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'''The Ozarks''' (also referred to as '''Ozark Mountain Country''', the '''Ozark Mountains''' or the '''Ozark Plateau''') are a [[Physiography|physiographic]], [[Geology|geologic]], and [[culture|cultural]] highland region of the central [[United States]]. It covers much of the [[Ordinal directions|south]] half of [[Missouri]] and an extensive portion of [[Ordinal directions|northwest]] and North central [[Arkansas]]. The region also extends westward into [[Ordinal directions|northeast]] [[Oklahoma]] and extreme [[Ordinal directions|southeast]] [[Kansas]].
'''The Ozarks''' (also referred to as '''Ozark Mountain Country''', the '''Ozark Mountains''' or the '''Ozark Plateau''') are a [[Physiography|physiographic]], [[Geology|geologic]], and [[culture|cultural]] highland region of the central [[United States]]. It covers much of the [[Ordinal directions|south]] half of [[Missouri]] and an extensive portion of [[Ordinal directions|northwest]] and North central [[Arkansas]]. The region also extends westward into [[Ordinal directions|northeast]] [[Oklahoma]] and extreme [[Ordinal directions|southeast]] [[Kansas]].
Although sometimes referred to as the Ozark Mountains, the region is actually a high and deeply [[dissected plateau]]. Geologically, the area is a broad dome around the [[Saint Francois Mountains]]. The Ozark Highlands area, covering nearly {{convert|47000|sqmi|km2|-3}}, is by far the most extensive mountainous region between the [[Appalachians]] and the [[Rocky Mountains]]. Together, the Ozarks and [[Ouachita Mountains]] form an area known as the [[U.S. Interior Highlands]], and are sometimes referred to collectively. For example, the [[ecoregion]] called [[Ozark Mountain Forests]] includes the Ouachita Mountains, although the Arkansas River valley and the Ouachitas, both south of the [[Boston Mountains]], are not usually considered part of the Ozarks.
Although sometimes referred to as the Ozark Mountains, the region is actually a high and deeply [[dissected plateau]]. Geologically, the area is a broad dome around the [[Saint Francois Mountains]]. The Ozark Highlands area, covering nearly {{convert|47000|sqmi|km2|-3}}, is by far the most extensive mountainous region between the [[Appalachians]] and the [[Rocky Mountains]]. Together, the Ozarks and [[Ouachita Mountains]] form an area known as the [[U.S. Interior Highlands]], and are sometimes referred to collectively. For example, the [[ecoregion]] called [[Ozark Mountain Forests]] includes the Ouachita Mountains, although the Arkansas River valley and the Ouachitas, both south of the [[Boston Mountains]], are not usually considered part of the Ozarks.

These are the 4 steps that created the Ozark Plateau. Step one is that long ago Arkansas formed the Southern border of a deep sea called the Ouachita Basin. The second step was when South America appoached from the south. Then South America crunched against Arkansas causing the Ouachita mountains to form, creating a plateau to the north. When South America left, it left a shallow sea where the Ouachita Basin once was, which is now called the gulf coastal plain.


==Origin of the name==
==Origin of the name==
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The [[Saint Francois Mountain Range]] rises above the Ozark Plateau and is the geological core of the highland dome. The [[igneous]] and [[volcanic]] rocks of the Saint Francois Mountains are the remains of a [[Precambrian]] mountain range. The core of the range existed as an island in the [[Paleozoic]] seas. [[Reef]] complexes occur in the sedimentary layers surrounding this ancient island. These flanking reefs were points of concentration for later [[ore]]-bearing fluids which formed the rich [[lead]]-[[zinc]] ores that have been and continue to be [[mining|mined]] in the area. The [[igneous]] and volcanic rocks extend at depth under the relatively thin veneer of Paleozoic [[sedimentary]] rocks and form the basal crust of the entire region.<ref name="Missouri Geology">A.G. Unklesbay, Jerry D. Vineyard. ''Missouri Geology — Three Billion Years of Volcanoes, Seas, Sediments, and Erosion'', University of Missouri Press, 1992. ISBN 0-8262-0836-3</ref>
The [[Saint Francois Mountain Range]] rises above the Ozark Plateau and is the geological core of the highland dome. The [[igneous]] and [[volcanic]] rocks of the Saint Francois Mountains are the remains of a [[Precambrian]] mountain range. The core of the range existed as an island in the [[Paleozoic]] seas. [[Reef]] complexes occur in the sedimentary layers surrounding this ancient island. These flanking reefs were points of concentration for later [[ore]]-bearing fluids which formed the rich [[lead]]-[[zinc]] ores that have been and continue to be [[mining|mined]] in the area. The [[igneous]] and volcanic rocks extend at depth under the relatively thin veneer of Paleozoic [[sedimentary]] rocks and form the basal crust of the entire region.<ref name="Missouri Geology">A.G. Unklesbay, Jerry D. Vineyard. ''Missouri Geology — Three Billion Years of Volcanoes, Seas, Sediments, and Erosion'', University of Missouri Press, 1992. ISBN 0-8262-0836-3</ref>

The Ozark Plateau is underlain by Boone chert, a formation of limestone and flint layers that alternate. These are eroded and form steep hills, valleys and bluffs. Underground drainage feeds a number of springs and caves in the plateau. Water from these springs provides well water for humans, and water for cave dwelling animals.


==Regional economy of the Ozarks==
==Regional economy of the Ozarks==
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During the New Deal-era, the Civilian Conservation Corps employed hundreds in the construction of nearly 400 fire lookouts throughout the Ozarks at 121 known sites in [http://www.firelookout.org/towers/ar/ar.htm Arkansas] and 257 in [http://www.firelookout.org/towers/mo/mo.htm Missouri]. Of those lookouts, about half remain, and many of them are in use by the [[United States Forest Service|Forest Service]].
During the New Deal-era, the Civilian Conservation Corps employed hundreds in the construction of nearly 400 fire lookouts throughout the Ozarks at 121 known sites in [http://www.firelookout.org/towers/ar/ar.htm Arkansas] and 257 in [http://www.firelookout.org/towers/mo/mo.htm Missouri]. Of those lookouts, about half remain, and many of them are in use by the [[United States Forest Service|Forest Service]].

In 1986, Congress established the Ozark Plateau National Wildlife Refuge. It was to conserve some of the region's biological recoures.The refuge is trying to ensure the recovery of endangered and threatend species including the Ozark big-eared bat, Indiana bat, Ozark cavefish, eastern small-footed bat, southeastern bat, southeastern big-eared bat, longnose darter, Ozark cave crayfish, Bowman's cave amphipod, Ozark cave amphipod, bat cave isopod, and Ozark chinquapin. Many other endangered species have recovered immensely thanks to the refuge. In addition to cave-dwelling species, the refuge protects a number of other valuable Ozark resources like habitats for about 200 species of migratory birds, as well as geogical, archeological, historical, and paleontological resouces that provide rich scientific and educational opportunities.


===Growth industries===
===Growth industries===

Revision as of 21:32, 12 January 2009

"Ozark" redirects here. For other uses, see Ozark (disambiguation).
The Saint Francois Mountains, viewed here from Knob Lick Mountain, are the geologic core of the Ozarks.
The Ozarks and its primary physiographic regions.
Elevation map of the Ozarks. Click to enlarge.

The Ozarks (also referred to as Ozark Mountain Country, the Ozark Mountains or the Ozark Plateau) are a physiographic, geologic, and cultural highland region of the central United States. It covers much of the south half of Missouri and an extensive portion of northwest and North central Arkansas. The region also extends westward into northeast Oklahoma and extreme southeast Kansas. Although sometimes referred to as the Ozark Mountains, the region is actually a high and deeply dissected plateau. Geologically, the area is a broad dome around the Saint Francois Mountains. The Ozark Highlands area, covering nearly 47,000 square miles (122,000 km2), is by far the most extensive mountainous region between the Appalachians and the Rocky Mountains. Together, the Ozarks and Ouachita Mountains form an area known as the U.S. Interior Highlands, and are sometimes referred to collectively. For example, the ecoregion called Ozark Mountain Forests includes the Ouachita Mountains, although the Arkansas River valley and the Ouachitas, both south of the Boston Mountains, are not usually considered part of the Ozarks.

These are the 4 steps that created the Ozark Plateau. Step one is that long ago Arkansas formed the Southern border of a deep sea called the Ouachita Basin. The second step was when South America appoached from the south. Then South America crunched against Arkansas causing the Ouachita mountains to form, creating a plateau to the north. When South America left, it left a shallow sea where the Ouachita Basin once was, which is now called the gulf coastal plain.

Origin of the name

Etymology of the name is a subject of speculation.

"Ozarks" is a toponym believed to be derived as a linguistic corruption of the French abbreviation "aux Arks" (short for aux Arkansas, or "toward Arkansas" in English)[1] in the decades prior to the French and Indian War, aux Arkansas originally referring to the trading post at Arkansas Post, located in wooded Arkansas Delta lowland area above the confluence of the White River into the Mississippi River.[2][3][4] "Arkansas" seems to be the French version of what the Illinois tribe (further up the Mississippi) called the Quapaw, who lived in eastern Arkansas in the area of the trading post. Eventually, the term came to refer to all Ozark Plateau drainage into the Arkansas and Missouri Rivers.

Other possible derivations include "aux arcs" meaning "toward the arches"[5] in reference to the dozens of natural bridges formed by erosion and collapsed caves in the Ozark region. These include Clifty Hollow Natural Bridge (actually a series of arches) in Missouri,[6] and Alum Cove in the Ozark-St. Francis National Forest. It is even suggested "aux arcs" is an abbreviation of "aux arcs-en-ciel", French for "toward the rainbows" which are a common sight in the mountainous regions. After the Louisiana Purchase, American travelers in the region referred to various features of the upland areas using the term "Ozark", such as "Ozark Mountains" and "Ozark forests." By the early 20th century, "The Ozarks" had become a generic term.[7][8]

Geographic subdivisions

The Ozarks consist of four primary physiographic sections—the Springfield Plateau, the Salem Plateau, the Saint Francois Mountains, and the Boston Mountains. Topography is mostly gently rolling, except in the Boston Mountains, along the escarpments separating the Springfield and Salem Plateaus, and the Saint Francois Range where it is rugged. Karst features such as springs, losing streams, sinkholes, and caves are common in the limestones of the Springfield Plateau and abundant in the dolostone bedrock of the Salem Plateau and Boston Mountains.[9] Missouri is known as "The Cave State" with over 6000 recorded caves (second to Tennessee); the majority of these caves are found in the Ozark counties.[9][10] The Ozark Plateaus aquifer system affects groundwater movement in all areas except the igneous core of the St. Francois Mountains.[11][12][13][14] Geographic features unique to the Ozarks, particularly in Missouri, include limestone and dolomite glades—grasses and forbs in shallow soil on exposed bedrock in sloping, otherwise heavily forested areas.[15][16]

The Boston Mountains are the highest section of the Ozarks. Summits can reach elevations of just over 2,560 feet (780 m) with valleys 500 to 1,550 feet (472 m) deep (150 m to 450 m). Turner Ward Knob (TWK) is the highest named peak. Located in western Newton County, Arkansas, its elevation is 2,463 feet (751 m). Nearby, five unnamed peaks have elevations at or slightly above 2,560 feet (780 m).

The Saint Francois Mountain Range rises above the Ozark Plateau and is the geological core of the highland dome. The igneous and volcanic rocks of the Saint Francois Mountains are the remains of a Precambrian mountain range. The core of the range existed as an island in the Paleozoic seas. Reef complexes occur in the sedimentary layers surrounding this ancient island. These flanking reefs were points of concentration for later ore-bearing fluids which formed the rich lead-zinc ores that have been and continue to be mined in the area. The igneous and volcanic rocks extend at depth under the relatively thin veneer of Paleozoic sedimentary rocks and form the basal crust of the entire region.[17]

The Ozark Plateau is underlain by Boone chert, a formation of limestone and flint layers that alternate. These are eroded and form steep hills, valleys and bluffs. Underground drainage feeds a number of springs and caves in the plateau. Water from these springs provides well water for humans, and water for cave dwelling animals.

Regional economy of the Ozarks

Traditional economic activity

File:Sly Mill.jpg
Sly Mill, a grist and saw mill on Spring River in the Springfield Plateau, ca. 1860.

The Ozarks contain ore deposits of lead, zinc, iron, and barite. Many of these deposits have been depleted by historic mining activities, but much remains and is currently being mined in the lead belt of south-central Missouri. Historically the lead belt around the Saint Francois Mountains and the Tri-state district lead-zinc mining area around Joplin, Missouri, have been very important sources of metals. Mining practices common in the early 20th century left significant undermining and heavy metal contamination in topsoil and groundwater in the Tri-state district.[18][19]

Much of the area supports beef cattle ranching, and dairy farming is common across the area. Dairy farms are usually cooperative affairs, with small farms selling to a corporate wholesaler who packages product under a common brand for retail sales. Oil exploration and extraction also takes place in the Oklahoma portion of the Ozarks, as well as in the east half of the Boston Mountains in Arkansas. Logging of both softwood and hardwood timber species on both private land and in the National Forests has long been an important economic activity.

The majority of the Ozarks is forested; oak-hickory is the predominant type; cedars are common, with stands of pine often seen in the southern range. Less than a quarter of the region has been cleared for pasture and cropland.[20] Forests that were heavily logged during the early to mid-20th century have recovered. However, deforestation contributed through erosion to increased gravel bars along Ozark waterways in logged areas; stream channels have become wider and shallower and deepwater fish habitat has been lost.[13]

The numerous rivers and streams of the region saw hundreds of water powered timber and grist mills.[21] Mills were important centers of culture and commerce; dispersed widely throughout the region, mills served local needs, often thriving within a few miles of another facility. Few Ozark mills relied on inefficient water wheels for power; most utilized a dam, millrace, and water driven turbine.[22]

During the New Deal-era, the Civilian Conservation Corps employed hundreds in the construction of nearly 400 fire lookouts throughout the Ozarks at 121 known sites in Arkansas and 257 in Missouri. Of those lookouts, about half remain, and many of them are in use by the Forest Service.

In 1986, Congress established the Ozark Plateau National Wildlife Refuge. It was to conserve some of the region's biological recoures.The refuge is trying to ensure the recovery of endangered and threatend species including the Ozark big-eared bat, Indiana bat, Ozark cavefish, eastern small-footed bat, southeastern bat, southeastern big-eared bat, longnose darter, Ozark cave crayfish, Bowman's cave amphipod, Ozark cave amphipod, bat cave isopod, and Ozark chinquapin. Many other endangered species have recovered immensely thanks to the refuge. In addition to cave-dwelling species, the refuge protects a number of other valuable Ozark resources like habitats for about 200 species of migratory birds, as well as geogical, archeological, historical, and paleontological resouces that provide rich scientific and educational opportunities.

Growth industries

Big Spring in the Missouri Ozarks is one of the largest in the United States, discharging 276 million gallons of water per day into the Current River.

Tourism is the growth industry of the Ozarks as evidenced by the growth of the Branson, Missouri, entertainment center. The Corps of Engineers lakes that were created by damming the White River beginning in 1911 with Lake Taneycomo have provided a large tourist, boating and fishing economy along the Missouri-Arkansas border. All told, six lakes were created by the construction of dams in the White River basin from 1911 through 1960. White River lakes include Lake Sequoyah,[23] a small recreational fishing lake east of Fayetteville, Arkansas, formed in 1961; Sequoyah is the uppermost impoundment on the White River. Below Sequoyah (northeast of Fayetteville) is Beaver Lake, formed in 1960. The White River continues its northeasterly flow into Table Rock Lake (1958) in Missouri, which feeds directly into Taneycomo, where the river now zigzags southeasterly again into Arkansas forming Bull Shoals Lake along the Arkansas-Missouri line. Completed in 1952, Bull Shoals is the furthest downstream lake on the White River proper. Lake Norfork formed by damming the North Fork River, a tributary of the White River, in 1941.

The Lake of the Ozarks, Pomme de Terre Lake, and Truman Lake in the northern Ozarks were formed by damming the Osage River and its tributary the Pomme de Terre River in 1931, 1961 and 1979 respectively. Grand Lake in Northeast Oklahoma was built in 1940. Stockton Lake was formed by damming the Sac River near the city of Stockton, Missouri in 1969; via a pipeline it supplements the water supply of Springfield in nearby Greene County. Most of the dams were built with a dual prerogative of flood control and generating hydropower.

The creation of the lakes significantly altered the Ozark landscape and impacted traditional Ozark culture through displacement. Prior to the impoundments, communities, farms and mills concentrated along the river valleys and numerous streams for drinking water and power. Many farm roads, river fords and even railways were lost when the lakes came, disrupting rural travel and commerce. Prior to damming, the White and Osage River basins were similar to the current conditions of the Buffalo, Elk, Current, and Eleven Point Rivers.

The Buffalo National River was created by an Act of Congress in 1972 as the Nation's first National River administered by the National Park Service. In Missouri, the Ozark National Scenic Riverways,[24] was established in 1964 along the Current and Jacks Fork River; while not officially a "national river," it is the first US national park based on a river system. The Eleven Point River is included in the National Wild and Scenic Riverways System. These river parks annually draw a combined 1.5 million recreational tourists to the least populated counties in Arkansas and Missouri.

Missouri Ozark rivers include the Gasconade, Big Piney and Niangua Rivers in the north central region. The Meramac River and its tributaries Huzzah and Courtois Creeks are found in the northeastern Ozarks. The Black and St. Francis Rivers mark the eastern crescent of the Ozarks. The James, Spring, and North Fork Rivers are in south central Missouri. Forming the West central border of the Ozarks from Missouri through Kansas and into Oklahoma are Spring River and its tributary Center Creek. Grand Falls, Missouri's largest natural waterfall, a chert outcropping, includes bluffs and glades on Shoal Creek south of Joplin. All these river systems see heavy recreational use in season, including the Elk River in Southwest Missouri and its tributary Big Sugar Creek.

Big Sugar Creek in Southwest Missouri.

Ozark rivers and streams are typically clear water, with baseflows sustained by many seeps and springs, and flow through forests along limestone bluffs. Gravel bars are common along shallow banks, while deep holes are found along bluffs.[25] Except during periods of heavy rain or snowmelt – when water levels rise quite rapidly – their level of difficulty is suitable for most canoeing and tubing.

Fish hatcheries are common due to the abundance of springs and waterways. The Neosho National Fish Hatchery was built in 1888; it was the first Federal hatchery. The Missouri Department of Conservation operates numerous warm and cold water hatcheries and trout parks;[26] private hatcheries such as Rockbridge[27] are common.

In addition to tourism, poultry farming and food processing are significant industries throughout the region. The Tyson Foods corporation and ConAgra Foods each operates numerous poultry farms and processing plants throughout the Ozarks. Schreiber Foods, the largest privately held cheese company in the world, sees operations throughout southern Missouri. Stillwell foods has frozen vegetable and other food processing centers in eastern Oklahoma. Commercial farms and processing operations are known to raise levels of chemical and biological contaminants in Ozark streams, threatening water supplies and endangered native species.[28][29][30][31]

The trucking industry is important to the regional economy with national carriers based there including J. B. Hunt and Prime, Inc. Springfield remains an operational hub for BNSF Railway. Logging and timber industries are also significant in the Ozark economy with operations ranging from small family run sawmills to large commercial concerns. Fortune 500 companies such as Wal-Mart and Leggett & Platt were founded and are based in the Ozarks.

Ozark culture

Ozark also refers to a region of people with a distinct culture, architecture, and dialect shared by the people who live on the plateau. Traditional Ozark culture is a mixture of cultures similar to Appalachia and the Upland South. Early settlers in Missouri were American, followed in the 1840s and 1850s by Irish and German immigrants. Much of the Ozark population is of German and Scots-Irish descent, often including some Native American ancestry, and Ozark families tend to have lived in the area since the 19th century.[32]

Wild strawberries
Persimmon flower

Homesteads in rural areas tend to be isolated instead of being clustered into villages. Early settlers relied on hunting, fishing and trapping, as well as foraging to supplement their diets and incomes. Today hunting and fishing for recreation are common activities and an important part of the tourist industry. Foraging for mushrooms, especially morels and puffballs, and for medicinal native plant species, including St. John's Wort and ginseng, is common, and is financially supported by established buyers in the area. Other forages include poke, watercress, persimmons, and pawpaw; wild berries such as blackberry, raspberry, mulberry, wild cherry, wild strawberry, and dewberry; and wild nuts such as black walnut and even acorns.[33] Edible native legumes, wild grasses and wildflowers are plentiful, and beekeeping is common.

Ozark culture is widely referenced in print and broadcast media. Where the Red Fern Grows, the Shepherd of the Hills and As a Friend[34] are books set in the Ozarks. The 1999 film Ride with the Devil, based on the book Woe to Live On,[35] is set in Southwest Missouri during the Civil War. Several early and influential country music television and radio programs originated from Springfield in the 1950s and 60s, including ABC-TV's Ozark Jubilee and The Slim Wilson Show on KYTV. The shows featured many Ozark musicians including Porter Wagoner and old-time fiddler Bob Holt.[36] Examples of commercial interpretations of traditional Ozark culture include the two major family theme parks in the region, Silver Dollar City and the now defunct Dogpatch U.S.A., and the resort entertainment complex in Branson.

Traditional Ozark culture includes stories and tunes passed orally between generations through community music parties and other informal gatherings. Square dances were an important social avenue throughout the Ozarks into the 20th century. Square dances sprung up wherever people concentrated around mills and timber camps, and in geographically isolated communities; many of these saw their own local dance tunes and variations develop. Of all the traditional musicians in the Ozarks, the fiddler holds a distinct place in both the community and folklore. Community fiddlers revered for carrying local tunes; regionally, traveling fiddlers brought new tunes and entertainment, even while many viewed their arrival as a threat to morality.[36][37]

Boston Mountains in the Arkansas Ozarks.

Historians such as Vance Randolph collected Ozark folklore and lyrics in volumes such as the national bestseller Pissing in the Snow and Other Ozark Folktales (University of Illinois Press, 1976), and Ozark Folksongs (University of Missouri Press, 1980), a four-volume anthology of regional songs and ballads.[38] Ozark anecdotes from the oral tradition are bawdy more often than not, full of wild embellishments on everyday themes.

Population influx since the 1950s, coupled with proximity to the Midwest, the Mississippi embayment, and the Plains, contributes to changing cultural values in the Ozarks. Theme parks and theatres seen to reflect regional values have little in common with traditional Ozark culture. Community tradition bearers remain active, in decreasing numbers, far afield of commercial offers.[39][40]

Religion

Ozark religion, like that of Appalachia, was predominantly Baptist and Methodist during periods of early settlement; it tends to be conservative, or individualistic, with Anglicans, Assemblies of God, Baptists including Southern Baptists, Catholics, Church of Christ, and other Protestant Pentecostal denominations present.[41][42] Religious organizations headquartered in the Ozarks include the Assemblies of God and the Baptist Bible Fellowship International in Springfield, and the Pentecostal Church of God in Joplin. The 1960s and 70s saw back-to-the-land farms and communes established in rural counties. The Ozarks are also home to some sects unique to the area.

See also

References

  1. ^ Stewart, George R. (1967). Names on the Land: A Historical Account of Place-Naming in the United States, p. 137. Houghton Mifflin, Boston.
  2. ^ Randolph, Vance. The Ozarks: An American Survival of Primitive Society. New York: The Vanguard Press, p. 14. 1931.
  3. ^ Arnold, Morris S. Unequal Laws Unto a Savage Race: European Legal Traditions in Arkansas, 1686-1836. University of Arkansas Press, Fayetteville. 1985.
  4. ^ Arnold, Morris S. Colonial Arkansas 1686-1804: A Social and Cultural History. University of Arkansas Press, Fayetteville. 1991.
  5. ^ E. Joan Wilson Miller. The naming of the land in the Arkansas Ozarks: A study in culture processes. Abstract Annals of the Association of American Geographers, 59 (2), 240–251. 1969.
  6. ^ Watkins, Conor. Ozarks geology: Clifty Creek Natural Area includes natural bridge, The Ozarks Chronicle, Rolla, Mo.
  7. ^ Morrow, Lynn (1996). "Ozark/Ozarks: Establishing a Regional Term". White River Valley Historical Quarterly. 36 (2). Retrieved 2006-09-08.
  8. ^ McMillen, Margot Ford. A to Z Missouri: The Dictionary of Missouri Place Names, Columbia, Missouri: Pebble Publishing, 1996. ISBN 0-9646625-4-X
  9. ^ a b Karst, Springs and Caves in Missouri, Missouri Department of Natural Resources
  10. ^ Scott House (2005-05-14). "Fact Sheet on 6000 Caves". The Missouri Speleological Survey, Inc. Retrieved 2008-03-16. {{cite web}}: Check date values in: |date= (help)
  11. ^ Ozark Aquifer Map, United States Geological Survey.
  12. ^ Rafferty, Milton.The Ozarks as a Region: A Geographer's Description, OzarksWatch, Vol. I, No. 4, Spring 1988.
  13. ^ a b Project Tour - A quick visit to the Ozarks Stream Geomorphology Project, United States Geological Survey.
  14. ^ Ground Water Atlas of the United States: Kansas, Missouri, and Nebraska. United States Geological Survey
  15. ^ Spatial Interaction Webs in Ozark Glades. John Chase, Assistant Professor. Washington University in St. Louis.
  16. ^ Ware, Stewart. Rock Outcrop Plant Communities (Glades) in the Ozarks: A Synthesis, Abstract. The Southwestern Naturalist, Vol. 47, No. 4 (Dec., 2002), pp. 585-597.
  17. ^ A.G. Unklesbay, Jerry D. Vineyard. Missouri Geology — Three Billion Years of Volcanoes, Seas, Sediments, and Erosion, University of Missouri Press, 1992. ISBN 0-8262-0836-3
  18. ^ Lasmanis, Raymond. Tri-State and Viburnum Trend Districts, Rocks & Minerals, 11/1/1997.
  19. ^ GeoKansas: Lead and Zinc Mining, Kansas Geological Survey. Updated May 5, 2005.
  20. ^ Primary Distinguishing Characteristics of Level III Ecoregions of the Continental United States, U.S. Environmental Protection Agency. Revised April 2000.
  21. ^ Index to the old mills of Missouri. Hosted by rootsweb, this incomplete list includes almost 250 old mills in Missouri alone.
  22. ^ Suggs, George E., Jr. Water Mills of the Missouri Ozarks. University of Oklahoma Press: Norman, OK. 1990
  23. ^ Boss, Stephen K., Heil-Chapdelaine, Vanessa M. Mapping Landscape Change: An Historic and Bathymetric Study of Lake Sequoyah, Washington County, Arkansas
  24. ^ http://www.nps.gov/ozar Ozark National Scenic Riverways
  25. ^ MS Panfil, RB Jacobson. Hydraulic Modeling of In-channel Habitats in the Ozark Highlands of Missouri: Assessment of Physical Habitat Sensitivity to Environmental Change. USGS-Biological Resources Division.
  26. ^ http://mdc.mo.gov/areas/hatchery/ Missouri Fish Hatcheries and Trout Parks
  27. ^ http://www.watersheds.org/outdoors/recreation.htm Rockbridge
  28. ^ Endangered Species Guidesheet. Missouri Department of Conservation.
  29. ^ Research Project: Poultry Manure Management To Reduce Non-Point Source Phosphorus Pollution. United States Department of Agriculture: Agricultural Research Service.
  30. ^ B. E. Haggard, P. A. Moore, Jr, I. Chaubey and E. H. Stanley. Nitrogen and Phosphorus Concentrations and Export from an Ozark Plateau Catchment in the United States: Abstract. Biosystems Engineering, Volume 86, Issue 1, September 2003, Pages 75-85.
  31. ^ Missouri Water Quality Report: 2006. Missouri Department of Natural Resources: Water Protection Program. April 1, 2007.
  32. ^ Rafferty, Milton D. The Ozarks: Land and Life, University of Arkansas Press, 2nd ed., 2001. ISBN 1-55728-714-7
  33. ^ Phillips, Jan. Wild Edibles of Missouri. Missouri Department of Conservation, 2nd edition (1998). Cover, Introduction, Acknowledgments; Color Plates.
  34. ^ Gander, Forrest. As a Friend. New York, NY: New Directions Publishing Corporation. 2008.
  35. ^ Woodrell, Daniel. Woe to Live On. Henry Holt, 1987.
  36. ^ a b Henigan, Julie. Play Me Something Quick and Devilish: Bob Holt - Old-Time Square Dance Fiddler, Musical Traditions, Article MT021, June 1998.
  37. ^ Edited and photography by Allen Gage. Old-Time Fiddling: A Traditional Folk Art With Four Ozark Musicians, Bittersweet, Volume IX, No. 3, Spring 1982.
  38. ^ Smith, Vic. Review of Ozark Folksongs, Musical Traditions, January 2001.
  39. ^ Jam Sessions in Southwest Missouri. Missouri State University Libraries.
  40. ^ Bob Holt: Fiddler from the Missouri Ozarks. Local Legacies project of the Library of Congress.
  41. ^ http://www.thearda.com/mapsReports/reports/state/05_2000.asp
  42. ^ http://www.thearda.com/mapsReports/reports/state/29_2000.asp


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