Ohio History Journal




SOME OHIO BOWLDERS

SOME OHIO BOWLDERS.

 

 

E. L. TAYLOR.

In the Ohio State Archaeological and Historical Quarterly,

July, 1905, Mr. Basil Meek gave an interesting sketch of "A

Rock With a History." This bowlder is found in Sandusky

county seven miles southwest of the city of Fremont. The arti-

cle referred to has induced me to give a short account of three

large granite bowlders found in Franklin county and near the

city of Columbus.

The first of these is located in the bottom of a ravine, or

rather the bed of a run, which comes from the west and empties

into the Scioto river about three miles west from the center of

the city of Columbus. The bed of the run at this point is about

one hundred and fifty yards in width and the bowlder is near

the middle of the bed. It is on what is now the "State Hospital"

grounds and to the north and west of the main building about

a quarter of a mile. The late Dr. Edward Orton, who made the

geological report of Franklin county, told me that it was the

largest bowlder in Franklin county, and, perhaps, in this part

of the State, of which he had knowledge. This corresponds with

my own observation. There are granatic bowlders almost innu-

merable scattered over all parts of Franklin county. A great

many of them are comparatively small, but many of them are

large and vary in their composition to a very considerable extent.

There is perhaps not a farm of any extent in the county where

they are not found. In some places they are so numerous as to

be quite a hindrance to the cultivation of the land, and thousands

of them have been removed by the owners of the soil in order

that they might better cultivate their farms. As we have said,

this particular bowlder is the largest of them all insofar as we

have knowledge or information.

We give herewith a diagram showing its outline above the

ground. The bowlder is 49 feet around at the base and at the

(155)



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highest point is 71/2 feet high. No digging was done to ascertain

what portion was beneath the soil, but the conformation of the

bowlder would indicate that at least one-half, if not more, is under

ground. If that estimate is correct, the whole weight of the bowl-

der would be in the neighborhood of from 80 to 100 tons, and this,

we think, to be a fair estimate. The bowlder shows evidence of

very considerable disintegration. When it was first dropped at

that point it was probably very materially larger than at the

present time, and must have been seventy-five or more feet above

its present position. The geological formation at that point was

Devonian limestone, and this bowlder was necessarily deposited

there in the age of "floating ice" and long prior to the beginning

of the formation of the Scioto river and its branches.  The lit-

tle valley in which this bowlder now reposes is at least seventy-

five or more feet below the upper strata of the limestone as it

was at the time the bowlder was deposited. Since that time the

Scioto river has worn its way down through the limestone forma-

tion to its present level, and the numerous streams and ravines

which lead into it have also been formed since that remote period.



Some Ohio Bowlders

Some Ohio Bowlders.               157

 

It so happens that a dry run which drains the country west of it

for two or three miles found its way to the river on a line where

this bowlder was deposited. The bowlder is not many feet above

high water-mark on the Scioto, and less than a half mile from it.

We give herewith the outline as photographed in October, 1905.

This photograph was kindly furnished by Dr. George Stockton,

Superintendent of the State Hospital. The measurements were

made by Major A. D. Rogers of Columbus, Ohio, and are as

follows:

BOWLDER NO. 1.

Circumference   at   ground ..............................  49'

H eight  . .                ...................................  7 1/2'

 

 

BOWLDER NO. 2.

There is another very interesting bowlder to be found almost

directly northeast across the Scioto river about one mile from

No. 1. It is on the east side of the Scioto river in a precinct or

district called Grandview. Singularly enough it is just at the mouth

of a deep and narrow ravine where it opens out into the bottom



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lands of the Scioto. This bowlder is interesting both for its size

and its unusual height. Like No. 1, it is much larger at the

ground than at any point above. In height it exceeds any bowlder

in Franklin county of which we have knowledge. Like No. 1,

this great bowlder has sunk down from its original position, prob-

ably seventy-five or more feet, as the elements have worn away

the limestone during the long period which has elapsed since the

water went away and the Scioto river began to take its form and

cut its way down through the limestone formation. From appear-

ances of the bowlder it would seem that a very large proportion

of it was hidden underground. No digging has been made to

ascertain what is below the surface, but there certainly must

be at least one-third and probably one-half of the bowlder hidden

beneath the soil. The dimensions of this bowlder, by actual



Some Ohio Bowlders

Some Ohio Bowlders.                        159

 

measurement, made by Henry C. Taylor in October, 1905, are as

follows:

M easure      at         surface                     .................................                                          30'     4"

1/4  distance  from    base...............................                          29'     10"

2/3 distance from base.............   .........                                      23'     4"

Circumference  of  top ...............................                            20'     5"

H eight  ............................................                                                                                    10'         5"

 

BOWLDER NO. 3.

This bowlder is east from the center of the city of Columbus

about five miles and is about three hundred yards north of the

line of the old National road. It is in plain sight from the road.

It is situated entirely different from No. 1 and No. 2. It stands on

the great level which extends from Alum creek to Walnut creek,

and is about half way between them. The region round about is

very flat and level in every direction, and there are no streams



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small or large anywhere near it. It rests on a bed of clay which

overlies a heavy slate formation (Devonian shale), which is from

fifteen to twenty feet below the surface. The peculiarity of this

bowlder is that it is slightly smaller at the ground surface than

it is two or three feet above the surface. It is very symmetrical

in form, and while not so large as either No. 1 or No. 2 is never-

theless a very interesting bowlder.      The measurements are as

follows:

Circumference at the ground........................ 29'                      5"

Circumference half way from base to summit........ 30'                                                 5"

Circumference near top ............................                                                                          24'        7"

H eight  ............................................                                                                                      6'          4"

All of these bowlders are on almost a line from east to west,

and all of the same composition and probably came from the same

locality, and probably near the same period of time. If a line were



Some Ohio Bowlders

Some Ohio Bowlders.                161

drawn from No. 1 to No. 3, from east to west, they would all be

within a quarter of a mile of a straight line, No. 2 being slightly

to the north of the line. They are all within one-half mile of the

line of the National road.

This bowlder has escaped injury at the hands of thoughtless

persons, while No. 1 and No. 2 have both suffered severely by

having large pieces pried or thrown off from them where time

and the elements have opened seams in the bowlders which made

the mutilation possible. Large pieces are lying around the base

of each of these bowlders which could only have been detached or

removed by human agencies. It is greatly to be hoped that this

has not been the case in other places where large bowlders are

found. They are by far the oldest monuments or landmarks that

we have, having been brought here by the mighty agency of float-

ing ice long before the waters subsided and the dry earth appeared

in this region. They have been silent witnesses of the mighty

changes and transformations which have taken place around them

in the formation of hills and valleys and other changes in the sur-

face of the earth in this region during the vast period of time

which has intervened between the close of the Ice Age anti the

present time, and it would seem they should be exempt from

mutilation at human hands, as they were brought here long before

human life or animal life was possible in this region.

That there are larger bowlders of like nature within the bor-

ders of the state, there is no doubt; perhaps many of them. Prof.

E. B. Andrews, who made the geological report of Fairfield

county, says (Geological Survey, 1870, page 58):

"The forces which carried bowlders and gravel were evi-

dently exerted in an unusual degree through all the eastern part

of Fairfield county. A bowlder near the roadside a few miles

northeast of Lancaster, is the largest I have met with in the State.

Most of it is buried, but judging from the exposed part I should

infer that it might weigh one hundred tons."

Prof. John Hussey in his report (Vol. III, Geological Sur-

vey, Ohio, page 437) says:

"The largest bowlder perhaps which is found so far south in

this state is found in Clinton county on the county infirmary farm

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near Wilmington, and this lies on a fine-grained clay upon which

it would seem to have fallen by washing away of the clay in which

it was formerly imbedded, and which, at a higher level, lies near it

on all sides. This bowlder contains about 1,200 cubic feet and

weighs upwards of ninety tons."

In the same report (Vol. III, page 462) Prof. Hussey says:

"While the transported rocks do not constitute a marked

feature in Shelby county, still there are many of them. .

The largest bowlder, however, that has, as yet, come under my

observation in the state, lies near the railroad one mile east of

Sidney. It contains 1,250 cubic feet, and weighs one hundred

and three tons."

Prof. Edward Orton in his report of the geology of War-

ren county (Geological Survey, Vol. III, page 389) cays:

"Bowlders, of northern origin, are everywhere distributed

through the county. There are several of unusual size, and one

of them deserves especial notice. It is found three miles to the

southeast of Lebanon. The bowlder is composed of gneiss - in

which rose colored felspar is a large element-a composition

shared by most of the largest erratics of the region. It weathers

very rapidly, and must have had considerably greater dimensions

at an earlier day. It now measures above ground seventeen feet

in length, thirteen feet in breadth, and eight foot in height. Ex-

amination shows it to be sloping outwords under ground in all

directions. It is fair to conclude that at least one-half of it lies

buried. Its weight above ground will not fall below one hundred

and forty tons."

The weight of this bowlder as here given is greater than

that of any in the State so far as I am informed. But a com-

parison of its measurements with Bowlder No. 1 heretofore men-

tioned, shows that there is no great difference in their bulk, so

that Bowlder No. 1 may properly be classed among the largest

of these erratics from the far off Canadian highlands in the

State insofar as they have been observed.

Columbus, Ohio.