Grand Canyon National Park

Grand Canyon National Park

Carved out by the Colorado River, the Grand Canyon (nearly 1,500 m deep) is the most spectacular gorge in the world. Located in the state of Arizona, it cuts across the Grand Canyon National Park. Its horizontal strata retrace the geological history of the past 2 billion years. There are also prehistoric traces of human adaptation to a particularly harsh environment.

Parc national du Grand Canyon

Sculpté par le Colorado, le Grand Canyon, de près de 1 500 m de profondeur, est la gorge la plus spectaculaire du monde. Situé dans l'Arizona, il traverse le parc national du Grand Canyon. Ses strates horizontales retracent une histoire géologique s'étendant sur 2 milliards d'années. On y trouve aussi les vestiges préhistoriques d'une adaptation humaine à un environnement particulièrement rude.

منتزه غراند كانيون الوطني

الغراند كانيون منحوتة حفرها نهر كولورادو بمياهه وهو ينخفض في وادٍ سحيق على عمق أكثر من 15000 متر وهو المضيق الأعظم في العالم. يقع في أريزونا ويعبر منتزه غراند كانيون الوطني. تخطّ طبقاته الأفقيّة سيرة تاريخ جيولوجي يمتد على ملياري سنة. وفيه أيضاً آثار من العصر الحجري تعكس تعاطي البشر مع بيئةٍ شديدة القسوة.

source: UNESCO/ERI



source: UNESCO/ERI

Национальный парк Гранд-Каньон

Выработанный водами реки Колорадо, этот каньон глубиной до 1500 м является самым грандиозным из всех каньонов планеты. Он протягивается по территории штата Аризона, и составляет главную природную ось одноименного национального парка. Обнажающиеся геологические слои отражают последние 2 млрд. лет земной истории. Здесь также обнаружены следы пребывания доисторического человека.

source: UNESCO/ERI

Parque Nacional del Gran Cañón

Situado en el Estado de Arizona, este parque está surcado por el gigantesco cañón cavado por el río Colorado, que con sus 1.500 metros de profundidad es el desfiladero más espectacular del mundo. En sus estratos horizontales está plasmada la historia geológica de los últimos dos mil millones de años. También se hallan en este sitio vestigios de los esfuerzos de adaptación del hombre prehistórico a un entorno particularmente inhóspito.

source: UNESCO/ERI


source: NFUAJ

Nationaal park Grand Canyon

Met een diepte van bijna 1.500 meter is de Grand Canyon in de staat Arizona de meest spectaculaire kloof ter wereld . De canyon is ontstaan dankzij uitslijtprocessen van de Colorado-rivier, die het hele park doorkruist. De horizontale lagen geven de geologische geschiedenis van de afgelopen twee miljard jaar weer. Er zijn ook prehistorische sporen te vinden van mensen die zich moesten aanpassen aan de bijzonder moeilijke omstandigheden van de omgeving. Door de verschillende hoogtes in het gebied bestaat er een verscheidenheid aan klimaten en leefgebieden. Het nationaal park wordt hierdoor gezien als enorm groot biologisch museum dat zich uitstrekt over vijf verschillende leef- en vegetatiezones.


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Statement of Significance

The Grand Canyon is among the earth’s greatest on-going geological spectacles. Its vastness is stunning, and the evidence it reveals about the earth’s history is invaluable. The 1.5-kilometer (0.9 mile) deep gorge ranges in width from 500 m to 30 km (0.3 mile to 18.6 miles). It twists and turns 445 km (276.5 miles) and was formed during 6 million years of geologic activity and erosion by the Colorado River on the upraised earth’s crust. The buttes, spires, mesas and temples in the canyon are in fact mountains looked down upon from the rims. Horizontal strata exposed in the canyon retrace geological history over 2 billion years and represent the four major geologic eras.

Criterion (vii): Widely known for its exceptional natural beauty and considered one of the world's most visually powerful landscapes, the Grand Canyon is celebrated for its plunging depths; temple-like buttes; and vast, multihued, labyrinthine topography. Scenic wonders within park boundaries include high plateaus, plains, deserts, forests, cinder cones, lava flows, streams, waterfalls, and one of America’s great whitewater rivers.

Criterion (viii): Within park boundaries, the geologic record spans all four eras of the earth's evolutionary history, from the Precambrian to the Cenozoic. The Precambrian and Paleozoic portions of this record are particularly well exposed in canyon walls and include a rich fossil assemblage. Numerous caves shelter fossils and animal remains that extend the paleontological record into the Pleistocene.

Criterion (ix): Grand Canyon is an exceptional example of biological environments at different elevations that evolved as the river cut deeper portraying five of North America’s seven life zones within canyon walls. Flora and fauna species overlap in many of the zones and are found throughout the canyon.

Criterion (x): The park’s diverse topography has resulted in equally diverse ecosystems. The five life zones within the canyon are represented in a remarkably small geographic area. Grand Canyon National Park is an ecological refuge, with relatively undisturbed remnants of dwindling ecosystems (such as boreal forest and desert riparian communities), and numerous endemic, rare or endangered plant and animal species.

Long Description

Grand Canyon National Park was created on 26 February 1919 by an act of Congress. First protected in 1893 as a forest reserve in which mining, lumbering and hunting continued to be allowed: upgraded to a game reserve in 1906, giving protection to the wildlife: redesignated a National Monument in 1908.

The park is dominated by the spectacular Grand Canyon: a twisting, 1.5 km deep and 445.8 km long gorge, formed during some 6 million years of geological activity and erosion by the Colorado River on the raised Earth's crust (2.5 km above sea level). It divides the park into the North Rim and South Rim which overlook the 200 m to 30 km wide canyon; the buttes, spires, mesas and temples in the canyon are in fact mountains looked down upon from the rims. Ongoing erosion by the seasonal and permanent rivers produces impressive waterfalls and rapids of washed-down boulders along the length of the canyon and its tributaries. Exposed horizontal geological strata in the canyon span some 2,000 million years of geological history, providing evidence of the four major geological eras, early and late Precambrian, Palaeozoic, Mesozoic and Cenozoic. The early Precambrian strata, known as the Vishnu Schist formation, are devoid of fossils. The first fossil evidence appears in the late Precambrian Bass Limestone with remains of early plant forms. Subsequent strata dating from the Palaeozoic era catalogue the sequence of local history, with both marine and terrestrial fossils demonstrating the periods in the distant past when the whole region was alternately submerged and raised. The Mesozoic era is less well illustrated within the park, but tracks made by early reptiles are found to the east in the Navajo Indian reservation. They are a few fossil remains of mammals from the early Cenozoic.

Altitudinal range provides a variety of climates and habitats, ranging from desert to mountain conditions. The canyon is a vast biological museum stretching through five different life and vegetation zones: Hudsonian on the North Rim plateau with Colorado blue spruce and Rocky Mountain maple; Canadian near the North Rim, with aspen and Ponderosa and forests of Douglas fir, white fir and aspen at 2,500 m; high-altitude Transition (Ponderosa) forests of Pinus ponderosa and gambel oak; upper Sonoran on and below the South Rim with Utah juniper, pinon pine and sagebrush; and the Lower Sonoran down the canyon and at the bottom (desert cacti, rabbitbrush, mesquite, Morman tea and Manzanita).

Over 1,000 plant species have so far been identified from the park. There are 11 plant species listed as threatened in the United States statutes in the park, including Palmer amsonia, goldenweed, plains cactus, scouler catchfly, wild buckwheats, primrose and clute penstemon. In addition, 15 plant species are recommended for consideration as threatened species under the Endangered Species Act.

Concerning the fauna, 76 mammal, 299 bird and 41 reptile and amphibian species have been identified from the park and some 16 fish species inhabit the Colorado River and its tributaries. Rare or threatened birds are listed under the United States Endangered Species Act of 1973.

The park contains more than 2,600 documented prehistoric ruins, including evidence of Archaic cultures (the earliest known inhabitants), Cohonina Indians along the South Rim, and Anasazi Indians on both the South Rim, North Rim, and within the Inner Canyon. Hualapai and Havasupai Indians moved into the canyons at this time, where they remained undisturbed until the Anglo-Americans arrived in 1860. Archaeological remains show the adaptation of human societies to severe climate and physiographic environment.

Historical Description

Created a national park on 26 February 1919 by an act of Congress. First protected in 1893 as a forest reserve in which mining, lumbering and hunting continued to be allowed; upgraded to a game reserve in 1906, giving protection to the wildlife; redesignated a national monument in 1908. Accepted as a World Heritage site on 24 October _979.

Source: Advisory Body Evaluation