DESCRIPTION OF THE PLATE.

We are indebted to Photography for enabling us to represent the

remarkable slab from Greenfield, and its numerous objects, in a small

space, yet with perfect accuracy. This slab is four feet seven and

one-half inches in one direction, and four feet one inch transversely

to this; in thickness it measures about an inch. It is composed of

gray sandstone, in which the micaceous element is conspicuous, and

contains many interesting impressions on both surfaces.

The most interesting surface is the inferior; and the objects are, of

course, presented in relief. They are, first, two Chelonian tracks;

second, four sets of bird-tracks; third, footsteps of an unknown

animal. The _Chelonian tracks_ are two in number: the longest measures

four feet ten inches; the shorter, two feet nine inches. Both of these

impressions are made apparently by the plastron of the turtle. They

are from four to eight inches in width, and composed of elevated

striae. These striae are formed by raised lines, pursuing a course

generally regular, but accompanied with some inflections: they are, as

the plate represents, very distinct. The shorter track appeared to me

to be crossed by another; but the photographic impression, though only

a few inches long, enabled me to ascertain that this appearance was

produced by bird-tracks above and below.

The _bird-tracks_ are all tridactylous. The first set lies above and

to the right of the shorter turtle-track, and is composed of only two

steps, proceeding in the course of the plate downwards. The second set

of bird-tracks has five impressions, extending from the right superior

pointed angle of the slab across the small turtle-track to the larger,

in which it is lost. The third set of bird-tracks begins by an

impression larger than any other on the piece at the left extremity of

the longer turtle-track; and the remainder, three in number,

descending towards the right, are the least distinct of any. The

fourth set of bird-tracks begins below the longer turtle-track, and

ascends by four impressions, crossing the track till it meets the

first.

The most curious track, consisting of six digitated impressions, still

remains. The first is seen on the left of the longer turtle-track,

near the largest bird-track; the second is on the track; the third is

above the track; the others cross the slab by fainter impressions.

Each of them is composed by two feet, and each foot contains four

toes, which are seen more distinctly in some impressions than in

others. The largest of these double tracks is about three inches in

diameter. Perhaps it would be useless to speculate upon what kind of

animal they were made by. There is a similarity between these and the

tracks of the Anomoepus Scambus, spoken of in the sixth group. In the

latter, however, the toes are five and three. Some experienced persons

think they are tracks of the mink, Mustela Lutreola, an animal common

at the present day in these parts. This has five toes; but it may be

in this as in some other digitigrades, that one of the toes in each

foot does not make an impression; or perhaps it is safer to believe,

till further investigation is made, that it was an animal of a

construction not now existing.

The direction of these tracks presents a puzzle we are not able to

unravel; it exhibits the impressions of four toes, and we have

supposed it might possess five. In either of these cases, we have no

right to consider it a bird-track, but probably a reptile or a mammal.

Admitting this to be the fact, we are unable to account for the

direction of the steps, which is not alternate, as in the quadruped,

but in straight lines. In other words, this animal, supposed to have

four legs, gives us the impressions of two only, and both of these

placed together.

When the tridactylous tracks are attentively considered, compared with

each other, and with the digitated tracks, they appear to exhibit the

character of the impressions of the feet of birds so very decidedly,

that it would require something more than a philosophic incredulity to

question their ornithic origin.

The other side of this slab contains interesting impressions. In the

first place, this surface is covered with ripple-marks, each about two

inches broad, extending with various degrees of distinctness across

the slab, and having an interval of an inch. The width of the ridges

is greater than in any of the specimens we have seen.

This surface is almost covered by rain-drops. It has also, among other

impressions, one which has been drawn by Mr. Silsbee, our

photographist, and represented by the figure below of its proper size.

This figure, nearly four and a half inches in length, is an exact

resemblance in form, but not in size, of the great Otozoum, as

depicted by President Hitchcock, and shown by the actual impression,

in our hands, of the great foot, twenty inches long, and of

proportionate breadth. The form of the heel, or posterior part of the

foot, is the same in the two figures; the toes are equal in both, viz.

four in number; the two internal toes correspond in their

articulations, and the two external are nearly alike, with a little

allowance for a different amount of adipose texture. Whether this was

the impression of an infant Otozoum, I pretend not to determine: the

drawing was taken by a gentleman who knew nothing of the Otozoum.

There are similar impressions, smaller than that last described, on

the same surface.

The stone, though now very hard and intractable, having resisted all

the chemical agents we could employ, must have remained in a soft

state for some time; for the impressions of the foot shown below

penetrate to the opposite surface.

[Illustration: Fossil foot impression]

In this description we have not attempted to point out all the objects

worthy of interest on both sides of this curious slab. Every part

of it is full of interest, and presents a field for protracted

observations. The surface represented in the plate may, by the aid of

a magnifier, be studied without the presence of the stone itself; for

the photographic art displays the most minute objects without

alteration or omission.

* * * * *

Transcriber's Notes.

With the exception of several presumed typographical error which have

been changed as noted below, the text presented is that shown in the

original printed version. The original text included Greek characters.

For this text version these letters have been replaced with

transliterations. Also, the 'AE' and 'ae' ligatures are included (for

examples, AEthyopus and striae); but the 'oe' ligatures (for example,

Anomoepus) are shown as 'oe' for readability as the ligature character

is not present in many fonts.

Typographical Errors:

"Alleghanies" => "Alleghenies" (Pg. 18)

"Mastodon Giganteus." => "Mastodon Giganteus," (Pg. 25)

Emphasis Notation:

_text_ - italicized

Remarks on some fossil impressions in the sandstone rocks of Connecticut River · 第 18 / 18 题