected] [email protected] We obtained the following information above from sources we believe to be reliable. However, we have not verified its accuracy and make no guarantee, warranty or representation about it. It is submitted subject to the possibility of errors, omissions, change of price, rental or other conditions, prior sale, lease or financing, or withdrawal without notice. We include projections, opinions, assumptions or estimates for example only, and they may not represent the current or future performance of the property. You and your tax and legal advisors should conduct your own investigation of the property and transaction. Highway Frontage | 21 Acres Disclaimer | 03 Confidentiality & Disclaimer All materials and information received or derived from KW South Valley Keller Williams its directors, officers, agents, advisors, affiliates and/or any third party sources are provided without representation or warranty as to completeness , veracity, or accuracy, condition of the property, compliance or lack of compliance with applicable governmental requirements, developability or suitability, financial performance of the property, projected financial performance of the property for any party’s intended use or any and all other matters. Neither KW South Valley Keller Williams its directors, officers, agents, advisors, or affiliates makes any representation or warranty, express or implied, as to accuracy or completeness of the materials or information provided, derived, or received. Materials and information from any source, whether written or verbal, that may be furnished for review are not a substitute for a party’s active conduct of its own due diligence to determine these and other matters of significance to such party. KW South Valley Keller Williams will not investigate or verify any such matters or conduct due diligence for a party unless otherwise agreed in writing. EACH PARTY SHALL CONDUCT ITS OWN INDEPENDENT INVESTIGATION AND DUE DILIGENCE. Any party contemplating or under contract or in escrow for a transaction is urged to verify all information and to conduct their own inspections and investigations including through appropriate third-party independent professionals selected by such party. All financial data should be verified by the party including by obtaining and reading applicable documents and reports and consulting appropriate independent professionals. KW South Valley Keller Williams makes no warranties and/or representations regarding the veracity, completeness, or relevance of any financial data or assumptions. KW South Valley Keller Williams does not serve as a financial advisor to any party regarding any proposed transaction. All data and assumptions regarding financial performance, including that used for financial modeling purposes, may differ from actual data or performance. Any estimates of market rents and/or projected rents that may be provided to a party do not necessarily mean that rents can be established at or increased to that level. Parties must evaluate any applicable contractual and governmental limitations as well as market conditions, vacancy factors and other issues in order to determine rents from or for the property. Legal questions should be discussed by the party with an attorney. Tax questions should be discussed by the party with a certified public accountant or tax attorney. Title questions should be discussed by the party with a title officer or attorney. Questions regarding the condition of the property and whether the property complies with applicable governmental requirements should be discussed by the party with appropriate engineers, architects, contractors, other consultants and governmental agencies. All properties and services are marketed by KW South Valley Keller Williams in compliance with all Copyright © 2020 CREOP, LLC. All Rights Reserved. applicable fair housing and equal opportunity laws. Highway Frontage | 21 Acres Executive Summary 01 Executive Summary Offering Summary Zoning Summary HIGHWAY FRONTAGE | 21 ACRES Development Summary Location Summary ................................................ Highway Frontage | 21 Acres Offering Summary | 05 OFFERING SUMMARY ADDRESS Sec 26, T40S, R21E Bluff UT 84512 COUNTY San Juan OFFERING PRICE $1,100,000 PRICE PSF $1.20 LAND SF 914,324 SF PRICE PER ACRE $52,405.90 ZONING TYPE R # OF PARCELS 1 APN 40S21E266000 Highway Frontage | 21 Acres APEX Commercial Real Estate | KW South Valley Keller Williams is pleased to present the sale of a 21 Acre Parcel that is located on Highway US-191 in the historic Bluff, Utah. The property is located approx. 0.5 Miles South from the developed district of town. Prime Development Property The property is currently zoned R-Residential, however, previously this property was zoned C-3 prior to Bluff being incorporated back in 2018, when the new planning and zoning commission was implemented and rezoned this property. It is recommended to convert this property back to C-3. Great Property for RV Park, Campground, Tourism Business Located in a central location for Several National Monuments and National Parks, providing a great opportunity for touring company and/or a place for the thousands of RV's that pass through this location as they visit the Mighty-5 in Utah. High Visibility Location This property boasts an excellent “Main Street” location on the Southwest end of town. Highway US-191 happens to be main street of Bluff, UT and continues south to the many attractions Southeast Utah has to offer. DESERT ROSE RESORT Zoning Summary | 06 Current Zoning | Residential District A. Allowed uses include single family homes; accessory dwelling units; accessory structures; duplexes; apartments; condominiums; parks, open space; places of worship; government and public buildings; and home occupations. B. Setbacks in the Residential district shall be twenty-five (25) feet from the front right of way and fifteen (15) feet from side and rear property boundaries. C. Accessory structures. The maximum accessory structure building height shall be eighteen (18) feet measured from finished grade of the primary structure to the peak of the roof. D. Minimum lot area shall be one half (1/2) acre for one dwelling unit and one accessory dwelling unit. For nonconforming lots, see Section 6.01.030 F. E. Building Height. The maximum building height shall be twenty-six (26) feet measured from finished grade of the primary structure to the peak of the roof. Chimneys, antennae, ornamental elements, or the like shall not be used in calculating maximum building height. Dwellings shall not exceed two (2) stories above finished grade level. Zoning Documents Zoning Ordinance.pdf Zoning Map.pdf Zoning Map West.pdf DESERT ROSE RESORT Zoning Summary | 07 Recommended Zoning | Commercial C-3 District A. Allowed uses in the C-3 District include: all uses allowed in the C-1 or C-2 districts; amusement or recreational facilities; golf courses; vehicle or automotive sales; building material supply (wholesale or retail, including outdoor storage); hotels, motels, and lodging establishments; taverns; theaters; kennels or animal shelters; and veterinary offices; recreational vehicle parks. B. Setbacks in the C-3 district shall be fifty (50) feet from the front right of way and fifteen (15) feet from side and rear property boundaries. C. Minimum lot size shall be three quarters of an (.75) acre. D. Building Height. The maximum building height shall be thirty-five (35) feet measured from finished grade of the primary structure to the peak of the roof. Chimneys, antennae, ornamental elements, or the like shall not be used in calculating maximum building height. Zoning Documents Zoning Ordinance.pdf Zoning Map.pdf Zoning Map West.pdf DESERT ROSE RESORT Development Summary | 08 Future Development of Bluff, UT Bluff is a recently new incorporated town located in the southeast region of Utah. Several studies were completed by universities and Bonneville Research to determine the feasibility of Bluff becoming an incorporated town. These include: a city wide survey named "Listening to Bluff", a Regional Framework for Southern San Juan County, Utah Study, along with a feasibility study. These studies clearly state the economics, feasibility, and the desires of the Bluff community, and will be a crucial component of any new land/business owner in the area. "Listening to Bluff" Bluff Incorporation Feasibility Study Regional Framework Study In the fall of 2016 the University of Utah was invited The results of this study indicate that-incorporation Bluff sits at the southern end of San Juan County, in to work in collaboration with the community of Bluff is feasible for the Bluff Study Area, based the southeastern Utah. The area remains mostly rural in to assist in developing an idea of what the future requirements of Utah Code 10-2a-302. its industries, population, and policies. With the could hold for the community. The mission for Bears Ears National Monument designation, Listening to Bluff is to work in collaboration with the * The proposed incorporated Town of Bluff would development pressure has increased throughout the community; to listen and seek to understand the have an initial population of 265 persons and 25 region. The region will face challenges regarding character, stories, values, and goals guiding the current businesses employing 167 persons. how best to manage the anticipated growth without future of Bluff. losing the character and authenticity that makes the * Bluff is located in the southern portion of San Juan region special.
Load more

Recommended publications
  • Monument Valley Meander
    RV Traveler's Roadmap to Monument Valley Meander However you experience it, the valley is a wonder to behold, a harsh yet hauntingly beautiful landscape. View it in early morning, when shadows lift from rocky marvels. Admire it in springtime,when tiny pink and blue wildflowers sprinkle the land with jewel-like specks of color. Try to see it through the eyes of the Navajos, who still herd their sheep and weave their rugs here. 1 Highlights & Facts For The Ideal Experience Agathla Peak Trip Length: Roughly 260 miles, plus side trips Best Time To Go: Spring - autumn What To Watch Out For: When on Indian reservations abide by local customs. Ask permission before taking photos, never disturb any of the artifacts. Must See Nearby Attractions: Grand Canyon National Park (near Flagstaff, AZ) Petrified Forest National Park (near Holbrook, AZ) Zion National Park (Springdale, UT) 2 Traveler's Notes Monument Valley Navajo Tribal Park The stretch of Rte. 163 called the Trail of the Ancients in honor of the vanished Anasazis cuts across Monument Valley at the Utah border on its way to the little town of Mexican Hat. Named for a rock formation there that resembles an upside-down sombrero a whimsical footnote to the magnificence of Monument Valley—Mexican Hat is the nearest settlement to Goosenecks State Park, just ahead and to the west via Rtes. 261 and 316. The monuments in the park have descriptive names. They are based on ones imagination. These names were created by the early settlers of Monument Valley. Others names portray a certain meaning to the Navajo people.
    [Show full text]
  • Reevaluating Evidence for the Pre-Lllinoian Entrenchment of Northeastern Iowa River Valleys
    Journal of the Iowa Academy of Science: JIAS Volume 95 Number Article 3 1988 Reevaluating Evidence for the Pre-lllinoian Entrenchment of Northeastern Iowa River Valleys Curtis M. Hudak University of Iowa Let us know how access to this document benefits ouy Copyright © Copyright 1989 by the Iowa Academy of Science, Inc. Follow this and additional works at: https://scholarworks.uni.edu/jias Part of the Anthropology Commons, Life Sciences Commons, Physical Sciences and Mathematics Commons, and the Science and Mathematics Education Commons Recommended Citation Hudak, Curtis M. (1988) "Reevaluating Evidence for the Pre-lllinoian Entrenchment of Northeastern Iowa River Valleys," Journal of the Iowa Academy of Science: JIAS, 95(4), 109-113. Available at: https://scholarworks.uni.edu/jias/vol95/iss4/3 This Research is brought to you for free and open access by the Iowa Academy of Science at UNI ScholarWorks. It has been accepted for inclusion in Journal of the Iowa Academy of Science: JIAS by an authorized editor of UNI ScholarWorks. For more information, please contact [email protected]. ]our. Iowa Acad. Sci. 95(4): 109-113, 1988 Reevaluating Evidence for the Pre-lllinoian Entrenchment of Northeastern Iowa River Valleys 1 CURTIS M. HUDAK2 Department of Geology, University of Iowa, Iowa City, Iowa 52242 Previous workers have proposed a pre-Illinoian age for the deepest bedrock entrenchment of northeastern Iowa valleys. Lines of evidence used ro support a pre-Illinoian age of entrenchment are: ( 1) deep bedrock-entrenchment interpreted ro take "long" periods of time, (2) "valleys" filled with "red-weathered drift", which was interpreted as "old", (3) differences in cross-valley profiles supposedly related to glacial advances, (4) thick beds of gravel could only be deposited by outwash streams, and (5) glacially buried (drift-filled) bedrock valleys exist outside of the Paleozoic Plateau ro the west and south.
    [Show full text]
  • Status and Ecology of Mexican Spotted Owls in the Upper Gila Mountains Recovery Unit, Arizona and New Mexico
    Status and Ecology of Mexican Spotted Owls in the Upper Gila Mountains Recovery Unit, Arizona and New Mexico Joseph L. Ganey James P. Ward, Jr. David W. Willey United States Forest Rocky Mountain General Technical Report Department Service Research Station RMRS-GTR-256WWW of Agriculture May 2011 Ganey, Joseph L.; Ward, James P. Jr.; Willey, David W. 2011. Status and ecology of Mexican spotted owls in the Upper Gila Mountains recovery unit, Arizona and New Mexico. Gen. Tech. Rep. RMRS-GTR-256WWW. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station. 94 p. Abstract This report summarizes current knowledge on the status and ecology of the Mexican spot- ted owl within the Upper Gila Mountains Recovery Unit (UGM RU). It was written at the request of U.S. Forest Service personnel involved in the Four Forests Restoration Initia- tive (4FRI), a collaborative, landscape-scale restoration effort covering approximately 2.4 million ac (1 million ha) across all or part of four National Forests (Apache-Sitgreaves, Coconino, Kaibab, and Tonto National Forests) located within the UGM RU. The UGM RU supports >50% of the known population of Mexican spotted owls, and the central location of the UGM RU within the overall range of the owl appears to facilitate gene flow throughout that range. Consequently, the UGM population is viewed as important to stability within the overall range of the owl, and management that impacts owls within the UGM RU could affect owl populations beyond that RU. Keywords: abundance, demography, habitat selection, diet composition, movements Authors Joseph L.
    [Show full text]
  • Historical Geomorphology of the Verde River
    Historical Geomorphology of the Verde River by Philip A. Pearthree Arizona Geological Survey Open-File Report 96-13 June, 1996 Arizona Geological Survey 416 W. Congress, Suite #100, Tucson, Arizona 85701 Research conducted in cooperation with CH2MHILL as part of the basic data collection for assessment of river navigability in Arizona at the time of Statehood (1912 J. Funding was provided by the Arizona State Land Department This report is preliminary and has not been edited or reviewed for conformity with Arizona Geological Survey standards Introduction The Verde River drainage is a major river system that heads in Big Chino Valley in north­ central Arizona, flows generally southeast through the rugged terrain of central Arizona, and empties into the Salt River east of the Phoenix metropolitan area. It is unusual in Arizona because much the main channel of the Verde River is perennial for much its length. Data summarized in this report were gathered to aid in the assessment of the navigability of the Verde River in February, 1912, when Arizona became a State. These investigations were conducted in cooperation with CH2MHill and were funded by the Arizona State Land Department. The purposes of this report are to (1) outline the geologic and geomorphic framework of the Verde River, (2) to describe the physical character of the channel of the Verde River, and (3) to evaluate how channel morphology and position have changed in the past century. Physiography, Geology, and General Geomorphology of the River The Verde River heads in and flows through the rugged highlands and valleys of central Arizona (Figure 1).
    [Show full text]
  • N Red Rock Beauty N Salt Lake City N Outdoor Adventure N Dinosaurs
    n Red Rock Beauty n Salt Lake City n Outdoor Adventure n Dinosaurs Plus: Arts, Winter Sports, Golf A SPECIAL SUPPLEMENT TO THE JANUARY 2009 ISSUE OF When you come to Utah, visit TEMPLE SQUARE In the heart of Salt Lake City many venues to choose from... All are Free Brigham Young Historic Park Church Office Building State Street Conference Center Relief Society Building Main Street Lion House and Beehive House North Temple Street Salt Lake Temple Joseph Smith Memorial Building West Temple Street North Visitors' Center Tabernacle South Temple Street South Visitors' Center Museum of Church History and Art Assembly Hall Family History Library Hear the world-famous Mormon See the magnificent spires of the Find your roots in the world’s Tabernacle Choir. Salt Lake Temple. largest collection of genealogical information. Enjoy the imposing 11-foot marble Christus statue at the North Visitors' Center. For information, go to visittemplesquare.com, lds.org/placestovisit, or call 1-800-537-9703 For information about The Church of Jesus Christ of Latter-day Saints, visit mormon.org © 2008 by IRI. 7/08. Printed in the USA. 04089. Illustration of Temple Square by Dilleen Marsh © 1999 IRI. Photo of Mormon Tabernacle Choir © 2001 Busath Photography UTAH Life Elevated Utah. 4 Life Elevated Northern Utah. 8 Salt Lake, Dinosaurland & Everything Inbetween Central Utah . 14 Nordic Traditions & Outdoor Wilderness Southwestern Utah . 16 National Parks, Western History & Rugged Beauty Southeastern Utah . 22 Dinosaurs, Swells & Desert Beauty UTAH – A SPECIAL SUPPLEMENT TO THE JANUARY 2009 ISSUE OF CANADIAN TRAVELLER Published 12 times a year by 88 East Pender Street, Suite 555 Vancouver, BC Canada, V6A 3X3 Contents © 2009 by ACT Communications Inc.
    [Show full text]
  • Creating Memorable Travel Experiences Since 1979 2021
    2021 DREAM BOOK LLC CREATING MEMORABLE TRAVEL EXPERIENCES SINCE 1979 One from the Road… When we returned to the road in August, one of our first trips was By the end of the tour, you feel like you just watched Ellen, Dr. Phil across Nevada to pick up the historic (which later and Saturday Night Live. You have truly met the locals once you Lincoln Highway SUCCESS STORIES—A SpECIAl AdvERTISIng SECTIOn became U.S. 50) and make our way back to Sacramento. Small finish walking among the headstones. towns proved to be a good way to gently try and return to traveling. Sure, we would all I didn’t know Wally would even be in town. Last I heard he was prefer not to have to wear a mask and wash buying a camper and heading out to see the world when he retired. our hands every 20 minutes. But if you love For reasons I’m hopeful I’ll hear about some day, he was back in to travel, right now you have to make a few Eureka. compromises. With any luck, those will be short term and we will be able to travel more It’s possible the folks on the trip may have noticed the tear in my eye freely soon. or the crack in my voice when my friend showed up to say hi. Or when he starting telling a couple members of our group about the Our trip went well. We slipped in and out of a cemetery tour and I broke out laughing really loud.
    [Show full text]
  • Utah Geology: Making Utah's Geology More Accessible. View South-East
    5/28/13 Utah Geology: Geologic Road Guides Utah Geology: Making Utah's geology more accessible. View south-east over St. George, Utah Road Guide Quick Select. Selection Map HW-160, 163 & 191 Tuba City to Kayenta, Bluff & Montecello, Utah (through Monument Valley) 0.0 Junction of U.S. Highways 160 and 89 , HW-160 Road Guide. follows U.S. Highway 160 east toward Tuba city and Kayenta. U.S. Highway 89 leads south toward the entrance to Grand Canyon National Park and Flagstaff. For a route description along U.S. Highway 89 northward from here see HW-89A Road Guide.. The road junction is in the Petrified Forest Member of the Chinle Formation. The member is composed of interbedded stream channel sandstone and varicolored shale and mudstone. This member erodes moderately easily and forms the strike valley to the north and south. From here the route of this guide leads upsection into younger and younger beds of the Chinle Formation. 0.7 Cross Hamblin Wash and rise from the Petrified Forest Member into the pinkish banded Owl Rock Member of the Chinle Formation. The upper member forms pronounced laminated pinkish gray and green badlands, distinctly unlike the rounded Painted Desert-type massive badlands of the underlying member. 1.6 Road rises up through the upper part of the Chinle Formation, a typical wavy to hummocky road. Highway construction is easy across the slope-forming parts of the formation, but holding the road after construction is difficult because the soft volcanic ash-bearing shales heave under load or after wetting and drying.
    [Show full text]
  • RV Sites in the United States Location Map 110-Mile Park Map 35 Mile
    RV sites in the United States This GPS POI file is available here: https://poidirectory.com/poifiles/united_states/accommodation/RV_MH-US.html Location Map 110-Mile Park Map 35 Mile Camp Map 370 Lakeside Park Map 5 Star RV Map 566 Piney Creek Horse Camp Map 7 Oaks RV Park Map 8th and Bridge RV Map A AAA RV Map A and A Mesa Verde RV Map A H Hogue Map A H Stephens Historic Park Map A J Jolly County Park Map A Mountain Top RV Map A-Bar-A RV/CG Map A. W. Jack Morgan County Par Map A.W. Marion State Park Map Abbeville RV Park Map Abbott Map Abbott Creek (Abbott Butte) Map Abilene State Park Map Abita Springs RV Resort (Oce Map Abram Rutt City Park Map Acadia National Parks Map Acadiana Park Map Ace RV Park Map Ackerman Map Ackley Creek Co Park Map Ackley Lake State Park Map Acorn East Map Acorn Valley Map Acorn West Map Ada Lake Map Adam County Fairgrounds Map Adams City CG Map Adams County Regional Park Map Adams Fork Map Page 1 Location Map Adams Grove Map Adelaide Map Adirondack Gateway Campgroun Map Admiralty RV and Resort Map Adolph Thomae Jr. County Par Map Adrian City CG Map Aerie Crag Map Aeroplane Mesa Map Afton Canyon Map Afton Landing Map Agate Beach Map Agnew Meadows Map Agricenter RV Park Map Agua Caliente County Park Map Agua Piedra Map Aguirre Spring Map Ahart Map Ahtanum State Forest Map Aiken State Park Map Aikens Creek West Map Ainsworth State Park Map Airplane Flat Map Airport Flat Map Airport Lake Park Map Airport Park Map Aitkin Co Campground Map Ajax Country Livin' I-49 RV Map Ajo Arena Map Ajo Community Golf Course Map
    [Show full text]
  • The Ultimate Journey Itinerary
    The Ultimate Journey Itinerary visitutah.com /plan-your-trip/recommended-itineraries/mighty5/ultimate-journey A 10-day expedition from Salt Lake City through Arches, Canyonlands, Capitol Reef, Bryce Canyon and Zion national parks. 10 days in Southern Utah? Good choice. Take off your coat and stay awhile! You'll appreciate giving yourself a little extra time to experience each park more intimately and to be able to linger at incredible stops along the way. Explore the itinerary below or download the PDF now. Day 1: Salt Lake City to Arches National Park Distance: 231 miles/3.5 to 4 hours Adventure in Arches National Park picks up where 300 million years of patient erosion has resulted in unbelievably dramatic landscapes that look more sculpted by giant mythological beings than the processes of time. Arches National Park contains about 2,000 windowed arches, towering spires, harrowing hoodoos, and precarious pinnacles on display, including Delicate Arch, perhaps Utah's most iconic feature, which is a must-hike destination in the park. A paved 40-mile scenic drive from the park entrance provides numerous parking areas for trail access and scenic overlooks. Guided Tour: Reserve a tour through the Fiery Furnace. This twisting labyrinth of brilliant red rock fissures and spines is so intricate it is highly recommended to find your way through with a guide. Hikes: The 1.5-mile hike to Delicate Arch is beautiful, with the end reward of viewing Utah's famous landmark, a famed standing any bucket list. Or hike some of the easy short trails in the park, such as the Park Avenue Trail and trails in the Windows Section of the park, or some of the longer trails in the park, such as Double O Arch, Tower Arch, and Landscape Arch.
    [Show full text]
  • Analyzing Rivers with Google Earth
    Name____________________________________Per.______ Analyzing Rivers with Google Earth River systems exist all over the planet. You are going to examine several rivers and landforms created by rivers during this activity using Google Earth. While your iPad can view each location, you will need a laptop to use the ruler function. A B Figure 1: Meandering river terms. Image from: http://www.sierrapotomac.org/W_Needham/MeanderingRivers.htm Part I: Meandering Rivers: Figure 1 shows several terms used to describe meandering rivers. We are going to focus on wavelength, amplitude, and sinuosity. Sinuosity is the ratio of river length (distance traveled if you floated down the river) divided by straight length line (bird’s flight distance, i.e. from point A to B). The greater the number, the more tortuous (strongly meandering) the path the river takes. 1. Fly to Yakeshi, China. Just north of the city is a beautiful series of scroll bars (former point bars that have been abandoned) formed by the meandering river moving across the landscape. 1a. Describe the features you see. What “age” river is this (young, mature, old)? How are the meanders moving over time? Is the river becoming straighter or more curved? 1b. Find an area where the current river channel and clear meanders are easy to see (i.e. 49o18’30”N, 120o35’45”E). Measure the wavelength, amplitude and sinuosity of the river in this area. To measure straight line paths for wavelength, amplitude, and bird’s flight distance, go to Tools Ruler Line. Use kilometers. Click and drag your cursor across the area of interest.
    [Show full text]
  • 72-3-203 State Park Access Highways -- Escalante Petrified Forest State Park to Huntington State Park
    Utah Code 72-3-203 State park access highways -- Escalante Petrified Forest State Park to Huntington State Park. State park access highways include: (1) ESCALANTE PETRIFIED FOREST STATE PARK. Access to Escalante Petrified Forest State Park begins in Garfield County at State Highway 12 and proceeds northwesterly on a county road a distance of 1 mile to the park's visitor center and is under the jurisdiction of Garfield County. (2) FLIGHT PARK STATE RECREATION AREA. Access to Flight Park State Recreation Area begins in Utah County at East Frontage Road and proceeds northeasterly on Air Park Road, a distance of 0.5 miles to the park entrance and is under the jurisdiction of Utah County. (3) FREMONT INDIAN STATE PARK MUSEUM. Access to the Fremont Indian State Park Museum begins in Sevier County at the Sevier Junction on Highway 89 and proceeds westerly on county road 2524 to interchange 17 on Interstate 70, a distance of 5.9 miles and is under the jurisdiction of Sevier County. (4) GOBLIN VALLEY STATE PARK (East Access). The East Access to the Goblin Valley State Park begins in Emery County at the junction of State Highway 24 and county road 1012 and proceeds westerly on county road 1012, a distance of 5.2 miles; then southerly on county road 1013, a distance of 6.0 miles; then southerly on county road 1014, a distance of 0.4 miles to the park entrance. The East Access is under the jurisdiction of Emery County. (5) GOBLIN VALLEY STATE PARK (North Access). The North Access to the Goblin Valley State Park begins in Emery County at the junction of Interstate 70 and county road 332 and proceeds southwesterly on county road 332, a distance of 10 miles; then southerly on county road 1033, a distance of 3.1 miles; then southeasterly on county road 1012, a distance of 10.6 miles; then southerly on county road 1013, a distance of 6.0 miles; then southerly on county road 1014, a distance of 0.4 miles to the park entrance.
    [Show full text]
  • Abstract Cenozoic Tectonism Can Be Seen in a Variety of Different Ways In
    Abstract Cenozoic tectonism can be seen in a variety of different ways in the Coastal Plain of North Carolina. Using high resolution Light Detecting and Ranging digital elevation models (LiDAR), the geology of the coast can be analyzed to look for evidence supporting recent tectonism and disequilibrium. The rivers in the Coastal Plain, as well as other features, provide much evidence to support this theory. Looking at the complicated geomorphology of the rivers, particularly the Cape Fear River, gives insight to potential fault locations along the rivers. Most of the streams exhibit stream capture, another sign of disequilibrium, and the amount of stream capture was quantified on the Cape Fear River. There is a southwest migration trend in the major rivers of the Coastal Plain. While the Cape Fear Arch can explain this trend in the Cape Fear River, it does not explain the southwest migration in other rivers in the north as well. Knickpoints were found in all of the rivers in the Coastal Plain. While most of them can be associated with sea level fall or changes in underlying lithologies, there are many that are caused by tectonics. Wave-cut escarpments were once deposited horizontally in various places due to rises and falls in sea level. Elevation profiles along these scarps show a higher elevation in the north than in the south, which could be explained by uplift. This uplift would also account for the southwest migration trend in the rivers. Introduction As every geologist knows, everything on Earth is constantly changing. Mountains are being formed as well as destroyed, plates are moving, new crust is being formed as old crust is subducted and recycled, and rivers are moving.
    [Show full text]