What is the Doe River and where is it located?

The Doe River is a tributary of the Watauga River situated in the northeast region of Tennessee, United States. It plays a significant role in the local geography of Carter County.

Where does the Doe River originate geographically?

The Doe River originates on the northern slopes of Roan Mountain, specifically within the Roan Highlands area. Its formation point is in Carter County, Tennessee, close to the North Carolina border and south of Roan Mountain State Park.

What is the general course and path of the Doe River?

The Doe River flows from its source on Roan Mountain, passing through Roan Mountain State Park and the town of Roan Mountain, Tennessee. It then proceeds westward, paralleled by U.S. Route 19E, and flows to the east of Fork Mountain. After moving north of Hampton, Tennessee, and being joined by McCathern Spring and the Little Doe River, it continues northward through the Valley Forge community before reaching Elizabethton, where it eventually merges with the Watauga River.

To which larger river system does the Doe River belong?

The Doe River is a tributary that flows into the Watauga River.

In which specific state and region of the United States can the Doe River be found?

The Doe River is located in the United States, specifically within the northeast region of the state of Tennessee.

Which county in Tennessee is the origin point for the Doe River?

The Doe River begins its course in Carter County, Tennessee.

What prominent mountain feature serves as the source for the Doe River?

The Doe River originates from the northern slopes of Roan Mountain, a significant geographical feature in the Roan Highlands.

What is the ultimate destination where the Doe River concludes its flow?

The Doe River flows to Elizabethton, Tennessee, where it ultimately empties into the Watauga River.

How does the Doe River's path interact with U.S. Route 19E?

U.S. Route 19E runs parallel to the Doe River along significant portions of its course, including west of Roan Mountain, Tennessee, and again as the river approaches Elizabethton.

What is the relationship between the Doe River and the Little Doe River?

The Little Doe River is a tributary that flows into the Doe River near Hampton, Tennessee. Geographically, the Little Doe River flows west of Fork Mountain, while the Doe River flows to the east of it.

What contribution does McCathern Spring make to the Doe River?

McCathern Spring adds its waters to the Doe River, increasing its volume as the river passes through a mountain gap north of Hampton, Tennessee.

Can you describe the Doe River's passage through the Valley Forge community?

After converging with the Little Doe River near Hampton, the Doe River flows generally northward through the area known as the Valley Forge community.

What is the historical significance of the Elizabethton Covered Bridge in relation to the Doe River?

The Elizabethton Covered Bridge, constructed in 1882, is a historic landmark that spans across the Doe River in downtown Elizabethton, Tennessee.

What are the rules regarding access and traffic for the Elizabethton Covered Bridge?

The Elizabethton Covered Bridge is open for use by pedestrians and bicyclists, but it is closed to all motor vehicle traffic.

What structures does the Doe River flow under in Elizabethton before it joins the Watauga River?

In Elizabethton, after passing a weir dam downstream from the covered bridge, the Doe River flows beneath two concrete arch bridges built in 1928: the Elk Avenue Bridge in the downtown area and the Broad Street Bridge, which carries Tennessee State Route 67.

What is the primary difficulty rating for most of the Doe River section between Valley Forge and Elizabethton, according to the International Scale of River Difficulty?

The majority of the Doe River section, from the Valley Forge put-in to the take-out point near Elizabethton, is classified as Class/Grade I on the International Scale of River Difficulty.

Are there any parts of the Doe River that present greater challenges for whitewater activities?

Yes, while most of the river is rated Class I, certain brief segments along the Valley Forge-Charity Hill-East Side run are considered Class/Grade II. Furthermore, the stretch from Hampton High School to Valley Forge Elementary involves Class 2/3 rapids, and the Doe Gorge is rated Class III/IV.

How long does it typically take to float a specific section of the Doe River using inner tubes?

It takes approximately three hours to float down the Doe River on inner tubes from the Valley Forge put-in point to the take-out location near where the river merges with the Watauga River.

What specific maneuver is required for kayakers and tubers at the weir dam near Elizabethton?

All individuals using river tubes and kayaks must perform a portage, which involves carrying their equipment around, the weir dam located immediately downstream of the Elizabethton Covered Bridge.

Where does the Doe Gorge whitewater section begin and end, and what is its classification?

The Doe Gorge, identified as a Class III/IV whitewater section, starts at the bridge on Bear Cage Road and concludes at the take-out point at Hampton High School.

How does the Doe River's flow regulation differ from that of the Watauga River?

Unlike the Watauga River, whose flow is managed by the Tennessee Valley Authority (TVA), the Doe River's water level naturally fluctuates in response to changes in rainfall or drought conditions.

What is the difference in water temperature characteristics between the Doe River and the Watauga River?

The Doe River's water temperature varies depending on the ambient air temperature, whereas the Watauga River maintains a consistent year-round temperature of approximately 52-53 degrees Fahrenheit.

During which season is the Doe River generally considered comfortable for recreational activities like kayaking and tubing?

The Doe River is typically comfortable for activities such as kayaking and river tubing during the summer months, due to its temperature variations aligning with warmer air temperatures.

How often does the Doe River valley experience severe flooding events?

Severe flooding is infrequent in the Doe River valley.

What natural factors contribute to the rapid rise of water levels in the Doe River?

The Doe River's steep stream course, combined with seasonal heavy rains (often May-early June) and snowmelt from its mountainous drainage region, allows water levels to rise rapidly along its banks.

When did the most recent significant flood occur on the Doe River, and what caused it?

The last severe recent flood of the Doe River happened overnight from January 7 to January 8, 1998. It was caused by sudden storms that resulted in seven inches (180 mm) of rain falling within a twelve-hour period.

What was the human cost associated with the January 1998 Doe River flood?

The flood in January 1998 led to the deaths of seven individuals in the Hampton area. This included Carles "Junior" Godsey, a rescue worker from Kingsport, whose boat overturned during the flood event.

What was the estimated financial impact of the 1998 Doe River flood on Carter County?

The property damages incurred in Carter County due to the 1998 Doe River flood were approximately $20 million.

What types of climate information are provided in the table for Elizabethton, Tennessee?

The climate table offers data on average monthly and annual temperatures (in Fahrenheit and Celsius), average high and low temperatures, average monthly and annual rainfall in inches, and average monthly and annual snowfall in inches.

What is the average annual temperature recorded for Elizabethton, Tennessee, based on the provided climate data?

According to the climate data, the average annual temperature in Elizabethton, Tennessee, is 55.5 degrees Fahrenheit (13.1 degrees Celsius).

What is the average annual rainfall figure for Elizabethton, Tennessee?

The average annual rainfall in Elizabethton, Tennessee, is documented as 40.7 inches.

What is the average annual snowfall total for Elizabethton, Tennessee?

Elizabethton, Tennessee, receives an average annual snowfall of 15.6 inches, according to the provided climate statistics.

What is the average high temperature in July for Elizabethton, Tennessee?

The average high temperature during July in Elizabethton, Tennessee, reaches 84.6 degrees Fahrenheit (29.2 degrees Celsius).

What is the average low temperature in January for Elizabethton, Tennessee?

In January, the average low temperature in Elizabethton, Tennessee, is 24.3 degrees Fahrenheit, which is equivalent to -4.3 degrees Celsius.

What is the average monthly rainfall amount for April in Elizabethton, Tennessee?

The average rainfall for the month of April in Elizabethton, Tennessee, is 3.3 inches.

What is the average monthly snowfall for December in Elizabethton, Tennessee?

The average snowfall for December in Elizabethton, Tennessee, is 2.6 inches.

What is the source cited for the climate data presented for the Doe River area?

The climate data for the Doe River area in Elizabethton, Tennessee, is sourced from the website climate-zone.com.

How does the Doe River's path relate to Fork Mountain?

The Doe River flows to the east of Fork Mountain, while its tributary, the Little Doe River, flows to the west of the same mountain.

What is the approximate drop per mile characteristic of the Doe Gorge section?

The Doe Gorge section of the river is characterized by a steep drop, ranging between 100 and 160 feet per mile.

What is the purpose of the `mw-kartographer-map` element within the source text?

The `mw-kartographer-map` element is utilized to display an interactive map, illustrating the geographical location and context of the Doe River with specified zoom levels and map styles.

What information does the `infobox-caption` provide for the first image in the article?

The `infobox-caption` for the initial image clarifies that it shows the Doe River flowing from its origin on Roan Mountain towards its destination in Elizabethton, Tennessee.

What is the geographic coordinate of the Doe River's source?

The geographic coordinates for the source of the Doe River are approximately 36°08′49″N 82°08′39″W / 36.1470607°N 82.1442922°W.

What is the geographic coordinate of the Doe River's mouth?

The geographic coordinates for the mouth of the Doe River, where it converges with the Watauga River, are approximately 36°21′25″N 82°12′48″W / 36.3570526°N 82.2134656°W.

What are the named tributaries of the Doe River mentioned in the provided text?

The text explicitly names McCathern Spring as a left tributary and the Little Doe River as a right tributary of the Doe River.

How does the Doe River flow through Roan Mountain State Park?

After originating from the northern slopes of Roan Mountain, the Doe River flows directly through Roan Mountain State Park.

What is the significance of the Elizabethton Covered Bridge's proximity to local amenities?

The Elizabethton Covered Bridge is situated adjacent to a city park and county government areas, enhancing its role as a central and accessible landmark within Elizabethton.

How does the steep stream course of the Doe River affect its water levels?

The steep gradient of the Doe River's stream course allows its water levels to rise rapidly along the river banks, particularly during periods of heavy precipitation or snowmelt.

What role does Roan Mountain State Park play in the Doe River's geography?

Roan Mountain State Park is located near the origin of the Doe River and the river itself flows through the park after descending from Roan Mountain.

What is the approximate duration for an inner tube float trip from Valley Forge to the Elizabethton confluence?

An inner tube float trip from the Valley Forge put-in to the take-out near the confluence with the Watauga River typically lasts about three hours.

What specific type of bridges cross the Doe River in Elizabethton, and when were they constructed?

The Doe River flows under two concrete arch bridges in Elizabethton, both of which were built in 1928.

What is the average high temperature in August for Elizabethton, Tennessee?

The average high temperature in August for Elizabethton, Tennessee, is 84.1 degrees Fahrenheit (28.9 degrees Celsius).

Doe River Wiki: The Doe River: A Hydrological and Geographical Profile of a Tennessee Waterway

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River Overview

Geographic Context

The Doe River is a significant tributary located in the northeastern region of Tennessee, United States. It originates in Carter County, near the border with North Carolina, and flows through the town of Elizabethton before converging with the Watauga River. Its course is intrinsically linked to the Appalachian Mountain landscape from which it springs.

Hydrological Connection

As a tributary, the Doe River plays a vital role in the regional watershed. Its waters contribute to the larger Watauga River system, influencing downstream flow dynamics and contributing to the overall water resources of the area. Understanding its characteristics is key to comprehending the broader hydrological network of Northeast Tennessee.

Origin and Destination

The river's journey begins on the northern slopes of Roan Mountain, a prominent peak within the Roan Highlands. It carves its path through mountainous terrain and valleys, eventually reaching Elizabethton, where it meets its larger counterpart, the Watauga River. This journey traverses diverse ecological and topographical zones.

Detailed Geography

Source and Upper Course

The Doe River originates in Carter County, Tennessee, on the northern declivities of Roan Mountain. Its initial flow is proximate to Roan Mountain State Park and the community of Roan Mountain, Tennessee. This upper section is characterized by the steep gradients typical of the Appalachian Mountains, influencing its early flow characteristics.

Flow Path and Tributaries

The river proceeds westward, often paralleled by U.S. Route 19E. Key tributaries augment its volume: the Little Doe River joins near Fork Mountain, and McCathern Spring contributes water north of Hampton. The confluence of the Doe River and the Little Doe River occurs at Hampton, marking a significant point in its hydrological development.

Mouth and Confluence

The Doe River culminates its journey in Elizabethton, Tennessee, where it merges with the Watauga River. The precise coordinates for its source are approximately 36°08′49″N 82°08′39″W, and its mouth is located at approximately 36°21′25″N 82°12′48″W. This confluence is a critical hydrological juncture within the regional watershed.

Key Locations

The river flows through or near several important locations: Roan Mountain, Hampton, and Elizabethton. It also passes by geographical features such as Fork Mountain. The region is part of Northeast Tennessee, within Carter County.

Notable Features

Elizabethton Covered Bridge

A significant historical landmark, the Elizabethton Covered Bridge, constructed in 1882, spans the Doe River in downtown Elizabethton. This historic structure connects 3rd Street and Hattie Avenue and is now reserved for pedestrian and bicycle use, adjacent to public park and government facilities. It stands as a testament to the river's integration into the local community's heritage.

River Structures

Downstream from the covered bridge, the Doe River flows over a weir dam. Further within Elizabethton, it passes beneath two concrete arch bridges dating from 1928: the Elk Avenue Bridge in the downtown area and the Broad Street Bridge, which carries Tennessee State Route 67. These structures represent infrastructural elements interacting with the river's flow.

Recreation

Whitewater Kayaking

The Doe River offers distinct sections for whitewater enthusiasts. The stretch between Valley Forge and the Elizabethton confluence is generally classified as Class I on the International Scale of River Difficulty, suitable for novice paddlers. However, brief segments within this run can present Class II challenges. A more demanding section, known as the Doe Gorge, begins at the bridge over the river on Bear Cage Rd. and ends at the take-out at Hampton High School, featuring Class III/IV rapids with significant drops per mile, requiring advanced paddling skills.

River Tubing

River tubing is a popular activity on the Doe River, particularly during the summer months when water temperatures are comfortable. The float from the Valley Forge put-in to the take-out near the Watauga River confluence typically takes about three hours. Paddling through Roan Mountain State Park is also feasible, though less documented than the gorge section.

Navigational Considerations

Paddlers and tubers must be aware of specific hazards. A portage is required around the weir dam located downstream of the Elizabethton Covered Bridge. The section from Hampton High School to Valley Forge presents Class 2/3 rapids and is considered more challenging than the downstream sections.

Climatic Influences

Temperature and Precipitation

The climate data for Elizabethton, Tennessee, reveals distinct seasonal variations. Average annual temperatures hover around 55.5°F (13.1°C), with summer highs reaching the low 80s°F (around 29°C) and winter lows dipping into the low 30s°F (around -1°C). The region receives approximately 40.7 inches of rain annually, distributed relatively evenly throughout the year, with slightly higher amounts in summer months.

Seasonal Weather Patterns

Snowfall averages around 15.6 inches per year, primarily occurring during the winter months. The Doe River's water temperature fluctuates significantly with ambient air temperatures, unlike the Watauga River's regulated, consistent temperature. This variability makes the Doe River more responsive to seasonal weather changes, particularly rainfall and snowmelt, which can cause rapid water level increases.

Climate Data Table

The following table summarizes the average monthly climate statistics for the Elizabethton area, providing a quantitative overview of the region's meteorological conditions:

Month	Jan	Feb	Mar	Apr	May	Jun	Jul	Aug	Sep	Oct	Nov	Dec	Annual
Climate of Doe River in Elizabethton, Tennessee
Avg °F(°C)	34.0°F (1.1°C)	37.4°F (3.0°C)	47.2°F (8.4°C)	55.2°F (12.9°C)	63.4°F (17.4°C)	71.1°F (21.7°C)	74.4°F (23.6°C)	73.6°F (23.1°C)	67.9°F (19.9°C)	56.7°F (13.7°C)	47.0°F (8.3°C)	38.2°F (3.4°C)	55.5°F (13.1°C)
Avg high °F(°C)	43.7°F (6.5°C)	48.0°F (8.9°C)	58.9°F (14.9°C)	67.4°F (19.7°C)	75.2°F (24.0°C)	82.2°F (27.9°C)	84.6°F (29.2°C)	84.1°F (28.9°C)	79.1°F (26.2°C)	69.1°F (20.6°C)	58.2°F (14.6°C)	48.1°F (8.9°C)	66.6°F (19.2°C)
Avg low °F(°C)	24.3°F (-4.3°C)	26.8°F (-2.9°C)	35.4°F (1.9°C)	43.0°F (6.1°C)	51.6°F (10.9°C)	59.9°F (15.5°C)	64.1°F (17.8°C)	63.1°F (17.3°C)	56.6°F (13.7°C)	44.2°F (6.8°C)	35.9°F (2.2°C)	28.2°F (-2.1°C)	44.4°F (6.9°C)
Rain (inches)	3.2 in.	3.4 in.	3.7 in.	3.3 in.	3.8 in.	3.5 in.	4.3 in.	3.2 in.	3.3 in.	2.6 in.	2.9 in.	3.4 in.	40.7 in.
Snow (inches)	5.2 in.	4.2 in.	2.3 in.	0.4 in.	0.05 in.	0.05 in.	0.0 in.	0.0 in.	0.05 in.	0.0 in.	0.9 in.	2.6 in.	15.6 in.
Source: climate-zone.com

Historical Context

The 1998 Flood Event

The Doe River valley has experienced severe flooding, notably during the overnight period of January 7-8, 1998. Intense rainfall, measuring seven inches in twelve hours, caused rapid water level increases. This event resulted in seven fatalities, including a rescue worker, and approximately $20 million in property damages within Carter County. This highlights the river's potential for rapid and destructive hydrological responses due to its mountainous watershed and steep course.

Community Integration

The river's historical presence is marked by structures like the Elizabethton Covered Bridge, built in 1882, demonstrating its long-standing relationship with the local populace. The river has been a source of recreation and a geographical feature around which communities like Elizabethton and Hampton have developed.

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References

U.S. Geological Survey Geographic Names Information System: Doe River

A full list of references for this article are available at the Doe River Wikipedia page

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Disclaimer

Important Notice

This page has been generated by an Artificial Intelligence and is intended for informational and educational purposes only. The content is derived from a snapshot of publicly available data and may not be entirely accurate, complete, or up-to-date. It is presented to facilitate advanced study and understanding.

This is not professional advice. The information provided herein is not a substitute for expert geographical, hydrological, or environmental consultation. Always consult with qualified professionals for specific analyses or project requirements related to river systems, water resources, or regional geography.

The creators of this page are not responsible for any errors or omissions, or for any actions taken based on the information provided.

The Doe River

💡 Dive in with Flashcard Learning! 💡

River Overview ℹ️

🗺️ Geographic Context

🔗 Hydrological Connection

🏞️ Origin and Destination

Detailed Geography ⛰️

📍 Source and Upper Course

➡️ Flow Path and Tributaries

confluence Mouth and Confluence

🏛️ Key Locations

Notable Features 🌉

🏛️ Elizabethton Covered Bridge

🌊 River Structures

Recreation 🛶

🚣 Whitewater Kayaking

🛟 River Tubing

⚠️ Navigational Considerations

Climatic Influences ☀️

🌡️ Temperature and Precipitation

❄️ Seasonal Weather Patterns

📊 Climate Data Table

Historical Context ⏳

🌊 The 1998 Flood Event

🏛️ Community Integration

Teacher's Corner 🧑‍🏫

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📜 Important Notice

Dive in with Flashcard Learning!

River Overview

Geographic Context

Hydrological Connection

Origin and Destination

Detailed Geography

Source and Upper Course

Flow Path and Tributaries

Mouth and Confluence

Key Locations

Notable Features

Elizabethton Covered Bridge

River Structures

Recreation

Whitewater Kayaking

River Tubing

Navigational Considerations

Climatic Influences

Temperature and Precipitation

Seasonal Weather Patterns

Climate Data Table

Historical Context

The 1998 Flood Event

Community Integration

Teacher's Corner

True or False?

Test Your Knowledge!

Gamer's Corner

Discover other topics to study!

References

Feedback & Support

Disclaimer

Important Notice