Little Wapwallopen Creek is a tributary of the Susquehanna River in Luzerne County, Pennsylvania, in the United States.

It then turns west for a few tenths of a mile and receives Nuangola Outlet, its first named tributary, from the right.

Several tenths of a mile further downstream, it passes through Andy Pond and turns west-northwest for a short distance.

Its valley broadens and it flows west-southwest for a few miles, receiving the tributary Pond Creek and crossing Pennsylvania Route 239.

[4] The concentration of dissolved oxygen in the waters of Little Wapwallopen Creek was measured in the 1970s to be 11.0 milligrams per liter (0.0110 oz/cu ft).

[3] In the 1970s, the concentration of calcium in the waters of Little Wapwallopen Creek were found to range from 5.00 to 5.90 milligrams per liter (0.00499 to 0.00589 oz/cu ft).

[3] The concentration of dissolved solids in Little Wapwallopen Creek was once measured to be 60 milligrams per liter (0.060 oz/cu ft).

[3] At its mouth, the peak annual discharge of Little Wapwallopen Creek has a 10 percent chance of reaching 2,750 cubic feet per second (78 m3/s).

[5] At a point 0.6 miles (0.97 km) downstream of Blue Ridge Trail, the peak annual discharge of Little Wapwallopen Creek has a 10 percent chance of reaching 1,400 cubic feet per second (40 m3/s).

At a point 0.3 miles (0.48 km) upstream of Blue Ridge Trail, the peak annual discharge of the creek has a 10 percent chance of reaching 1,250 cubic feet per second (35 m3/s).

[7] Alluvium, which consists of stratified sand, silt, and gravel, as well as some boulders, occurs in the valley of Little Wapwallopen Creek to a depth of 10 feet (3.0 m) or more.

Alluvial terrace also occurs near the creek, which is the only place in the quadrangle of Sybertsville that contains it in the surficial geology.

Wisconsinan Loess, which consists of windblown silt and fine sand, occurs in the southern part of the creek's valley in the Sybertsville quadrangle.

[8] In the Sybertsville quadrangle, the surficial geology in the valley of Little Wapwallopen Creek mainly consists of alluvium, alluvial terrace, alluvial fan, Wisconsinan Ice-Contact Stratified Drift, and some small patches of Wisconsinan Till.

[9] The surficial geology near the creek in the Wilkes-Barre West quadrangle mainly consists of Wisconsinan Till, with some scattered areas of bedrock and alluvium.

Henry C. Bradsby's book History of Luzerne County, Pennsylvania described Round Pond as being in the watershed as well.

[10] A package wastewater treatment facility operated by the Crestwood School District discharges into Little Wapwallopen Creek in Rice Township.

Another package wastewater treatment facility is operated by Wilbar Realty in the same township and discharges into the creek.

[17] Little Wapwallopen Creek is one of the main sources of flooding in Conyngham Township, along with the Susquehanna River.

[6] Historically, a Native American path went from Council Cup up the Little Wapwallopen Creek valley and to Wilkes-Barre.

The path ran from Council Cup to the creek and then northeast alongside it before going past Lily Lake and over Penobscot Mountain towards where Wilkes-Barre is now located.

A concrete stringer/multi-beam or girder bridge carrying Blytheburn Road was built over Little Wapwallopen Creek in 1920.

[20] A three-span bridge carrying Interstate 81 northbound over Little Wapwallopen Creek was constructed in Rice Township in 1964 and repaired in 1987.

In 1975, a prestressed stringer/multi-beam or girder bridge carrying State Route 3008/Ruckle Hill Road was built over the creek.

[20] Floodwaters from Little Wapwallopen Creek reached a height of 2 feet (0.61 m) over St. Marys Road in Dorrance Township during a storm in 1972.

The creek also once flooded to a depth of 18 to 20 inches (46 to 51 cm) over Hislop Road in Rice Township.

[5] In August 2002, the Pennsylvania Environmental Council received $57,897.76 to carry out a restoration plan on the upper reaches of Little Wapwallopen Creek.