About fifteen miles Southeast of the town of Salem
in Southeastern Missouri, near the junction of Dent County Roads 559 & 560,
a spring-fed brook begins its journey North. Before long, the brook merges
with the ‘Dry Branch’ (on the right), ‘Wofford Branch’ and ‘Carty Branch’
(both on the left) and becomes the source of the Meramec River. For many
millions of years the Meramec has been carving its twisting, sometimes tortuous
240 mile course into the solid rock of the Ozark Plateau, scouring its way
through a deep, slowly widening valley, bordered by limestone bluffs and
steep hills. It is joined along the way by innumerable springs, creeks,
and four large tributaries, which transform the Meramec into a one hundred
yard - to two hundred yard wide flood plane stream at its confluence with
the Mighty Mississippi eighteen miles below St. Louis.
Maramec spring (note the spelling) is the first of
the four major contributors, it pours an average volume of one hundred million
gallons of cold clear water into the Meramec per day, swelling the river
to twice its size. It is interesting to note that the Dry Fork, which is
about the same size as the Meramec in that area, loses most of its volume
underground to become a major contributor to Maramec Spring, and in a round-about
way - a major contributor to the Upper Meramec. Over the next thirty miles,
the inflows from many smaller branches turn the river into a prime stream.
Then, from the right, the translucent waters of the second and largest of
the headwater contributors, the Courtois--(pronounced code-away)--Huzzah
creek, mingles with the Meramec, giving it the impression of a truly big
river. Swirling on past Onondaga Cave (Leasburg), Meramec State Park (Sullivan),
and the Meramec Caverns (Stanton)--all on the left-- the Meramec receives
the cloudy waters of the Bourbeuse River--its only major contributor from
the west. As the darker waters flow on, the valley widens, and the river
becomes a series of long, slow, wide pools, connected by short, fast, riffles.
Around twenty-five miles below the Bourbeuse River confluence, the last
major contributor, the Big River, flows into the Meramec from the right.
Now, even wider and more sluggish, it enters the Mississippi flood-plain,
and wends its way another thirty miles before draining into the Mississippi.