96-24716. Establishment of the Grand Staircase-Escalante National Monument  

  • [Federal Register Volume 61, Number 186 (Tuesday, September 24, 1996)]
    [Presidential Documents]
    [Pages 50223-50227]
    From the Federal Register Online via the Government Publishing Office [www.gpo.gov]
    [FR Doc No: 96-24716]
    
    
          
    
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    Part VIII
    
    
    
    
    
    The President
    
    
    
    
    
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    Proclamation 6920--Establishment of the Grand Staircase-Escalante 
    National Monument
    
    
                            Presidential Documents 
    
    
    
    Federal Register / Vol. 61, No. 186 / Tuesday, September 24, 1996 / 
    Presidential Documents
    
    ___________________________________________________________________
    
    Title 3--
    The President
    
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                    Proclamation 6920 of September 18, 1996
    
                    
    Establishment of the Grand Staircase-Escalante 
                    National Monument
    
                    By the President of the United States of America
    
                    A Proclamation
    
                    The Grand Staircase-Escalante National Monument's vast 
                    and austere landscape embraces a spectacular array of 
                    scientific and historic resources. This high, rugged, 
                    and remote region, where bold plateaus and multi-hued 
                    cliffs run for distances that defy human perspective, 
                    was the last place in the continental United States to 
                    be mapped. Even today, this unspoiled natural area 
                    remains a frontier, a quality that greatly enhances the 
                    monument's value for scientific study. The monument has 
                    a long and dignified human history: it is a place where 
                    one can see how nature shapes human endeavors in the 
                    American West, where distance and aridity have been 
                    pitted against our dreams and courage. The monument 
                    presents exemplary opportunities for geologists, 
                    paleontologists, archeologists, historians, and 
                    biologists.
    
                    The monument is a geologic treasure of clearly exposed 
                    stratigraphy and structures. The sedimentary rock 
                    layers are relatively undeformed and unobscured by 
                    vegetation, offering a clear view to understanding the 
                    processes of the earth's formation. A wide variety of 
                    formations, some in brilliant colors, have been exposed 
                    by millennia of erosion. The monument contains 
                    significant portions of a vast geologic stairway, named 
                    the Grand Staircase by pioneering geologist Clarence 
                    Dutton, which rises 5,500 feet to the rim of Bryce 
                    Canyon in an unbroken sequence of great cliffs and 
                    plateaus. The monument includes the rugged canyon 
                    country of the upper Paria Canyon system, major 
                    components of the White and Vermilion Cliffs and 
                    associated benches, and the Kaiparowits Plateau. That 
                    Plateau encompasses about 1,600 square miles of 
                    sedimentary rock and consists of successive south-to-
                    north ascending plateaus or benches, deeply cut by 
                    steep-walled canyons. Naturally burning coal seams have 
                    scorched the tops of the Burning Hills brick-red. 
                    Another prominent geological feature of the plateau is 
                    the East Kaibab Monocline, known as the Cockscomb. The 
                    monument also includes the spectacular Circle Cliffs 
                    and part of the Waterpocket Fold, the inclusion of 
                    which completes the protection of this geologic feature 
                    begun with the establishment of Capitol Reef National 
                    Monument in 1938 (Proclamation No. 2246, 50 Stat. 
                    1856). The monument holds many arches and natural 
                    bridges, including the 130-foot-high Escalante Natural 
                    Bridge, with a 100 foot span, and Grosvenor Arch, a 
                    rare ``double arch.'' The upper Escalante Canyons, in 
                    the northeastern reaches of the monument, are 
                    distinctive: in addition to several major arches and 
                    natural bridges, vivid geological features are laid 
                    bare in narrow, serpentine canyons, where erosion has 
                    exposed sandstone and shale deposits in shades of red, 
                    maroon, chocolate, tan, gray, and white. Such diverse 
                    objects make the monument outstanding for purposes of 
                    geologic study.
    
                    The monument includes world class paleontological 
                    sites. The Circle Cliffs reveal remarkable specimens of 
                    petrified wood, such as large unbroken logs exceeding 
                    30 feet in length. The thickness, continuity and broad 
                    temporal distribution of the Kaiparowits Plateau's 
                    stratigraphy provide significant opportunities to study 
                    the paleontology of the late Cretaceous Era. Extremely 
                    significant fossils, including marine and brackish 
                    water mollusks, turtles, crocodilians, lizards, 
                    dinosaurs, fishes, and mammals, have been recovered
    
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                    from the Dakota, Tropic Shale and Wahweap Formations, 
                    and the Tibbet Canyon, Smoky Hollow and John Henry 
                    members of the Straight Cliffs Formation. Within the 
                    monument, these formations have produced the only 
                    evidence in our hemisphere of terrestrial vertebrate 
                    fauna, including mammals, of the Cenomanian-Santonian 
                    ages. This sequence of rocks, including the overlaying 
                    Wahweap and Kaiparowits formations, contains one of the 
                    best and most continuous records of Late Cretaceous 
                    terrestrial life in the world.
    
                    Archeological inventories carried out to date show 
                    extensive use of places within the monument by ancient 
                    Native American cultures. The area was a contact point 
                    for the Anasazi and Fremont cultures, and the evidence 
                    of this mingling provides a significant opportunity for 
                    archeological study. The cultural resources discovered 
                    so far in the monument are outstanding in their variety 
                    of cultural affiliation, type and distribution. 
                    Hundreds of recorded sites include rock art panels, 
                    occupation sites, campsites and granaries. Many more 
                    undocumented sites that exist within the monument are 
                    of significant scientific and historic value worthy of 
                    preservation for future study.
    
                    The monument is rich in human history. In addition to 
                    occupations by the Anasazi and Fremont cultures, the 
                    area has been used by modern tribal groups, including 
                    the Southern Paiute and Navajo. John Wesley Powell's 
                    expedition did initial mapping and scientific field 
                    work in the area in 1872. Early Mormon pioneers left 
                    many historic objects, including trails, inscriptions, 
                    ghost towns such as the Old Paria townsite, rock 
                    houses, and cowboy line camps, and built and traversed 
                    the renowned Hole-in-the-Rock Trail as part of their 
                    epic colonization efforts. Sixty miles of the Trail lie 
                    within the monument, as does Dance Hall Rock, used by 
                    intrepid Mormon pioneers and now a National Historic 
                    Site.
    
                    Spanning five life zones from low-lying desert to 
                    coniferous forest, with scarce and scattered water 
                    sources, the monument is an outstanding biological 
                    resource. Remoteness, limited travel corridors and low 
                    visitation have all helped to preserve intact the 
                    monument's important ecological values. The blending of 
                    warm and cold desert floras, along with the high number 
                    of endemic species, place this area in the heart of 
                    perhaps the richest floristic region in the 
                    Intermountain West. It contains an abundance of unique, 
                    isolated communities such as hanging gardens, tinajas, 
                    and rock crevice, canyon bottom, and dunal pocket 
                    communities, which have provided refugia for many 
                    ancient plant species for millennia. Geologic uplift 
                    with minimal deformation and subsequent downcutting by 
                    streams have exposed large expanses of a variety of 
                    geologic strata, each with unique physical and chemical 
                    characteristics. These strata are the parent material 
                    for a spectacular array of unusual and diverse soils 
                    that support many different vegetative communities and 
                    numerous types of endemic plants and their pollinators. 
                    This presents an extraordinary opportunity to study 
                    plant speciation and community dynamics independent of 
                    climatic variables. The monument contains an 
                    extraordinary number of areas of relict vegetation, 
                    many of which have existed since the Pleistocene, where 
                    natural processes continue unaltered by man. These 
                    include relict grasslands, of which No Mans Mesa is an 
                    outstanding example, and pinon-juniper communities 
                    containing trees up to 1,400 years old. As witnesses to 
                    the past, these relict areas establish a baseline 
                    against which to measure changes in community dynamics 
                    and biogeochemical cycles in areas impacted by human 
                    activity. Most of the ecological communities contained 
                    in the monument have low resistance to, and slow 
                    recovery from, disturbance. Fragile cryptobiotic 
                    crusts, themselves of significant biological interest, 
                    play a critical role throughout the monument, 
                    stabilizing the highly erodible desert soils and 
                    providing nutrients to plants. An abundance of packrat 
                    middens provides insight into the vegetation and 
                    climate of the past 25,000 years and furnishes context 
                    for studies of evolution and climate change. The 
                    wildlife of the monument is characterized by a 
                    diversity of species. The monument varies greatly in 
                    elevation and topography and is in a climatic zone 
                    where northern and southern
    
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                    habitat species intermingle. Mountain lion, bear, and 
                    desert bighorn sheep roam the monument. Over 200 
                    species of birds, including bald eagles and peregrine 
                    falcons, are found within the area. Wildlife, including 
                    neotropical birds, concentrate around the Paria and 
                    Escalante Rivers and other riparian corridors within 
                    the monument.
    
                    Section 2 of the Act of June 8, 1906 (34 Stat. 225, 16 
                    U.S.C. 431) authorizes the President, in his 
                    discretion, to declare by public proclamation historic 
                    landmarks, historic and prehistoric structures, and 
                    other objects of historic or scientific interest that 
                    are situated upon the lands owned or controlled by the 
                    Government of the United States to be national 
                    monuments, and to reserve as a part thereof parcels of 
                    land, the limits of which in all cases shall be 
                    confined to the smallest area compatible with the 
                    proper care and management of the objects to be 
                    protected.
    
                    NOW, THEREFORE, I, WILLIAM J. CLINTON, President of the 
                    United States of America, by the authority vested in me 
                    by section 2 of the Act of June 8, 1906 (34 Stat. 225, 
                    16 U.S.C. 431), do proclaim that there are hereby set 
                    apart and reserved as the Grand Staircase-Escalante 
                    National Monument, for the purpose of protecting the 
                    objects identified above, all lands and interests in 
                    lands owned or controlled by the United States within 
                    the boundaries of the area described on the document 
                    entitled ``Grand Staircase-Escalante National 
                    Monument'' attached to and forming a part of this 
                    proclamation. The Federal land and interests in land 
                    reserved consist of approximately 1.7 million acres, 
                    which is the smallest area compatible with the proper 
                    care and management of the objects to be protected.
    
                    All Federal lands and interests in lands within the 
                    boundaries of this monument are hereby appropriated and 
                    withdrawn from entry, location, selection, sale, 
                    leasing, or other disposition under the public land 
                    laws, other than by exchange that furthers the 
                    protective purposes of the monument. Lands and 
                    interests in lands not owned by the United States shall 
                    be reserved as a part of the monument upon acquisition 
                    of title thereto by the United States.
    
                    The establishment of this monument is subject to valid 
                    existing rights.
    
                     Nothing in this proclamation shall be deemed to 
                    diminish the responsibility and authority of the State 
                    of Utah for management of fish and wildlife, including 
                    regulation of hunting and fishing, on Federal lands 
                    within the monument.
    
                    Nothing in this proclamation shall be deemed to affect 
                    existing permits or leases for, or levels of, livestock 
                    grazing on Federal lands within the monument; existing 
                    grazing uses shall continue to be governed by 
                    applicable laws and regulations other than this 
                    proclamation.
    
                    Nothing in this proclamation shall be deemed to revoke 
                    any existing withdrawal, reservation, or appropriation; 
                    however, the national monument shall be the dominant 
                    reservation.
    
                    The Secretary of the Interior shall manage the monument 
                    through the Bureau of Land Management, pursuant to 
                    applicable legal authorities, to implement the purposes 
                    of this proclamation. The Secretary of the Interior 
                    shall prepare, within 3 years of this date, a 
                    management plan for this monument, and shall promulgate 
                    such regulations for its management as he deems 
                    appropriate. This proclamation does not reserve water 
                    as a matter of Federal law. I direct the Secretary to 
                    address in the management plan the extent to which 
                    water is necessary for the proper care and management 
                    of the objects of this monument and the extent to which 
                    further action may be necessary pursuant to Federal or 
                    State law to assure the availability of water.
    
                    Warning is hereby given to all unauthorized persons not 
                    to appropriate, injure, destroy, or remove any feature 
                    of this monument and not to locate or settle upon any 
                    of the lands thereof.
    
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                    IN WITNESS WHEREOF, I have hereunto set my hand this 
                    eighteenth day of September, in the year of our Lord 
                    nineteen hundred and ninety-six, and of the 
                    Independence of the United States of America the two 
                    hundred and twenty-first.
    
                        (Presidential Sig.)
    
    [FR Doc. 96-24716
    Filed 9-23-96; 12:27 pm]
    
    Billing code 3195-01-P
    
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    [GRAPHIC] [TIFF OMITTED] TD24SE96.086
    
    
    
    Billing code 3195-01-C
    
    
    

Document Information

Published:
09/24/1996
Department:
Executive Office of the President
Entry Type:
Presidential Document
Document Type:
Proclamation
Document Number:
96-24716
Pages:
50223-50227 (5 pages)
EOCitation:
of 1996-09-18
PDF File:
96-24716.pdf