place

Denny P. Hadley House

Central-passage houses in TennesseeHouses completed in 1840Houses in Williamson County, TennesseeHouses on the National Register of Historic Places in TennesseeNational Register of Historic Places in Williamson County, Tennessee
Williamson County, Tennessee Registered Historic Place stubs

The Denny P. Hadley House is a house in Brentwood, Tennessee, United States, that dates from c.1840 and that was listed on the National Register of Historic Places in 1988. It has also been known as Green Pastures and as Hadleywood. The structure is a two-story brick central passage plan house and other architecture. The house was considered notable as an example of brick ante-bellum central passage plan residence. When listed, the property included three contributing buildings and three non-contributing structures on an area of 3.7 acres (1.5 ha).Denny Porterfield Hadley was born in 1797 and moved to Williamson County in 1808. In 1821, Hadley married Elizabeth Smith, and they were gifted 200 acres of land by her father. Around 1840, the Hadleys hired builder Asa Vaugn to build the house, with most construction materials coming from their farm. During the Civil War, the house was used several times as a campsite by both armies.The NRHP-eligibility of the property was covered in a 1988 study of Williamson County historical resources.

Excerpt from the Wikipedia article Denny P. Hadley House (License: CC BY-SA 3.0, Authors).

Denny P. Hadley House
Franklin Road,

Geographical coordinates (GPS) Address Nearby Places
placeShow on map

Wikipedia: Denny P. Hadley HouseContinue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N 35.981 ° E -86.822 °
placeShow on map

Address

Franklin Road 1526
37027
Tennessee, United States
mapOpen on Google Maps

Share experience

Nearby Places

Nashville Basin

The Nashville Basin, also known as the Central Basin, is a term often used to describe the area surrounding Murfreesboro, Tennessee, in which Nashville is located. The Central Basin was caused by an uplifting which produced a dome known as the Nashville Dome. The Nashville Dome is evidenced by the underlying rock strata that all dip downward away from Nashville. The uplifting of the Nashville Dome fractured overlying strata, making it more easily eroded, and thus the "dome" resulted in a "basin". Uplifted strata in the center of a geological dome have higher potential erosive energy than the surrounding strata, because they are physically higher. Erosion thus acts on the uplifted area at a greater rate than on the surrounding flat-lying area, creating a low area, i.e., a basin. This area is more correctly referred to as the "Central Dome" of Tennessee. Nashville is located in the northwestern portion of the Central Basin. The basin extends for approximately forty-five to sixty miles to the east of Nashville and about eighty miles to the south, near the Tennessee–Alabama state line. Travelers leaving Nashville in a northerly or easterly direction will soon begin the climb up the escarpment that marks the bordering geographic/geologic province, the Highland Rim and further eastwards, the Cumberland Plateau. The southern edge of the Highland Rim is more distant and somewhat less pronounced. The only downhill routes leaving the area follow the course of the Cumberland River as it flows northwest toward Ashland City and Clarksville, Tennessee. The Central Basin is underlain primarily by limestone from the Ordovician Period. The Nashville Basin and a similar but smaller area surrounding Lexington, Kentucky referred to as the "Kentucky Bluegrass" area, are the two primary areas of this sort in the world.The Inner Basin of the flattest terrain and most limestone-derived soil chemistry is located to the south and east of Nashville, primarily in the counties of Marshall, Rutherford, Wilson, and Bedford. Here also are seen the horse farms somewhat reminiscent of the Kentucky Bluegrass region. Supposedly the underlying rock weathers to a soil particularly suited to the growing of the sorts of grasses most favored by horses. Limestone glades (or cedar glades), located to the east of Nashville, primarily in Wilson and Rutherford Counties, are open areas where the flat limestone rock is denuded of overlying soil or nearly so, provide an environment for flora unlike any other in the world.