How Many Miles To Tennessee

Overview of the geography of the U.Southward. state of Tennessee

The U.S. state of Tennessee is geographically various, with varying terrains and several distinct physiographic regions. Its landforms range from the Blue Ridge Mountains in the eastern part of the state to flat and fertile plains along the Mississippi River. The land is geographically, legally, culturally, and economically divided into 3 Grand Divisions: East Tennessee, Middle Tennessee, and Due west Tennessee.

Overview [edit]

Tennessee is in the Southeastern United States. Most of the state is considered part of the Upland South, and the eastern third is part of Appalachia.^[1] Tennessee covers roughly 42,143 square miles (109,150 kmⁱⁱ), of which 926 foursquare miles (2,400 km²), or 2.2%, is water. It is the 16th smallest state in terms of state area. The state is nearly 440 miles (710 km) long from east to west and 112 miles (180 km) wide from north to south. Tennessee is geographically, culturally, economically, and legally divided into iii Grand Divisions: Due east Tennessee, Center Tennessee, and West Tennessee. As culturally and historically distinct regions, the 1000 Divisions are sometimes called "The 3 Tennessees". Tennessee borders eight other states: Kentucky and Virginia to the north, N Carolina to the east, Georgia, Alabama, and Mississippi on the south, and Arkansas and Missouri on the west. It is tied with Missouri as the country bordering the almost other states. Information technology is trisected by the Tennessee River, and its geographical heart is in Murfreesboro, the state's sixth-largest city. The purlieus between Eastern and Central Time passes across the Cumberland Plateau through the state.^[2]

Borders [edit]

Tennessee's eastern boundary roughly follows the highest crests of the Blue Ridge Mountains, and the Mississippi River forms its western boundary.^[three] Due to flooding of the Mississippi River that has inverse its path, the state'due south western boundary deviates from the river in some places.^[4] Neither the northern nor the southern edge of Tennessee follows a geographic feature. The northern border was originally defined as the parallel 36°30′ due north and the Regal Colonial Boundary of 1665, but due to faulty surveys, the border begins n of this line in the eastward, and to the due west, gradually veers north with multiple minute shifts.^[three] Once at the Tennessee River in the western function of the land, the edge shifts s onto the actual 36°30′ parallel.^[5] An 1818 survey erroneously placed the state'due south southern border 1 mile (1.6 km) south of the 35th parallel; Georgia legislators continue to dispute this placement, as it prevents Georgia from accessing the Tennessee River.^[vi]

Topography [edit]

Marked by a multifariousness of landforms and topographies, Tennessee features half dozen principal physiographic provinces, from east to westward, which are function of three larger regions: the Blue Ridge Mountains, the Ridge-and-Valley Appalachians, and the Cumberland Plateau, function of the Appalachian Mountains; the Highland Rim and Nashville Bowl, role of the Interior Low Plateaus of the Interior Plains; and the East Gulf Coastal Plain, role of the Atlantic Plains.^{[seven] [viii]} Minor regions include the southern tip of the Cumberland Mountains, the Western Tennessee Valley, and the Mississippi Alluvial Plain. The land's highest point is Clingmans Dome, at vi,643 feet (2,025 k) above sea level.^[ix] Clingmans Dome is the highest point on the Appalachian Trail and the tertiary-highest peak in the U.s.a. eastward of the Mississippi River. The state's everyman point, 178 feet (54 g), is on the Mississippi River at the Mississippi state line in Memphis.^[10] Tennessee is home to the most caves in the United States, with more than 10,000 documented.^[11]

Blue Ridge Mountains [edit]

The western Blue Ridge Mountains lie within Tennessee's eastern edge. This range is characterized by towering mountains and jumbled terrains, and is divided into several subranges, namely the Great Smoky Mountains, the Bald Mountains, the Unicoi Mountains, the Unaka Mountains, and the Iron Mountains. The average meridian of the Bluish Ridge Mountains in Tennessee is 5,000 feet (1,500 one thousand) above bounding main level. The land'due south border with Due north Carolina roughly follows the highest peaks of this range, including Clingmans Dome, the state'south highest point. The Blue Ridge area was never more than than sparsely populated, and today most of it is protected by the Cherokee National Forest, the Swell Smoky Mountains National Park, and several federal wilderness areas and country parks.^{[ citation needed ]}

Ridge-and-Valley Appalachians [edit]

Stretching west from the Bluish Ridge Mountains for virtually 55 miles (89 km) are the Ridge-and-Valley Appalachians, also known as the Tennessee Valley^[a] or Great Valley of East Tennessee. This area of Tennessee consists of numerous linear parallel ridges and valleys that tendency northeast to southwest, the general management of the entire Appalachian range.^[12] Nigh of these ridges are low, but some of the higher ones are normally called mountains.^[12] Nearly of this province is coterminous with the Great Appalachian Valley, where the valleys become broader and the ridges lower. In this region are numerous towns and three of the state'south urban areas: Knoxville and Chattanooga, the country'due south third and quaternary-largest cities, respectively; and the Tri-Cities: Bristol, Johnson City, and Kingsport. Numerous tributaries join to form the Tennessee River in the Ridge and Valley Region.^{[ commendation needed ]}

Cumberland Plateau and Cumberland Mountains [edit]

Fall Creek Falls, the tallest waterfall in the eastern U.s., is located on the Cumberland Plateau

The Cumberland Plateau rises to the west of the Tennessee Valley. This landform is part of the larger Appalachian Plateau, and is more often than not covered by flat-topped tablelands.^[13] The elevation of the Cumberland Plateau ranges from about one,500 to 2,500 anxiety (460 to 760 m) above sea level, with an average tiptop of approximately 2,000 feet (610 m). The eastern part of the plateau is, on average, higher than the western office, and most of the h2o on the Plateau drains to the west into the Cumberland River. The plateau's eastern edge is relatively distinct, but the western escarpment is irregular, with several long, crooked stream valleys separated by rocky cliffs that run into the interior of the plateau and contain numerous waterfalls.^[14] The Cumberland Mountains, with peaks above 3,500 feet (one,100 m), comprise the northeastern function of the Appalachian Plateau in Tennessee, and the southeastern part of the Cumberland Plateau is divided past the largely undeviating Sequatchie Valley.^[14] The boundary between East and Heart Tennessee straddles the top of the Cumberland Plateau, as does the boundary betwixt Eastern and Primal Time.^{[ citation needed ]}

Highland Rim and Nashville Basin [edit]

West of the Cumberland Plateau is the Highland Rim, an elevated plain that surrounds the Nashville Basin.^[15] Both of these physiographic provinces are office of the Interior Low Plateaus of the larger Interior Plains. The Highland Rim is Tennessee's largest geographic region, and is often divided into the Eastern and Western Highland Rim.^[16] The Eastern Highland Rim is characterized by relatively level plains dotted by rolling hills, and averages well-nigh one,000 feet (300 m) above sea level.^[17] The Western Highland Rim and western parts of the Nashville Basin are covered by a mix of uneven rounded knobs with steep ravines and meandering streams in between.^[eighteen] Elevations in the Western Highland Rim range from approximately 900 feet (270 m) along the eastern edge to 700 anxiety (210 g) at the western escarpment.

Much of the Nashville bowl is relatively level, and supports rich, fertile farmland and a great diversity of natural wildlife.^{[19] [20]} It averages about 600 feet (180 one thousand) in a higher place sea level, although elevations vary greatly, with some hills reaching college than the Eastern Highland Rim. Porous limestone bedrock underlies the Nashville Basin and much of the Eastern Highland Rim very close to the surface. These areas form karst, containing many caves, sinkholes, depressions, and surreptitious streams.^[17] Nashville is in the northwestern corner of the Basin, and virtually of its suburbs radiate outward to the south, southeast, and east, owing to its geography. Clarksville, the state's fifth largest metropolis, sits in the northwestern Highland Rim.^{[ citation needed ]}

To the west of the Highland Rim is a narrow region known as the Western Tennessee Valley, which consists of nearly 10 miles (16 km) in width of hilly land that runs along the banks of the Tennessee River.^[21] The Tennessee River forms the boundary between Middle and West Tennessee here. Most geographers exercise not include this region every bit a major physiographic province of Tennessee. Some maps place the portion of this region w of the Tennessee River as part of the Gulf Littoral Plainly; however this is inaccurate, as it is non part of the drainage basin of the Mississippi River.

Gulf Coastal Obviously and Mississippi embayment [edit]

West of the Tennessee River is the Gulf Coastal Plain, a broad expanse that begins at the Gulf of Mexico and extends northward into southern Illinois, gradually losing tiptop west.^[22] In Tennessee, this plain consists of 2 distinct sections.^{[b] [23]} From the due east, the plain begins with depression rolling hills and wide stream valleys, known as the West Tennessee Highlands, or Uplands, and gradually levels out to the west.^[23] The flat western function of the patently contains extremely fertile soils, and is one of the near productive cotton producing regions in the country. These parts likewise contain thick and fertile loess, and stop at steep bluffs overlooking the Mississippi embayment. This is the westernmost physiographic sectionalisation of Tennessee, and is part of the larger Mississippi Alluvial Patently.^[24] This flat strip, commonly known as the Mississippi Bottoms, ranges from 10 to 14 miles (16 to 23 km) broad, and has an meridian of less than 300 feet (91 m).^[25] Information technology consists of lowlands, floodplains, and swamplands, and is sometimes considered role of the Mississippi Delta region.^[25] Memphis is in the southwestern corner of the Gulf Coastal Plain, and is W Tennessee's well-nigh populous metropolis. All of West Tennessee is part of the Jackson Purchase historical region, and it is the least populated of the state's Grand Divisions.^{[ citation needed ]}

Geology [edit]

Geological formations in Tennessee largely correspond with the state's topographic features, and, in full general, subtract in age from e to west. About of the Bluish Ridge Mountains in the e were formed during the Precambrian era, and contain the state's oldest rocks, igneous strata that is more than 1 billion years old.^{[26] [27]} Most of the southern Blue Ridge Mountains are composed of Precambrian granite and sedimentary rocks, and Cambrian strata that have been altered past metamorphism.^[27] Nearly of the formations in Eastward and Middle Tennessee consist of strata deposited during the Paleozoic era. Shale and carbonate rocks that formed during the Ordovician catamenia are plant in the Nashville Bowl, Ridge-and-Valley region, and the Sequatchie Valley.^[28] The inner part of the Nashville Basin is a geological dome that was uplifted between 300 and 400 million years ago during the Carboniferous and Devonian periods.^[29] Devonian and Silurian strata are found in the Western Tennessee Valley and in pocket-size patches in the Western Highland Rim.^[30] The Highland Rim formed during the Mississippian era, and is underlain by soluble limestone bedrock that has formed karst, with patches of chert, shale, and sandstone.^[31] The Cumberland Plateau was formed during the Pennsylvanian period most 300 one thousand thousand years ago, and consists predominantly of sandstone, silt, and shale, with an abundance of coal.^[13] The eastern part of the Gulf Coastal Obviously is composed of Mesozoic Cretaceous;^[32] nigh of the plain to the west was deposited during the Cenozoic Tertiary era.^[33] The youngest geological formations in Tennessee are sands and silts deposited during the electric current Fourth period, and are located inside the Mississippi Alluvial Apparently and the valleys of rivers that drain into the Mississippi River.^[33]

Devonian and Silurian strata are found in the Western Tennessee Valley and in modest patches in the Western Highland Rim, formed 360 to 420 1000000 years ago.^[30] The Highland Rim formed during the Mississippian era about 350 million years ago, and is underlain by soluble limestone bedrock that has formed karst, with patches of chert, shale, and sandstone.^[31] and the Cumberland Plateau was formed during the Pennsylvanian menstruum well-nigh 300 million years ago.^[thirteen] Information technology consists predominantly of sandstone, silt, and shale, with an abundance of coal.^[thirteen] The eastern part of the Gulf Coastal Plain is equanimous of Mesozoic Cretaceous strata that appeared between 66 and 145 million years agone;^[32] virtually of the manifestly to the west was deposited during the Cenozoic Third era between 2.half-dozen and 66 one thousand thousand years ago.^[33] The youngest geological formations in Tennessee are sands and silts deposited during the current 4th menstruum in the last 2.6 million years, and are located within the Mississippi Alluvial Plain and the valleys of rivers that bleed into the Mississippi River.^[33]

Tennessee is considered seismically active and contains two major seismic zones, although destructive earthquakes rarely occur in the country.^{[34] [35]} The Eastern Tennessee Seismic Zone spans the entirety of East Tennessee from northwestern Alabama to southwestern Virginia. The region is considered one of the nearly seismically agile zones in the Southeastern Us, and often produces low-magnitude earthquakes.^[36] The New Madrid Seismic Zone is located in the northwestern part of the country. This seismic zone produced a series of devastating earthquakes between December 1811 and February 1812 that formed Reelfoot Lake most Tiptonville.^[37]

Hydrology [edit]

The state is drained past three major rivers, the Tennessee, Cumberland, and Mississippi. The Tennessee River begins at the juncture of the Holston and French Broad rivers in Knoxville, flows southwest to Chattanooga, and exits into Alabama before reemerging in the western part of the country and flowing n into Kentucky.^[38] Major tributaries of the Tennessee River include the Clinch, Trivial Tennessee, Hiwassee, Sequatchie, Elk, Beech, Buffalo, Duck, and Big Sandy rivers.^[38] The Cumberland River flows through the north-key part of the state, emerging in the northeastern Highland Rim, passing through Nashville and the northern part of the Nashville Bowl before turning northwest to Clarksville and entering Kentucky west of the Tennessee River.^[39] Its principal branches in Tennessee are the Obey, Caney Fork, Stones, Harpeth, and Reddish rivers.^[39] The Mississippi River forms the state's western boundary, where Memphis lies.^[xl] Its tributaries are the Obion, Forked Deer, Hatchie, Loosahatchie, and Wolf rivers.^[xl] The Tennessee Valley Dominance (TVA) and U.S. Army Corps of Engineers operate many hydroelectric dams on the Tennessee and Cumberland rivers and their tributaries. These dams form many large reservoirs throughout the state.^[41]

About half the state'south land area is in the Tennessee Valley drainage basin of the Tennessee River.^[38] The Cumberland River basin covers the northern half of Middle Tennessee and a small portion of East Tennessee.^[39] A small part of north-fundamental Tennessee in Sumner, Macon, and Clay Counties is in the Green River watershed.^[42] All three of these basins are tributaries of the Ohio River watershed. Most of Westward Tennessee is in the Lower Mississippi River watershed.^[xl] The entirety of the state is in the Mississippi River watershed, except for a small sliver in Bradley and Polk Counties traversed by the Conasauga River, which is part of the Mobile Bay watershed.^[43]

Ecology [edit]

Cedar glades are an extremely rare blazon of ecosystem that is found in regions of Middle Tennessee where limestone bedrock is close to the surface

Tennessee is within a temperate deciduous forest biome commonly known as the Eastern Deciduous Forest.^[44] It has 8 ecoregions: the Blueish Ridge, Ridge and Valley, Key Appalachian, Southwestern Appalachian, Interior Low Plateaus, Southeastern Plains, Mississippi Valley Loess Plains, and Mississippi Alluvial Plain regions.^[45] Due to its wide variety of terrains and ecosystems, Tennessee is the most biodiverse inland land.^[46] The Swell Smoky Mountains National Park is the most biodiverse national park,^{[47] [48]} and the state'south Duck River is the virtually biologically diverse waterway in North America.^[49] The state is domicile to 340 species of birds, 325 freshwater fish species, 89 mammals, 77 amphibians, and 61 reptiles.^[47]

Forests comprehend virtually 52% of the country's land expanse, with oak–hickory the dominant type.^[fifty] Appalachian oak–pino and cove hardwood forests are found in the Blue Ridge Mountains and Cumberland Plateau, and bottomland hardwood forests are mutual throughout the Gulf Coastal Evidently.^[51] Pine forests are also found throughout the state.^[51] Some of the concluding remaining large American chestnut copse grow in the Nashville Basin. They are existence used to help breed blight-resistant trees.^[52] Middle Tennessee is dwelling to many unusual and rare ecosystems known every bit cedar glades, which occur in areas with shallow limestone bedrock that is largely barren of overlying soil and comprise many endemic institute species.^[53]

Mutual mammals found throughout Tennessee include white-tailed deer, red and gray foxes, coyotes, raccoons, opossums, wild turkeys, rabbits, and squirrels. Black bears are found in the Blue Ridge Mountains and on the Cumberland Plateau in Eastern Tennessee. Tennessee has the third-highest number of amphibian species, and is particularly known for its salamanders, with the Great Smoky Mountains National Park dubbed the "Salamander Capital of the World".^[54] The state too ranks second in the nation for the variety of its freshwater fish species.^[55]

Climate [edit]

A map of Köppen climate types in Tennessee

Most of the state has a boiling subtropical climate, with the exception of some of the college elevations in the Appalachians, which are classified every bit having a mountain temperate or boiling continental climate due to cooler temperatures.^[56] The Gulf of Mexico is the dominant factor in the climate of Tennessee, with winds from the south being responsible for well-nigh of the state'southward annual precipitation. Generally, the state has hot summers and mild to cool winters with generous precipitation throughout the year, with highest average monthly precipitation more often than not in the winter and spring months, between December and April. The driest months, on boilerplate, are August to October. On boilerplate the land receives 50 inches (130 cm) of precipitation annually. Snow ranges from 5 inches (13 cm) in West Tennessee to over 80 inches (200 cm) in the highest mountains in East Tennessee.^{[57] [58]}

Summers in the land are generally hot and humid, with about of the state averaging a high of around ninety °F (32 °C) during the summer months. Winters tend to be mild to cool, increasing in coolness at higher elevations. Generally, for areas outside the highest mountains, the boilerplate overnight lows are near freezing for most of the state. The highest recorded temperature is 113 °F (45 °C) at Perryville on August 9, 1930, while the lowest recorded temperature is −32 °F (−36 °C) at Mountain City on Dec 30, 1917.^[59]

While the state is far plenty from the coast to avoid whatever direct affect from a hurricane, the location of the country makes it likely to exist hit by the remnants of tropical cyclones which weaken over land and tin can cause pregnant rainfall.^[sixty] The state averages about fifty days of thunderstorms per twelvemonth, some of which can exist astringent with big hail and damaging winds. Tornadoes are possible throughout the state, with West and Middle Tennessee the most vulnerable. Occasionally, potent or violent tornadoes occur, such equally the devastating April 2011 tornadoes that killed 20 people in North Georgia and Southeast Tennessee.^[61] On average, the state has 15 tornadoes per twelvemonth.^[62] Tornadoes in Tennessee can be astringent, and Tennessee leads the nation in the pct of total tornadoes which have fatalities.^[63] Wintertime storms are an occasional problem, such as the infamous Blizzard of 1993, although ice storms are a more than probable occurrence. Fog is a persistent problem in parts of the state, especially in East Tennessee.^[64]

Climate information [edit]

Monthly Normal High and Low Temperatures For Various Tennessee Cities (F)[65]
City	Jan	Feb	Mar	Apr	May	Jun	Jul	Aug	Sep	Oct	Nov	Dec
Bristol	44/25	49/27	57/34	66/41	74/51	81/sixty	85/64	84/62	79/56	68/43	58/35	48/27
Chattanooga	50/31	54/33	63/40	72/47	79/56	86/65	90/69	89/68	82/62	72/48	61/40	52/33
Knoxville	47/30	52/33	61/40	71/48	78/57	85/65	88/69	87/68	81/62	71/50	60/41	fifty/34
Memphis	l/31	55/36	63/44	72/52	80/61	89/69	92/73	92/72	86/65	75/52	62/43	52/34
Nashville	47/28	52/31	61/39	70/47	78/57	85/65	89/70	89/69	82/61	71/49	59/twoscore	49/32

Climate data for Memphis (Memphis Int'l), 1991−2020 normals,[66] extremes 1872−present[67]
Month	Jan	Feb	Mar	Apr	May	Jun	Jul	Aug	Sep	Oct	Nov	Dec	Year
Tape loftier °F (°C)	79 (26)	81 (27)	87 (31)	94 (34)	99 (37)	104 (xl)	108 (42)	107 (42)	103 (39)	98 (37)	86 (30)	81 (27)	108 (42)
Mean maximum °F (°C)	seventy (21)	73 (23)	80 (27)	85 (29)	91 (33)	96 (36)	98 (37)	99 (37)	95 (35)	88 (31)	79 (26)	71 (22)	100 (38)
Average loftier °F (°C)	fifty.9 (10.5)	55.5 (13.1)	64.ii (17.9)	73.iv (23.0)	81.seven (27.6)	89.4 (31.9)	91.9 (33.three)	91.5 (33.one)	86.0 (thirty.0)	75.ane (23.9)	62.half-dozen (17.0)	53.4 (11.ix)	73.0 (22.8)
Daily mean °F (°C)	42.one (v.6)	46.i (7.viii)	54.2 (12.3)	63.two (17.3)	72.1 (22.iii)	79.9 (26.6)	82.8 (28.two)	82.one (27.eight)	76.0 (24.4)	64.six (18.1)	52.7 (11.v)	44.eight (vii.one)	63.4 (17.4)
Average low °F (°C)	32.vi (0.3)	36.3 (2.4)	44.1 (half dozen.7)	52.nine (11.6)	62.two (16.eight)	seventy.three (21.iii)	73.eight (23.2)	72.7 (22.6)	65.2 (18.4)	53.viii (12.1)	43.7 (half-dozen.5)	35.1 (1.7)	53.vi (12.0)
Mean minimum °F (°C)	16 (−9)	21 (−six)	26 (−iii)	37 (three)	48 (9)	60 (xvi)	67 (19)	65 (18)	52 (11)	38 (3)	27 (−three)	21 (−half dozen)	14 (−10)
Record low °F (°C)	−eight (−22)	−11 (−24)	12 (−xi)	27 (−3)	36 (two)	48 (9)	52 (11)	48 (9)	36 (ii)	25 (−4)	ix (−13)	−13 (−25)	−13 (−25)
Average precipitation inches (mm)	4.fourteen (105)	iv.55 (116)	v.74 (146)	5.87 (149)	v.27 (134)	three.99 (101)	four.82 (122)	3.37 (86)	3.03 (77)	three.98 (101)	4.69 (119)	5.49 (139)	54.94 (1,395)
Average snowfall inches (cm)	0.9 (2.3)	1.0 (two.5)	0.five (1.3)	0.0 (0.0)	0.0 (0.0)	0.0 (0.0)	0.0 (0.0)	0.0 (0.0)	0.0 (0.0)	0.0 (0.0)	0.i (0.25)	0.2 (0.51)	2.7 (6.9)
Average precipitation days (≥ 0.01 in)	x.0	9.9	11.v	ix.vi	10.half-dozen	viii.9	ix.5	7.6	7.i	7.v	9.0	10.2	111.4
Average snowy days (≥ 0.one in)	i.0	0.8	0.3	0.0	0.0	0.0	0.0	0.0	0.0	0.0	0.2	0.3	2.vi
Average relative humidity (%)	68.2	66.4	63.2	62.v	66.iv	66.8	69.1	69.vi	71.3	66.ii	67.7	68.8	67.2
Mean monthly sunshine hours	166.6	173.8	215.iii	254.6	301.five	320.six	326.nine	307.0	251.2	245.ix	173.0	151.ix	2,888.3
Per centum possible sunshine	53	57	58	65	69	74	74	74	68	lxx	56	50	65
Source: NOAA (relative humidity 1961−1990, sun 1961−1987)[68] [69] [lxx] [71] [72]

v t east Climate data for Nashville (Nashville Int'fifty), 1991–2020 normals,[c] extremes 1871−present[d]
Month	Jan	Feb	Mar	Apr	May	Jun	Jul	Aug	Sep	Oct	November	Dec	Twelvemonth
Tape high °F (°C)	78 (26)	84 (29)	89 (32)	91 (33)	96 (36)	109 (43)	107 (42)	106 (41)	105 (41)	99 (37)	88 (31)	79 (26)	109 (43)
Hateful maximum °F (°C)	68.v (xx.3)	73.iii (22.9)	fourscore.i (26.vii)	85.three (29.6)	89.9 (32.2)	94.7 (34.viii)	97.1 (36.ii)	96.7 (35.9)	93.4 (34.1)	86.4 (30.2)	78.1 (25.6)	69.6 (twenty.9)	98.5 (36.9)
Average high °F (°C)	49.1 (9.5)	53.viii (12.1)	62.seven (17.1)	72.6 (22.half-dozen)	80.4 (26.9)	87.vii (thirty.9)	90.ix (32.7)	90.4 (32.4)	84.4 (29.1)	73.5 (23.i)	61.4 (16.3)	52.2 (xi.2)	71.6 (22.0)
Daily hateful °F (°C)	39.half-dozen (4.two)	43.iv (half-dozen.3)	51.5 (10.8)	lx.8 (16.0)	69.3 (20.7)	77.ane (25.ane)	80.seven (27.1)	79.vii (26.5)	73.1 (22.viii)	61.7 (16.5)	50.3 (ten.ii)	42.7 (v.9)	60.8 (xvi.0)
Average low °F (°C)	xxx.i (−1.1)	33.0 (0.6)	40.two (4.6)	48.9 (9.four)	58.3 (xiv.6)	66.4 (19.ane)	70.5 (21.4)	69.0 (xx.half-dozen)	61.8 (16.6)	49.nine (9.9)	39.2 (4.0)	33.3 (0.vii)	50.1 (10.ane)
Mean minimum °F (°C)	11.2 (−11.half dozen)	xv.iv (−ix.two)	22.vii (−five.2)	32.7 (0.iv)	43.one (6.2)	55.2 (12.9)	62.four (xvi.9)	threescore.2 (fifteen.7)	47.3 (8.5)	33.iii (0.vii)	23.5 (−4.7)	17.4 (−viii.1)	nine.0 (−12.viii)
Tape low °F (°C)	−17 (−27)	−13 (−25)	2 (−17)	23 (−5)	34 (one)	42 (half dozen)	51 (11)	47 (8)	36 (2)	26 (−3)	−1 (−18)	−x (−23)	−17 (−27)
Average precipitation inches (mm)	4.02 (102)	4.47 (114)	4.52 (115)	4.72 (120)	five.02 (128)	four.36 (111)	four.16 (106)	3.79 (96)	3.80 (97)	3.36 (85)	iii.86 (98)	four.43 (113)	l.51 (1,283)
Average snowfall inches (cm)	two.0 (5.1)	1.5 (3.8)	0.vii (i.eight)	0.0 (0.0)	0.0 (0.0)	0.0 (0.0)	0.0 (0.0)	0.0 (0.0)	0.0 (0.0)	0.0 (0.0)	0.1 (0.25)	0.4 (i.0)	4.vii (12)
Average precipitation days (≥ 0.01 in)	10.viii	10.9	xi.6	eleven.ii	11.6	10.7	ten.3	9.4	7.8	viii.four	ix.0	11.4	123.1
Average snowy days (≥ 0.i in)	2.0	1.9	0.9	0.0	0.0	0.0	0.0	0.0	0.0	0.0	0.2	0.v	5.5
Average relative humidity (%)	70.4	68.five	64.6	63.2	69.v	70.iv	72.8	73.1	73.7	69.4	seventy.2	71.iv	69.8
Mean monthly sunshine hours	139.vi	145.2	191.3	231.5	261.8	277.7	279.0	262.i	226.four	216.viii	148.1	130.six	ii,510.1
Percent possible sunshine	45	48	52	59	60	64	63	63	61	62	48	43	56
Boilerplate ultraviolet index	ii	4	half-dozen	vii	9	10	ten	nine	7	5	3	ii	6
Source 1: NOAA (relative humidity and sun 1961−1990)[73] [74] [75]
Source 2: Weather condition Atlas (UV index)[76]

Notes [edit]

1. ^ Not to be confused with the Tennessee Valley, the drainage basin of the Tennessee River, which covers most of this region
2. ^ Many maps of the land do non separate this physiographic province into subregions.
3. ^ Hateful monthly maxima and minima (i.e. the expected highest and lowest temperature readings at whatsoever signal during the twelvemonth or given month) calculated based on data at said location from 1991 to 2020.
4. ^ Official records for Nashville were kept at downtown from May 1871 to December 1939, and at Nashville Int'l since January 1940. For more than data, meet Threadex

References [edit]

1. ^ Hudson, John C. (2002). Across this Land: A Regional Geography of the United States and Canada. JHU Press. pp. 101–116. ISBN978-0-8018-6567-1 – via Google Books.
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3. ^ ^{a b} Stein, Mark (2008). How the States Got Their Shapes. New York City: HarperCollins. pp. 257–262. ISBN978-0-06-143139-5.
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7. ^ Safford 1869, pp. 11–12. sfn error: no target: CITEREFSafford1869 (assist)
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30. ^ ^{a b} Foerste, A. F. (September 1903). "Silurian and Devonian Limestones of Western Tennessee". The Journal of Geology. The Academy of Chicago Press. 11 (half dozen): 554–583. Bibcode:1903JG.....xi..554F. doi:x.1086/621100. JSTOR 30059373.
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34. ^ Sadler, Megan (October 15, 2020). "Are you lot prepared for an convulsion? Tennessee projected to experience major convulse in coming years". WVLT-TV. Knoxville. Retrieved May 27, 2021.
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44. ^ Dyer, James K. (April 2006). "Revisiting the Deciduous Forests of Eastern Due north America". BioScience. Oxford University Press. 56 (iv): 341–352. doi:10.1641/0006-3568(2006)56[341:RTDFOE]two.0.CO;two.
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How Many Miles To Tennessee,

Source: https://en.wikipedia.org/wiki/Geography_of_Tennessee

Posted by: lemussout1994.blogspot.com

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