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Lahaska Creek

Stream in Wrightstown Township, Pennsylvania From Wikipedia, the free encyclopedia

Lahaska Creek (Lackawissa or Lahaskeekee) is a tributary of Mill Creek in Wrightstown Township, Bucks County, Pennsylvania.[1] The Geographic Name Information System I.D. is 1178763,[2] U.S. Department of the Interior Geological Survey I.D. is 02632.[3]

Nativename
CountryUnited States
CountyBucks
Quick facts Lahaska Creek Randalls Creek, Randalls Run, Randals Run, Native name ...
Lahaska Creek
Randalls Creek, Randalls Run, Randals Run
pushpin map showing location of
pushpin map showing location of
Location within Pennsylvania
Native name
Location
CountryUnited States
StatePennsylvania
CountyBucks
TownshipSolebury Township, Buckingham Township
Physical characteristics
Source 
 • coordinates40°21′25″N 75°1′58″W
 • elevation310 feet (94 m)
Mouth 
 • coordinates
40°18′47″N 75°3′23″W
 • elevation
210 feet (64 m)
Length3.04 miles (4.89 km)
Basin size
6.97 square miles (18.1 km2)
Basin features
ProgressionLahaska Creek → Mill Creek → Neshaminy Creek → Delaware River → Delaware Bay
River systemDelaware River
LandmarksHolicong Park
Slope
32.89 feet per mile (6.229 m/km)
Close

History

The area was originally inhabited by the Lenape native americans as Lackawissa or Lahaskeekee, "the place of much writing". In 1718, Richard Mitchell purchased 70 acres (28 hectares) and built a mill. It was replaced later by another mill known as Rush Valley Mills. After Mitchell, it was owned by Eldad Roberts, then by Joseph Watson.[1]

Course

Lahaska Creek rises near the southwest border of Solebury Township from an unnamed pond north of the village of Lahaska. Flowing just a little over 100 feet (30 m), it enters Buckingham Township running southwest, then south, then southwest again, runs through five more ponds, and is supplied by two unnamed tributaries before its junction with Watson Creek forming Mill Creek at the Mill Creek 6.80 river mile.[4]

Geology

The headwaters of Lahaska Creek begins in the Stockton conglomerate from the Triassic consisting of conglomerate and conglomeratic sandstone. Mineralogy is mostly quartz.

It quickly moves into the Stockton Formation also from the Triassic, which consists of sandstone, arkosic sandstone, shale, siltstone, and mudstone.

It then very briefly flows through a small portion of the Beekmantown Group, from the Ordovician, a layer of limestone containing dolomite, and chert.

Then it spends most of its time in the Allentown Formation, from the Cambrian. The Allentown consists of dolomite and impure limestone, siltstone containing calcium carbonate, oolites, stromatolites, and sharpstone.[5]

Municipalities

Crossings and Bridges

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