North Fork Trout Fishing

Ozark Off-Trail Hiking: Ball Pond Hollow


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A few pictures and a brief description of an off-trail hike through
Ball Pond Hollow on the North Fork River
Missouri Ozarks Hiking
By Jim
Photos by Jim

(Click on any picture for a larger image)

May 11th, 2002

The North Fork was bustling from the after effects of an Ozark's Spring rain, forcing the intermittent streams and springs to flow at spectacular rates. Seemed like a great day to take an Ozark's off-trail hiking adventure and explore Ball Pond Hollow, located within a few miles of the ROLF in the Mark Twain National Forest, North Fork River, Missouri Ozarks.

Ball Pond Hollow
Ball Pond Hollow's intermittent stream.

What started conceptually as a short 3 hour off-trail hike to locate Potato Cave, turned into a 6.5 hour trek marveling at the treasures that lined the path. By the time we got to Potato Cave Hollow we had ran short of adequate time to actually locate the cave, but had a great trip nevertheless.

One of my faults is I have a hard time hiking past any Karst topography that shows it might contain a cave; or any other oddity that captures my attention. Anytime I pass one of these features I must stop, drop my ruck, and take in the beauty and explore it to my content. I generally like to record it with my camera to share on the Web. This practice adds a considerable amount of time to the trek, but has its own rewards for the soul.

This particular cliff [located .3 miles up the stream bed from Kelly Ford Road] was a nice place to take a breather. The spring water gently dripping down from several places cooled the area a couple of degrees, making for a nice rest spot.

A cliff overhang dripping in multiple places makes a great spot to cool off during the hike
A cliff overhang dripping in multiple places makes a great spot to cool off during the off-trail trek.

A rather curiously bent tree was the next item to warrant a photo. The trunk was bent to form a rather long bench; with the tree stump, as well as the horizontal portion of the trunk, being hollow.

Numerous other picturesque settings presented themselves along the Ozark hike, and I snapped a few more pictures. For every picture I snapped there were a hundred more for the taking.

A curiously bent tree with a hollow stump and hollow horizontal section
A curiously bent tree with a hollow stump and hollow horizontal section
A bit of drift wood deposited from the last flood makes for a picturesque setting
A bit of drift wood deposited from the last flood makes 
for a picturesque setting
Spring water gently gliding over a limestone ledge
Spring water gently gliding over a
limestone ledge

As we continued to hike up the stream we came to a point where dual branches of intermittent streams dumped into the Ball Pond Hollow stream. Just through the trees we could hear rushing water from the first branch. What a pleasant surprise we encountered as we broke through the brush.

A beautiful waterfall, dubbed "5 Layer Falls" for the purpose of this article, was discovered. Cold spring water cascaded over the rocks forming 5 distinct drops, on its way to the stream. Its sister branch to the north could be heard, but not yet seen. I volunteered to explore the north branch, while my friend decided to explore "5 Layer Falls" upstream towards its source.

5 layer falls, the first of two branches feeding the stream at one point
"5 Layer Falls", the first of two branches feeding the stream at one point

The second stream of the dual branches had a nice little water fall, but was nowhere near as beautiful as "5 Layer Falls". We separately followed both streams upstream for a few minutes, but discovered nothing spectacular. We plan on returning to dual branches [located .8 miles up the stream bed from Kelly Ford Road; .5 miles from the dripping cliff] for another trip in the future, to follow both streams to their sources.

The second branch feeding the stream at the same point of 5 layer falls
The second branch feeding the stream at the same point of "5 Layer Falls"

As we continued on our Ozark's off-trail hike up the stream, we came upon a pair of water falls flowing into Ball Pond. The site was spectacular! Only we didn't know the real beauty of the formation was on the top side, where the water had carved its irregular path as a trough through the limestone. When I first saw the gentile turns and slope, I thought immediately how it reminded me of a log ride that you might find at an amusement park.

Ball Pond
The dual water falls and pool at "Ball Pond" This is a great spot for a picnic and swimming hole.

The cut channel is an amazing piece of work, but proved nearly impossible to capture on film. I have posted the three best photos I took from three different angles, but none document the pure raw beauty and uniqueness of the formation. "Ball Pond Falls" [located 1.1 miles up the stream bed from Kelly Ford Road; .3 miles from the dual branches] makes an excellent spot for a picnic.

Downstream view of the upper channel at "Ball Pond Falls"
Downstream view of the upper channel at
"Ball Pond Falls"
Perpendicular view of the upper channel at "Ball Pond Falls"
Perpendicular view of the upper channel at
"Ball Pond Falls"
Upstream view of the upper channel at "Ball Pond Falls"
Upstream view of the upper channel at
"Ball Pond Falls"

Our Missouri off-trail hiking trip moved on toward Potato Cave Hollow [located 1.5 miles up the stream bed from Kelly Ford Road; .4 miles from Ball Pond Falls]. At a few places during the hiking trip it became evident the stream was a "losing stream", as flowing surface water would suddenly disappear into the rocks, only to emerge again upstream. Don't despair if your Ozark off-trail hike in a stream bed suddenly turns into a trek in the rocks, as the stream might reappear as you approach a fresh source of water; such as a spring or intermittent stream branch.

By the time we got to Potato Cave Hollow we had less than an hour to find the cave and explore it, and we were wore out from our numerous excursions up the bluffs along the way looking for other caves or oddities. We hiked both sides of the hollow, up the bluff to the top of the ridge, and all along the ridge; but were unable to locate the cave. It was decided that Potato Cave would have to wait for another trip. Our legs thanked us.

At a brisk pace on the way back, following more game trails on the bank instead of hiking through the stream bed, we made it back to the road from "Ball Pond Falls" in about an hour.

Footnotes:
Potato Cave (called "Tater Cave" by the locals) was used at the turn-of, and the early, 20th century as a communal winter storage for tubers. [More to come on this North Fork history gem in a future article.]

Ball Pond was named after an 1800's homesteading family and was used as a communal watering hole for livestock in the dry summer months, as well as a picnic area and swimming hole. [More to come on this North Fork history gem in a future article.]

Topography Map of Ball Pond Hollow with landmarks noted.
 
Notes:
  • Please follow all safety rules when hiking and observe all Mark Twain National Forest rules and regulations.
  • Please respect the rights of the private land owners located along the road leading to and surrounding the lower part of the hollow.
  • This off-trail hike is at a gentle grade, but is moderately difficult due to the many rocks in the streambed. The streambed is usually the best route, but most of the time there are game trails along side the streambed for those wishing to avoid most of the water and rocks (but more bugs and brush). Please plan on possibly getting wet up to your knees at times (depending on the water level), as it is necessary to cross the stream several times even if you choose to hike solely along the banks.
  • Be sure and notify someone of your hiking route, time of return, and pack plenty of water and snacks for the trip. A compass, map, and the knowledge to use them are recommended.
  • Parking is best taken at Kelly Ford, necessitating a .3 mile walk back up the road to the low-water bridge where the Ball Pond Hollow intermittent stream crosses the road.
  • Ask Myron, or email the Webmaster (who wrote this article) for more details or if you have any questions.
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