Jacks Fork RiverThe Definitive Guide

Stretch 5 of 28 · miles 7½ to 9¼

McCubbin Hollow


In Reach D, Steel Bridge to Muck Forty · on Plate A4

Stretch 5: McCubbin Hollow
Stretch 5McCubbin Hollow · river miles 7½ to 9¼

Royal Hole

Pool · about mile 7.5 · Plate A4

The known as Royal Hole, a short way below Whitbeck Hole, is marked by backwater and rocks on the right. Wild goats, once common along the Current and the Jacks Fork, still lived near it around 1980. Royal Hole was on the park’s list of primitive campsites in 1981, and a short park road carries its name. A resident who came to Mountain View from Oklahoma in 1979 marked a pool a little below the bridge as Blue Hole, one of several on the upper river to carry that name (Reach C; Chapter 18).

The unnamed branch and the mussel bed

Side branch and riffles · left bank · about miles 7.6 to 8.4

A little over half a mile below the bridge the next creek of any size comes in from the north, draining about three-quarters of a square mile. It has no recorded name.

Between that and McCubbin Hollow lay the richest site found anywhere in the riverways in 2023–24. Six species were found there, five of them alive, more than at any other site in the park, among them the purple lilliput, a small mussel critically imperiled in Missouri, whose larvae are known to grow on green and longear sunfish. At a site near the bridge first searched in 1982, finding nineteen live mussels in 2017–19 took longer than at any other site on the upper river. The river’s mussels and their decline are the subject of Chapter 16.

Lily Pad Hole

Pool and springs · about mile 7.9 · Plate A4

The pool known as Lily Pad Hole, about 7 feet deep at , lies under a high on the left, with tall pines and cedars on the grassy slope above it and lily pads along the water’s edge. A good spring comes in on the left after running about a hundred feet down a small hollow from under a rock, and two small springs flow off the hill on the right; in summer they leave little more than slick rock to mark the place. A larger spring is said to roar out of in the bluff into a slough that reaches the river unseen through the thicket on the left. At or a short way below the hole the river passes from Texas County into Shannon County.

McCubbin Hollow and McCubbin Spring Hole

Hollow, spring and pool · right bank · mile 8.4 · Plate A4

McCubbin Hollow comes in from the south, the larger of two hollows that reach the river within a few hundred yards of each other. Its creek runs a little over two miles and drains about two square miles. The hollow is dark, rough and narrow, under three layers of growth: tall trees, shade-tolerant underbrush, and ferns and moss on the ground.

McCubbin Spring rises about a quarter of a mile up the hollow from under several slabs of rock on its right side. It is said to average about a million gallons a day, the largest spring on the river to this point. Its branch runs out of the hollow over a into McCubbin Spring Hole. A small spring comes in at the edge of the river above the hole, and nearby is a shelter.

A William McCubbin is said to have lived in the hollow and run a mill in the 1850s, placed both on the and on the river a little below Belew Hollow. McCubbin’s Mill was still standing during the Civil War, when a Union patrol came home by way of it in November 1863 (Chapters 5 and 6).

Belew Hollow

Hollow, cave and shelter · right bank · mile 8.6 · Plate A4

Belew Hollow, the smaller of the pair at about three-quarters of a square mile, is short and steep, and its creek drops through it in two wet-weather waterfalls. Under the lower one is Belew Hollow Shelter, a half-horseshoe overhang about thirty-five feet wide and up to twenty feet deep, with a splash pool outside. In normal flow the hollow’s stream sinks into its bed upstream and comes out again from the back wall of the shelter. The base of the Roubidoux lies at the lip of the upper waterfall, so the two falls step from the Gasconade up into the next formation. Belew Cave, thirty-five to feet long, opens in the same stretch (Chapter 13).

Floaters on overnight trips have used the mouth of the hollow as a stopping place, and in 2023 mussel surveyors found three species near it. One of the pools called Gar Hole has been placed near the mouth of Belew Hollow (Reach C; Chapter 18).

Simpson Hole

Pool and cave · about mile 8.8 · Plate A4

Simpson Hole is a good fishing hole in rocky water that suits smallmouth bass and . A small spring enters on the right, and nearby a shelter is marked by a large sycamore growing out of it. Simpson Hole Cave opens in the base of a vertical bluff in the same stretch, and anyone floating past can see its entrance, about thirty feet wide and twelve high. A caving party in 2007 found it heavily used, with the remains of a campfire, some broken formations and about two dozen pipistrelle bats, and suggested a gate (Chapter 13). Double Cave, named for its two large entrances and mapped in 1984, lies in the same stretch between the bridge and Blue Spring.

A little below Simpson Hole an unnamed branch drains a little over a square mile from the north. It is the largest creek in the reach without a recorded name.

Beaver Hole and Slant Rock Hole

Pools · about mile 9.2 · Plate A4

Beaver Hole, also called Beaver Den Hole, is a good fishing hole bordered by a bluff on the right. Little Bottom Hole, with a bluff on the left, lies somewhere above it; its place is not fixed.

Slant Rock Hole follows, and it is said to be the prettiest hole on the Jacks Fork. A high bluff stands on the right, and a large rock slants down into the water. The gravel bar on the left has long been a favorite place to camp.

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