The Chain of Rocks Bridge spans the Mississippi River on the north
edge of St. Louis, Missouri. The eastern end of the bridge is on
Chouteau Island, part of Madison, Illinois, while the western end
is on the Missouri shoreline. The bridge was used by U.S. Route 66
to cross over the Mississippi. Its most notable feature is a
22-degree bend occurring at the middle of the crossing, necessary
for navigation on the river. This bend is a compromise due to the
unique geology of the area and concerns about the navigation of
river traffic around the bridge pylons. Another interesting feature
is the Chain of Rocks, a rocky area in the Mississippi that gave
the bridge its name. This feature used to wreak havoc with river
navigation and has since been bypassed by the man-made Chain of
Rocks Canal.
To log this cache:
1. Take a picture of your face with the rock ledge in the
background. This is best taken from the coordinates.
2. Go up on the bridge (you can park free near the Illinois
side) and email the following items from the sign near the center
of the bridge on the south side. The river supports how many
species of fish and how many species of mussels? What is the cubic
feet of water per second that roughly flows out to the Gulf of
Mexico? What is the first line of the quote from Mark Twain about
his book “Life on the Mississippi.”?
LOGS NOT MEETING THE CRITERIA WILL BE DELETED.
Be sure to get the virtual cache GC2258 located on the bridge
while you are there.
There is parking access to the bridge from both sides but it is
recommended to park on the Illinois side as there is better
security and car break-ins have been reported on the Missouri side.
On 06/12/09, cacher BlueBeadMan reported: "...the Illinois side of
the river is just as dangerous as the Missouri side, it just
doesn't get the same publicity. You find just as much broken glass,
beer bottles, evidence of criminal activity, and things like used
condoms on the IL side as you do on the MO side. Perhaps the famous
murder case which occurred on the middle of the bridge and was
tried in MO gives the MO side a worse reputation. Who knows...the
IL side is more secluded and thereby more prone to criminal
activity than the MO side..."
Originally a motor route, it now carries walking and biking
trails over the river. The chain of rocks stretch for seven miles
immediately to the north of the city of St. Louis. The
Mississippi's water, narrowed by these rock ledges, rushes through
this reach at speeds of 12 feet per second, roaring down a decline
of 11 feet in seven river miles.
Both the strange 22-degree turn in the bridge and the Chain of
Rocks owe their existence to glaciers. During the last ice age, the
Mississippi River was re-routed from its original channel in soft
river sediment to its present channel over resistant, mainly
limestone, bedrock. The river has yet to wear down the bedrock and
this feature is still a rough spot in the river. If the bridge had
been built straight, the engineers would have had to choose between
two problematic routes. One route would have put the bridge in a
location where it couldn't have been solidly founded on bedrock.
The other route would have posed problems to river navigation by
not allowing barges to line up with the current, possibly causing
them to collide with the bridge. It served as a compromise between
geological and navigational concerns.
Other changes in the course of the river have occurred because
of earthquakes along the New Madrid Fault Zone, which lies between
Memphis and St. Louis. Three earthquakes in 1811 and 1812,
estimated at approximately 8 on the Richter Scale, were said to
have temporarily reversed the course of the Mississippi. The
settlement of Reverie, Tennessee was cut off from Tipton County,
Tennessee, during the 1811 and 1812 earthquakes and placed on the
western side of the Mississippi River, the Arkansas side. These
earthquakes also created Reelfoot Lake in Tennessee from the
altered landscape near the river.
The rapids seen just to the south of the bridge are actually
water spilling over the 2,925-foot low-water River Dam 27, the
first permanent rock-fill dam across a major river in the United
States. This dam was built in 1960 to insure adequate depths over
the lower sill of the old Alton Locks that was 12.5 river miles
upstream.
From the Illinois side of the bridge, signs marked "HISTORIC
ROUTE 66 SPUR" take travelers to the Illinois side of the bridge
and a "HISTORIC ROUTE 66" sign marks the Missouri side of the
bridge. The Gateway Arch is visible downriver, and immediately
downstream from the bridge, two water intakes for the St. Louis
Waterworks are visible. In the mid 1990s, a Bigfoot monster truck
drove over the "chain of rocks" located just downstream from the
Chain of Rocks Bridge.
A below water dam was built across the Mississippi River below
the Chain of Rocks to keep the river level high enough at the
upstream end of the canal to provide adequate flows/levels for
navigation within the canal. Just to the north of the Chain of
Rocks Bridge, the Missouri River flows into the Mississippi. The
site where these two rivers come together (confluence) was once
located on private property, but is now open for all to see thanks
to the Missouri Department of Conservation. Several trail routes to
the confluence are available from the conservation area parking
lot. The shortest route is about six miles round trip on flat
land.
Confluence of the Mississippi and Ohio Rivers is located at
Cairo, Illinois. The Missouri River flows from the confluence of
the Jefferson, Madison, and Gallatin to the Mississippi River.
Taken together, the Jefferson, the Missouri, and the Mississippi
form the longest river system in North America. If measured from
the source of the Jefferson at Brower's Spring, to the Gulf of
Mexico, the length of the Mississippi-Missouri-Jefferson
combination is approximately 3,900 miles, making the combination
the 4th longest river in the world. The uppermost 207 miles of this
combined river are called the Jefferson, the lowest 1,352 miles are
part of the Mississippi, and the intervening 2,341 miles are called
the Missouri.
It is a unique opportunity to be able to see two of the
world’s largest rivers combining. The water in the Missouri
River flows about 3,740 miles from its headwaters in Montana
through the Mississippi River and into the Gulf of Mexico. This
combined waterway is the world’s third longest with the Nile
and Amazon ranking first and second respectively. This feature also
owes its existence to the continental ice sheets covering North
America during the last ice age. Before this time, the Missouri
River used to flow through Canada and into the Hudson Bay. The
Missouri River’s modern day course is a good rough indicator
of the southernmost advance of the continental ice sheets.
The Mississippi River is the second longest river in the United
States, with a length of 2,340 miles from its source in Lake Itasca
in Minnesota to its mouth in the Gulf of Mexico. The longest river
in the United States is a Mississippi tributary, the Missouri
River, measuring 2,540 miles. The Mississippi River is part of the
Jefferson-Missouri-Mississippi river system, which is the largest
river system in North America and among the largest in the world:
by length, 3,900 miles, it is the fourth longest, and by its
average discharge of 572,000 cu ft/s, it is the tenth largest
river.
The Mississippi River runs through 10 states and was used to
define portions of these states' borders. The middle of the
riverbed at the time the borders were established was the line to
define the borders between states. The river has since shifted, but
the state borders of Wisconsin, Iowa, Illinois, Missouri, Kentucky,
Arkansas, Tennessee, and Mississippi have not changed; they still
follow the former bed of the Mississippi River as of their
establishment. The source of the Mississippi River is Lake Itasca,
1,475 ft above sea level in Itasca State Park located in Clearwater
County, Minnesota.
The uppermost lock and dam on the Mississippi River is the Upper
St. Anthony Falls Lock and Dam in Minneapolis, Minnesota. Above the
dam, the river's elevation is 799 feet. Below the dam, the river's
elevation is 750 feet. This 49-foot drop is the largest of all the
Mississippi River lock and dams. By the time the river reaches St.
Paul, Minnesota, below Lock and Dam #1, it has dropped more than
half its original elevation and is 687 feet above sea level. From
St. Paul to the Gulf of Mexico the river elevation falls much more
slowly and is controlled and managed as series of pools created by
locks and dams.
The Mississippi River empties into the Gulf of Mexico about 100
miles downstream from New Orleans. Measurements of the length of
the Mississippi from Lake Itasca to the Gulf of Mexico vary
somewhat, but the United States Geological Survey's number is 2,340
miles. The retention time from Lake Itasca to the Gulf is about 90
days. The Mississippi River discharges at an annual average rate of
between 200,000 and 700,000 cubic ft/s. On average, the Mississippi
has only 9% the flow of the Amazon River but is nearly twice that
of the Columbia River and almost 6 times the volume of the Colorado
River.
Many of the works of Mark Twain deal with or take place near the
Mississippi River. One of his first major works, Life on the
Mississippi, is in part a history of the river, in part a memoir of
Twain's experiences on the river, and a collection of tales that
either take place on or are associated with the river. Twain's most
famous work, Adventures of Huckleberry Finn, is largely a journey
down the river.
The Mississippi River probably has more nicknames than any other
river. Mississippi means "large river" to the Chippewa Indians. It
is called Big Muddy (also commonly used for the Missouri), Big
River, Body of a Nation, El Grande, El Grande de Soto, the Father
of Waters, the Gathering of Waters, the Great River, the Mighty
Mississippi, the Muddy Mississippi, Old Man River, etc. This
Earthcache is dedicated with much love to my dad, John Haslock, for
knowing all of those nicknames & for taking me to Cairo,
Illnois when I was young - even if I didn't even undertsand then
why he chose such an odd place to go on vacation. I am still not
sure why we drove a couple hundred extra miles to visit an old
slave house, but, besides my dad having some similarities to Clark
Grizwold, I am sure that destination had a purpose as well.
NOTICE:
For additional details on the Route 66 project
(plans, thoughts, template, etc) or to participate and create Route
66 caches along the "Mother Road" in your area, visit our site at
www.route66geocaching.org. (visit
link). . |