Question: What is the elevation range for the area that the eastern sector of the Colorado orogeny extends into?

Context articles: Los Estoraques Unique Natural Area
Colorado orogeny
Vikos–Aoös National Park
Nevadan orogeny
Swall Meadows, California
Sourdough Glacier
Algoman orogeny
High Plains (United States)
Sierra Nevada lower montane forest
East European Platform

The Los Estoraques Unique Natural Area (Spanish: "Área Natural Única Los Estoraques" ) is one of the smaller national parks, covering only 6 km2 , located in the Cordillera Oriental of Colombia in the Norte de Santander Department.
 The landscape is shaped by large brownstone pedestals and columns formed by thousands of years of erosion.
 The area is part of the Catatumbo River basin and elevation range from 1,450 to 1,900 meters above mean sea level.
 It was declared an "Área Natural Única" (Unique Natural Area) in 1998.
The Colorado orogeny, or Colorado orogen, was an orogeny in Colorado and surrounding areas which was a part of the development of the ancestral Rockies.
 The Colorado orogeny, formerly called the Colorado province, is a >500-km-wide belt of oceanic arc rock (1.78–1.65 Ga) that extends southward into New Mexico and composes a major part of the Proterozoic provinces of southwestern United States.
 This transcontinental collisional event occurred during the Paleoproterozoic (Statherian Period).
 The Wyoming sector of the Colorado orogeny was formerly called the Medicine Bow orogeny.
 The eastern sector extends into the High Plains and is called the Central Plains orogeny.
 The boundary between the Colorado orogeny and the Wyoming craton is the Cheyenne belt, a 5-km-wide mylonitic shear zone that verges northward.
 The Cheyenne belt transects and cuts off the south edge of the older Trans-Hudson orogeny.
The Vikos–Aoös National Park (Greek: Εθνικός Δρυμός Βίκου–Αώου "Ethnikós Drymós Víkou–Aóou") is a national park in the region of Epirus in northwestern Greece.
 The park, founded in 1973, is one of ten national parks in mainland Greece and is located 30 km north of the city of Ioannina in the northern part of the Pindus mountain range.
 It is named after the two major gorges of the area and encompasses 12600 ha of mountainous terrain, with numerous rivers, lakes, caves, deep canyons, dense coniferous and deciduous forest.
 The park is part of the Natura 2000 ecological network and one of UNESCO Geoparks and spans an elevation range from 550 to .
 Over 100,000 people visit the park each year and take part in activities including rafting, canoe-kayaking, hiking and mountain biking.
The Nevadan orogeny occurred along the western margin of North America during the Middle Jurassic to Early Cretaceous time which is approximately from 155 Ma to 145 Ma.
 Throughout the duration of this orogeny there were at least two different kinds of orogenic processes occurring.
 During the early stages of orogenesis an "Andean type" continental magmatic arc developed due to subduction of an oceanic plate beneath the North American Plate.
 The latter stages of orogenesis, in contrast, saw multiple oceanic arc terranes accreted onto the western margin of North America in a "Cordilleran type" accretionary orogen.
 Deformation related to the accretion of these volcanic arc terranes is mostly limited to the western regions of the resulting mountain ranges (Klamath Mountain range and Sierra Nevada Mountains) and is absent from the eastern regions.
 In addition, the deformation experienced in these mountain ranges is mostly due to the Nevadan orogeny and not other external events such as the more recent Sevier and Laramide Orogenies.
 It is noted that the Klamath Mountains and the Sierra Nevada mountains share similar stratigraphy indicating that they were both formed by the Nevadan orogeny.
 In comparison with other orogenic events, it appears that the Nevadan Orogeny occurred rather quickly taking only about 10 million years as compared to hundreds of millions of years for other orogenies around the World (ex.
 Trans-Hudson orogeny).
Swall Meadows is a census-designated place in southern Mono County, California.
 The community is residential, including second homes and a volunteer fire department, but no commercial development.
 Geographically, it sits partway up the Sherwin Grade below the Wheeler Crest of the eastern Sierra Nevada mountains, at an elevation range of approximately 6000 to .
 It is in pinon-juniper/subalpine zone habitat, with views south along the Sierra Crest, of Mt. Tom, and east across Owens Valley to the White Mountains toward Nevada (image, below).
 It is accessed from "old 395", or Lower Rock Creek Rd.
 Swall Meadows is located approximately 20 mi north of Bishop and 25 mi south of Mammoth Lakes (by highway distance).
 It is also well known in the area as an important deer migration route for the Round Valley Mule Deer population, which cherish the grazing in the meadow and apple falls from the old orchard trees.
 ZIP Code is 93514.
 The community is inside area code 760.
 The population was 220 as of the 2010 census.
Sourdough Glacier is in the Wind River Range, Bridger-Teton National Forest in the U.S. state of Wyoming.
 Sourdough Glacier is in the Bridger Wilderness, and is part of the largest grouping of glaciers in the American Rocky Mountains.
 The glacier extends from the north slope of Klondike Peak at an elevation range of 12800 to and flows into a proglacial lake.
The Algoman orogeny, known as the Kenoran orogeny in Canada, was an episode of mountain-building (orogeny) during the Late Archean Eon that involved repeated episodes of continental collisions, compressions and subductions.
 The Superior province and the Minnesota River Valley terrane collided about 2,700 to 2,500 million years ago.
 The collision folded the Earth's crust and produced enough heat and pressure to metamorphose the rock.
 Blocks were added to the Superior province along a 1200 km boundary that stretches from present-day eastern South Dakota into the Lake Huron area.
 The Algoman orogeny brought the Archaen Eon to a close, about ; it lasted less than 100 million years and marks a major change in the development of the earth’s crust.
The High Plains are a subregion of the Great Plains mostly in the Western United States, but also partly in the Midwest states of Nebraska, Kansas, and South Dakota, generally encompassing the western part of the Great Plains before the region reaches the Rocky Mountains.
 The High Plains are located in southeastern Wyoming, southwestern South Dakota, western Nebraska, eastern Colorado, western Kansas, eastern New Mexico, western Oklahoma, and south of the Texas Panhandle.
 The southern region of the Western High Plains ecology region contains the geological formation known as Llano Estacado which can be seen from a short distance or from on satellite maps.
 From east to west, the High Plains rise in elevation from around 1160 ft to over 7800 ft .
The Sierra Nevada lower montane forest is a plant community along a strip along the western and eastern edges of the Sierra Nevada mountain range in California.
 This zone is also known as a yellow pine forest.
 Its elevation range at the northern end is from 1200 - , at the southern end from 2500 - , and 3000-7000ft for the central Sierra.
The East European Platform or Russian Platform is a large and flat area covered by sediments in Eastern Europe spanning from the Ural Mountains to the Tornquist Zone and from the Peri-Caspian Basin to the Barents Sea.
 Over geological time the platform area has experienced extension, inversion and compression.
 It has an area of about 6 million km.
 The East European Platform sediments can be classified into the following groups: a "protoplatform" of metamorphosed sediments at the bottom, a "quasiplatform" of slightly deformed sediments, a "cataplatform", and a "orthoplatform" at the top.
 The Mesoproterozoic Jotnian sediments of the Baltic area are examples of a "quasiplatform".
 The oldest preserved continuous sedimentary cover in the platform date to the Vendian about 650 million years ago.
 The cycles of deposition of platform sediments are related to the development of nearby orogenies like the Timanide orogeny, the Uralian orogeny, the Hercynian orogeny and the Caledonian orogeny.