Dale Hollow Lake, Kentucky & Tennessee, USA

Lake Locations:

USA - South - Kentucky - Southern Lakes - Tennessee - Middle -

Also known as:  Dale Hollow Reservoir

Dale Hollow Lake, straddling the Kentucky-Tennessee border, is an artificial lake that was formed by damming the Obey and Cumberland Rivers. As with many other lakes in this region of the United States, the U.S. Army Corps of Engineers took on the project in order to provide flood control for the surrounding area. However, Dale Hollow Dam was the first such project in Kentucky, authorized in 1938, giving it the title of the oldest artificial lake in the state. A decade later, hydroelectric power generators were added to supply power to the surrounding countryside.

Dale Hollow Reservoir is named after William Dale, an early 19th century owner of the lands that eventually became known as Willow Grove. When the town was flooded in 1942, everything was buried under the lake’s waters, nicknaming Willow Grove “the town that drowned”. Since then, the lake has become a Kentucky recreational mecca. Water lovers flock to the shores of this 27,700 acre lake each year, partaking in the varied offerings such as swimming, boating, and fishing. The average summer pool is 651 feet above sea level; winter pool averages 632 feet. The original river channel near the dam is the deepest part of Dale Hollow Lake at 130 feet; average depth is around 50 feet.

Dale Hollow is an angler’s dream come true. Famous for its smallmouth bass fishing, the lake holds the world record for largest of this species ever caught (11 lbs., 15 oz.). Other species that proliferate here are catfish, crappie, gar, largemouth bass, muskellunge, trout, and walleye. At Dale Hollow, fishing season lasts 365 days a year, and the fish seem to be looking for a line to bite. If you’d like to try fishing of a different variety, Dale Hollow is an excellent location for underwater spear fishing of rough fish. Underwater spear fishing is restricted to hand-held or mechanically propelled spears; a fishing license is required.

Dale Hollow Lake State Resort Park borders the lake on the Kentucky (north) side, offering visitors some fantastic activity selections within its 3,400-acre boundaries. Nature lovers spend hours on the more than 15 miles of nature trail that the park offers, designed for beginner and advanced hiking, horseback riding, and mountain biking. The trails wind their way through the park, snaking past shoreline, leading to ridges with spectacular views, and introducing some of the unique sights and sounds of Kentucky.

Boaters love Dale Hollow Reservoir because of its large size and over 620 miles of shoreline (summer pool) to explore. Many small coves await adventurous boaters, and if you’re quiet enough, you’ll catch glimpses of the lake’s diverse fauna, especially the graceful birds that swoop and fly above your head. After relaxing in the coves, open up your motor and enjoy a quick-paced ride across crystalline blue waters. And if you’re a water skier or wake boarder, the wide open main channel will provide you with optimum opportunities.

For a more mellow mood, head to the shores of the lake and indulge in a little bit of swimming. Picnic tables dot the state park, so stop for a midday bite to eat in between rounds of swimming and splashing in the cool lake waters.

Swimming, boating, fishing, hiking, water-skiing: Dale Hollow Reservoir has something for every taste. Deep blue waters and a pristine shoreline invite you to indulge in all of these outdoor activities, so book your trip soon.

Things to do at Dale Hollow Lake

  • Vacation Rentals
  • Fishing
  • Boating
  • Swimming
  • Water Skiing
  • Picnicking
  • Hiking
  • Biking
  • Horseback Riding
  • Birding
  • State Park

Fish species found at Dale Hollow Lake

  • Bass
  • Black Bass
  • Catfish
  • Crappie
  • Gar
  • Largemouth Bass
  • Muskellunge
  • Perch
  • Pike
  • Smallmouth Bass
  • Trout
  • Walleye

Dale Hollow Lake Photo Gallery

Dale Hollow Lake Statistics & Helpful Links

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Trophic State | LakeLubbers

Trophic State measures the level of algae and nutrients in a lake.

An oligotrophic lake is very clear (blue in color) and does not support much plant or fish life. A hyper-oligotrophic lake is the clearest of all lakes, and is nearly devoid of plants and fish.

A mesotrophic lake is slightly green and supports a moderate degree of plant and fish life. A lake's most desired trophic state is generally this mid-point - the mesotrophic state.

A eutrophic lake is somewhat murky and supports a large amount of plant and fish life. A hypereutrophic lake is clouded with algae, plant life, and fish life. A eutrophic or hyper-eutrophic lake can be difficult to navigate by boat - and is often an unpleasant place to swim.

The use of phosphorus-rich and nitrogen-rich fertilizer on lawns and golf courses surrounding a lake can cause it to become eutrophic or hypereutrophic.


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Catchment or Drainage Area | LakeLubbers

This is the surrounding area that drains into a lake, including land, rivers and their tributaries. This is also known as the lake's "catchment basin".

Small lakes at the highest peaks of mountains have small drainage areas. The world's oceans have the largest drainage areas.


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Lake-Area Population | LakeLubbers

This is the estimated number of people who live in a house with a view of a lake, plus those who self-describe the lake as their home, for example: "I live at Smith Mountain Lake."


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Water Residence Time | LakeLubbers

This is the estimated time that it takes for an amount of water equal to the entire volume of a lake to flow out of - or evaporate from - the lake.

Residence Time can be as short as a few days for fast-flowing small lakes, and can exceed 100 years for slow-flowing large lakes.


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Completion Year | LakeLubbers

This is the year that a reservoir was first filled to the reservoir's normal elevation - or the year that a natural lake was first dammed. A large reservoir can take more than a year to fill after its dam is first closed.

The Grand Anicut in southern India is generally considered the world's oldest dam that still operates. Grand Anicut was constructed in the second century BC. It now impounds an irrigation network that includes roughly one million acres.

You can find many of the the world's newest reservoirs on LakeLubbers. Many of the world's oldest reservoirs appear on the last page of that list.


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Water Volume | LakeLubbers

This is the estimated volume of water that a lake contains -- measured at the lake's normal elevation. By this measure, the world's largest freshwater lake is Siberia's Lake Baikal.

You can find many of the the world's largest lakes (by water volume) on LakeLubbers.

Water Volume can be measured in acre-feet, in cubic miles, or in cubic kilometers. One acre-foot is the amount of water needed to cover one acre (43,560 square feet) to a depth of one foot. One cubic mile equals 3,379,200 acre-feet. One cubic kilometer equals 810,713 acre-feet.

1 acre-foot is equal to 325,851 US gallons. Siberia's Lake Baikal contains about 6,276,367,740,000,000 gallons of freshwater - nearly 1 million gallons for every living person on earth.

The other - and more widely used - measure of a lake's size is the lake's surface acreage. By that measure, the world's largest freshwater lake is North America's Lake Superior.


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Maximum Depth | LakeLubbers

This is the estimated greatest depth of the water in a lake -- measured at the lake's normal elevation. The world's deepest lake is Siberia's Lake Baikal; that lake's maximum depth is estimated at 5,314 feet.

You can find many of the the world's deepest lakes on LakeLubbers. If you select the last page of that list, you will find the (maximum depth of) the shallowest lakes in our database.


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Average Depth | LakeLubbers

This is the estimated average depth of the water in a lake -- measured at the lake's normal elevation. If the water volume and surface area of a lake are known, an estimate of the lake's average depth can be calculated:

Water volume ÷ Surface Area = Average Depth

Example: 1,000,000 acre-feet ÷ 20,000 acres = 50 feet average depth


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Maximum Elevation | LakeLubbers

This is a lake's highest water level, measured by the lake's surface distance above sea level, that can occur during flooding. A lake's highest possible maximum elevation is usually the top of the lake's dam or spillway.

At lakes that include residential development, government regulations usually forbid the construction of homes below a lake's maximum elevation.


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Minimum Elevation | LakeLubbers

This is a lake's lowest water level, measured by the lake's surface distance above sea level, that can be reasonably expected to occur. Low lake levels can occur due to deliberate seasonal draw downs for irrigation or impending snow melt, reduced water inflows, drought and evaporation, residential or commercial water demands, and hydropower generation.

Some lakes' minimum and maximum elevations are virtually the same. Lakes that generate hydropower may vary by several feet - according to power demand. Lakes whose primary purpose is to prevent flooding can seasonally vary by 100 feet or more.

When some lakes reach their minimum elevation, their boat ramps may not be long enough to permit boat access - and boats docked on shallow parts of the lake may end up on dry ground. In those cases, kayakers and shore-based anglers may be among the few happy recreational users of the lake.


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Normal Elevation | LakeLubbers

This is a lake's normal water level, measured by the lake's surface distance above sea level. For a reservoir, this water level is also known as "full pond" or "full pool".

You can find many of the world's highest-elevated lakes on LakeLubbers. Lakes with the lowest elevations (known by LakeLubbers) are shown on the final page of that list.


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Shoreline Length | LakeLubbers

This is the length of the exterior shoreline around a lake - measured at the lake's normal elevation. The shoreline length can be considerably shorter or longer when lake water levels are lower or higher than normal.

A lake with many coves has a much longer shoreline than a lake of similar surface area that is nearly circular in shape.

When known, the shoreline miles that we report in our statistics include only the lake's exterior shoreline, and exclude the shorelines of islands located within a lake's boundaries. In lakes with many islands, those islands' combined shorelines may exceed a lake's exterior shoreline.

You can find many of the world's longest-shoreline lakes on Lakelubbers.


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Surface Area | LakeLubbers

This is the area (acreage, square kilometers, etc.) of the top surface area of a lake - measured at a lake's normal elevation. The surface area can be considerably smaller or larger when lake levels are lower or higher than normal. North America's Lake Superior is the world's largest freshwater lake by this measure.

The other measure of a lake's size is the lake's water volume. By that measure, the world's largest freshwater lake is Lake Baikal in Siberia.

You can find many of the world's largest lakes (acres) on Lakelubbers. There is no widely-accepted minimum surface area that defines a lake. What Lakelubbers describes as a lake, you might call a pond. The smallest lake that Lakelubbers currently includes is Hawaii's 2-acre Lake Waiau.


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Water Level Control | LakeLubbers

This is the organization that controls water releases or outflows from the lake or reservoir. In the USA, this is often the US Army Corps of Engineers, a power company, a municipal water system, an irrigation district, or a paper manufacturing company. In the case of private or gated lakes, a homeowners' association may be the lake's controlling authority.

Many lakes cross borders, including North America's Great Lakes. The control of such lakes and their coveted freshwater may be amicably shared - or hotly disputed.

"Water wars" continue at many lakes as growing populations and crop irrigation needs compete for the freshwater that lakes contain.


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Lake Type | LakeLubbers

There are 3 basic types of lakes that are currently included on LakeLubbers. 2 types may be dammed or not dammed, producing 5 classifications.

- A Reservoir is a man-made freshwater lake that is usually created by damming rivers.

- A Natural Freshwater Lake occurs naturally - often by glacial activity - and has a salinity of less than 30 parts per thousand. It may be dammed to produce electricity or for other reasons.

- A Natural Saltwater Lake occurs naturally and has a salinity of more than 30 parts per thousand (ppt). It may be dammed.

"Brackish" water may be categorized as freshwater or saltwater, depending on its salt content (salinity). Oligohaline water has less than 15 ppt of salt. Mesohaline water has 15-29 ppt. Polyhaline has 30-335 ppt.


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