Waterfalls of Ontario.ca/

    Newburgh Falls

 Quick Facts

 

 

Home  |  Ottawa Valley Region |  

 

 

River

Napanee River

Class

Plunge

Size

Insignificant

Visitability

Average

Accessibility

Free

Activity

Occasional hikers

Walk Time

3min

Trail

Easy

Gorge Access

Moderate

Other Trails

Some

 Location      Driving Directions
       

County

Lennox and Addington

 

Follow Hwy 401 east to Lennox and Addington Rd 41 at Napanee. Go south on this road, but turn left at Industrial Blvd, which becomes Lennox and Addington Rd 1. Drive east for about 10 minutes to the village of Newburgh. Turn left on the main road into Newburgh (Lennox and Addington Rd #27), and then turn right on to Factory St. Follow this street to the end, and walk across the Newburgh Conservation Area to the river. The lower falls are behind the playground.

Settlement

Newburgh

 

NTS Map

31C/7

 

Easting

350536

 

Northing

4909602

 

UTM Zone

 18T  
 Map Quest  Map to this falls   
     
 Description    
 

Newburgh Falls is a very small waterfalls. A trip to the site isn't even recommended unless you are on your way to nearby Yarker Falls. The site is a nice pit stop however, where two long, low waterfalls each form steps in the river that are less than 1m high and about 15-20m wide. The Napanee River flows swiftly over flat limestone and has removed all but the largest blocks from the river bed.

While small, this site shows two important geological processes. Note that most of the fractures along the river and its banks run approximately east-west. This fracture orientation, quite convincingly controls the edge of the lower waterfall. Since the rock fracture represents a weak spot in the bedrock, the river has eroded small blocks of limestone off its bed along this line. Also visible are the thin beds (1-2cm) of shale that separate the limestone forming the upper and lower waterfalls. The easily eroded shale, which can be broken in your hand) wears quicker than the limestone, forming a small overhanging rock ledge in the upper limestone bed (just visible in the photograph). The different erosion rates of each rock are primarily responsible for forming the plunge class of waterfalls, regardless of the waterfall's size.

 
Buy the Book   More Information
  I have yet to find any interesting web links for this waterfall. Please let me know if you know of any!


CAUTION!  Waterfalls can be dangerous places!  Mark Harris takes no responsibility for your safety and he does not guarantee that it is fully safe and/or legal to visit these waterfalls.  You are responsible for your own safety at all times. Mark Harris cannot give you permission to trespass on any private land. CAUTION!

Copyright (2003) Mark Harris. Last Updated September 2, 2003..


This page was made with 4W WebMerge