A
BRIEF DESCRIPTION OF THE MERAMEC FROM SOURCE TO MOUTH.
Seven
miles northeast of the town of Salem in southeastern Missouri, a spring-fed brook
called the Watery Fork merges with a larger wet-weather branch 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 succession 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.