CHAPTER I

Early Western Travels

1748–1846

Volume XIII

Early Western Travels

1748–1846

A Series of Annotated Reprints of some of the best

and rarest contemporary volumes of travel, descriptive

of the Aborigines and Social and

Economic Conditions in the Middle

and Far West, during the Period

of Early American Settlement

Edited with Notes, Introductions, Index, etc., by

Reuben Gold Thwaites, LL.D.

Editor of “The Jesuit Relations and Allied Documents,” “Original

Journals of the Lewis and Clark Expedition,” “Hennepin’s

New Discovery,” etc.

Volume XIII

Nuttall’s Travels into the Arkansa

Territory, 1819

[Illustration: colophon]

Cleveland, Ohio

The Arthur H. Clark Company

1905

COPYRIGHT 1905, BY

THE ARTHUR H. CLARK COMPANY

ALL RIGHTS RESERVED

The Lakeside Press

R. R. DONNELLEY & SONS COMPANY

CHICAGO

CONTENTS OF VOLUME XIII

PREFACE. _The Editor_ 11

A JOURNAL OF TRAVELS INTO THE ARKANSA TERRITORY, during

the year 1819, with Occasional Observations on the

Manners of the Aborigines. _Thomas Nuttall, F.L.S._

Copyright Notice 24

Author’s Dedication 25

Author’s Preface 27

Author’s Table of Contents 31

Text 35

Appendix:

Section I. An Account of the Ancient Aboriginal

Population of the Banks of the Mississippi

and the Contiguous Country 319

Section II. The History of the Natchez 338

Section III. Observations on the Chicasaws

and Choctaws 353

Section IV. Thermometrical Observations in

the Arkansa Territory, during the year 1819 365

ILLUSTRATIONS TO VOLUME XIII

“A Map of the Arkansas River, by H. S. Tanner” 22

Facsimile of title-page to Nuttall 23

“Distant View of the Mamelle” 153

“Mamelle” 159

“Cadron Settlement” 163

“Magazin Mountain” 185

“Cavaniol Mountain” 203

PREFACE TO VOLUME XIII

The present volume of our series is devoted to a reprint of Thomas

Nuttall’s _Journal of Travels into the Arkansa Territory, during

the year 1819, with Occasional Observations on the Manners of the

Aborigines_, originally published at Philadelphia in 1821.

Nuttall was born in the market town of Settle, West Riding,

Yorkshire, in 1786.[1] His parents being in humble circumstances,

at an early age he was apprenticed to a printer, probably an uncle

who was a member of that craft, in Liverpool. After a few years,

becoming dissatisfied with his employer, he journeyed to London,

where his pecuniary condition approached so near to destitution that

he emigrated to the United States, arriving at Philadelphia in 1808,

aged twenty-two.

In spite of the disadvantages which had beset him in his early years,

a natural love for books and a faculty for application had by this

time given him some knowledge of history, Greek, and Latin, and

much of natural science, already his favorite study. Soon after his

arrival in Philadelphia, he was seeking information relative to a

plant which interested him, when he met Dr. Benjamin Smith Barton;

the interview stimulated him to the botanical studies on which

his fame as a scientist chiefly rests, and he soon began to make

excursions, especially along the seacoast as far south as North

Carolina. In 1810, he accompanied John Bradbury (whose _Travels_

comprise volume v of our series), on the latter’s scientific

expedition into the Missouri country, described in volume v of our

series.

Nuttall returned to Philadelphia early in 1811, and during the

succeeding eight years spent his summers in excursions within the

area east of the Mississippi, his winters being passed in studying

the collections thus acquired. The fruits of these studies appeared

in _The Genera of North American Plants and a Catalogue of the

Species to 1817_ (Philadelphia, 2 vols., 1818), for which he

personally set most of the type. Just before the appearance of this

work, Nuttall, who was already a member of the Linnæan Society of

London, was elected to membership both in the American Philosophical

Society and the Academy of Natural Sciences, at Philadelphia. To the

journal published by the Academy he became a frequent contributor.

Being well acquainted with the cis-Mississippi region, and having

already visited the Northwest, he now turned his thoughts to the

Southwest. He had long desired to visit the Arkansas country,

which still offered a practically virgin field for the scientific

investigator.[2] Accordingly, assisted by a number of friends who

were likewise interested in science,[3] he prepared for the journey

which is herein recorded, and set out from Philadelphia on the second

of October, 1818. Crossing southern Pennsylvania to Pittsburg, and

descending the Ohio and Mississippi by boat, he arrived at Arkansas

Post on January 22, 1819. Thence ascending the Arkansas River, he

reached the recently-founded Fort Smith on April 24. Here he remained

for three weeks, studying the flora of the vicinity. On May 16,

he set out from the post with the commandant, Major Bradford, and

a company of soldiers; and crossed the wilderness to Red River,

following the Poteau and Kiamichi. Near the mouth of the latter,

while loitering to collect some curious plants, he became separated

from his companions and was compelled to spend three weeks with the

squatters, awaiting the departure of a party for Fort Smith, where he

finally arrived after an absence of five weeks.

On July 6, Nuttall again left Fort Smith in the boat of a trader

whose establishment was situated at the mouth of Verdigris River.

Reaching this point on the fourteenth, nearly a month was spent

in making short trips to study the plant-life and geology of the

neighborhood, and in observing the habits of the Osage Indians.

On August 11, accompanied by a hunter for guide, he began the final

stage of his journey, having as its objective the river now called

Cimarron. At this season the streams were stagnant, and the intense

heat, foul water, poor food, and night dews soon brought on a fever,

which came near terminating our traveller’s career. The Indians,

moreover, were an almost constant source of annoyance and danger.

Nuttall rejected the guide’s suggestion of a return to the Verdigris,

and finally it became impracticable; so the two pushed on until the

Cimarron was reached. By this time his fever had somewhat abated, and

an effort was made to ascend that river. The loss of one of the two

horses, however, compelled the abandonment of the project, and a

canoe was built, in which the guide essayed to return by water while

his chief rode the remaining horse. Setting forth in this fashion,

still beset by Indians, who pilfered from them on every pretext, they

soon found that the horse could not keep pace with the boat. The two

travellers thereupon agreed to separate, and Nuttall completed the

journey to the Verdigris alone, arriving, more dead than alive, on

September 15. For a week he was unable to proceed farther; at Fort

Smith another long halt was necessary, but on October 16 he began

the descent of the Arkansas, and reached New Orleans on February 18,

1820, without further mishap.

Two years later, Nuttall was appointed curator of the botanical

garden of Harvard College. He spent several years at Cambridge

cultivating rare plants, pursuing his studies, and delivering

occasional lectures. These years were fruitful in contributions

to _Silliman’s Journal_, the _Journal_ of the Academy of Natural

Sciences, the _Transactions_ of the American Philosophical Society,

and the _American Journal of the Medical Sciences_.[4] A little later

appeared his _Introduction to Systematic and Physiological Botany_,

and at about the same time he produced the _Manual of the Ornithology

of the United States and Canada_ (Part I, Land Birds, Cambridge,

1832; Part II, Water Birds, Boston, 1834). The life at Cambridge

was, however, distasteful to him; he declared that he was, like his

plants, only vegetating. His instincts and habits drew him to the

wilderness, that he might unravel its secrets. About the beginning

of 1833, he had received a collection of plants gathered by Captain

Nathaniel Jarvis Wyeth during a journey overland to Oregon. With

interest in the far Northwest thus quickened, Nuttall joined Wyeth

when he set out on a second expedition,[5] resigning his position

at Harvard when the college authorities refused to grant a leave of

absence. He was accompanied by John K. Townsend, as representative

of the Philosophical Society and the Academy of Natural Sciences.

The party rendezvoused at Independence, Missouri, and began the long

march on April 28, 1834. Nuttall and Townsend passed the autumn

exploring the environs of Fort Vancouver; but as winter drew near,

they embarked on a Boston brig bound for the Sandwich Islands, where

they arrived January 5, 1835. Two months later, leaving Townsend,

Nuttall sailed to the California coast, where he passed the summer,

returning thence to the Sandwich Islands and embarking for Boston

by way of Cape Horn, on board the vessel whose cruise has been made

famous by Dana’s _Two Years before the Mast_.

Upon reaching the United States, Nuttall resumed his abode in

Philadelphia. In 1840, the results of the Pacific journey were

published in the _Transactions_ of the Philosophical Society, in the

form of two long essays, entitled: “Descriptions of new species and

genera of plants in the natural order Compositæ, collected in a tour

across the continent to the Pacific, a residence in Oregon, and a

visit to the Sandwich Islands and California, in the years 1834 and

1835;” and “Description and notices of new and rare plants of the

natural orders Lobeliaceæ, Campanulaceæ, Vacciniceæ and Ericaceæ,

collected in a journey across the continent of North America, and

during a visit to the Sandwich Islands and Upper California.”

Nuttall’s last work, _The North American Sylva; or a Description

of the Forest-Trees of the United States, Canada and Nova Scotia,

not described in the work of François André Michaux_ (Philadelphia,

3 vols., 1842–49), was, as the title indicates, undertaken as a

supplement to the earlier work of Michaux.[6] It was completed on

the eve of his departure from the United States, and entrusted to

a friend for publication. Part one of the first volume appeared in

1842, and the second part the following year. The remaining volumes

were delayed by various causes, not being printed until 1846 and

1849, respectively.

In 1841, by the bequest of an uncle, Nuttall received the estate of

Nutgrove, near Liverpool, with the accompanying condition that during

the remainder of his life he reside in England at least nine months

of each year. Reluctantly leaving the land of his adoption and the

field of his labors, impelled, it is said,[7] by regard for the needs

of his sisters’ families, he retired to the ancestral estate, which

he largely devoted to the cultivation of rare plants. He revisited

America in 1847–48; by taking three months at the end of the first

year and three at the beginning of the next, he was able to spend

six consecutive months outside of England without infraction of the

terms of his relative’s will. After seventeen years of the simple

farm life which both his disposition and circumstances required, his

death came, September 10, 1859, as the result of overstraining in his

eagerness at unpacking a case of plants which had been sent to him

from Asia.

Nuttall’s natural shyness was enhanced by the character of his

studies, so largely pursued in the solitude of the field or forest.

Both in Cambridge and Philadelphia, his circle of acquaintance was

quite small; even his intimates in Philadelphia declaring that they

knew not the place of his residence--his intercourse with them was

largely in their homes. Of a contemplative mind, his manner was often

abstracted, yet with those of like interests he was companionable

and communicative. His head was large and bald, his forehead broad,

his features small; he was fair of feature, and often pale from

application to his work; and stout and slightly stooped of frame,

but above middle height. The story of his explorations proves him

to have been of an active temperament. A persistent worker, his

enthusiasm was unlimited. “To me,” he said, “hardships and privations

are cheaply purchased, if I may but roam over the wild domain of

primeval nature.... My chief converse has been in the wilderness

with the spontaneous productions of nature; and the study of these

subjects and their contemplation have been to me a source of constant

delight.” Several anecdotes are related, which illustrate his ardor.

On one of his early excursions to the Carolina coast, he was badly

bitten by mosquitoes; but, absorbed in his investigations, was

unconscious of the presence of the insects until, upon approaching

a dwelling, he was thought to be afflicted with small-pox, and

well-nigh driven away. When rounding Cape Horn, with the vessel beset

by wind and icebergs, he vainly pleaded with the captain to be set on

shore if only for a few hours, that he might examine the vegetation

of that little-known coast.[8]

Nuttall will chiefly be remembered as a man of science. His work was

painstaking, and he made solid contributions to the knowledge of his

generation. Nor was he in his own lifetime denied his meed of praise,

especially for his botanical work. Contemporary reviews of his

books were usually appreciative; a fellow-member[9] of the American

Philosophical Society left this testimony: “No other explorer of the

botany of North America has, personally, made more discoveries; no

writer on American plants, except perhaps Professor Asa Gray, has

described more new genera and species. His name will live as long as

our Flora remains an object of study.”

The journal of the Arkansas journey, reprinted in the present volume,

while primarily interesting to the scientist is not without value

for the historian. The author was fairly well acquainted with the

principal printed accounts of Spanish and French exploration in

the region, as well as with the reports of the previous American

visitors. But Nuttall’s historical statements are not invariably

accurate; the value of the work lies in the record of his personal

observations, from which we obtain often graphic descriptions of

the settled portions of the Arkansas country and the state of

civilization prevalent there in 1819. Neither does our author neglect

the Indians, in whom he was much interested. His book ranks high as

a source of information regarding the native tribes of that region,

especially the Quapaw; although such of his information as was

obtained second hand needs the corrective of critical study.

In the preparation of this volume for the press, the Editor has had

the assistance of Homer C. Hockett, fellow in American history in the

University of Wisconsin.

R. G. T.

MADISON, WIS., February, 1905.

FOOTNOTES:

[1] The chief source of information concerning Nuttall’s life is

a “Biographical Notice” prepared upon his death by Elias Durand,

for the American Philosophical Society, and published in their

_Proceedings_ for 1859–60 (volume viii, p. 297). Other details are

given in his writings, especially the _Journal_, and in Bradbury and

Townsend, who were his associates on other expeditions (see volumes v

and xxi of our series).

[2] The expeditions of William Dunbar and Dr. George Hunter, who

explored the Ouachita as far as Hot Springs in 1804, under a

commission from President Jefferson, and of Lieutenant James B.

Wilkinson, who descended the Arkansas River under General Z. M.

Pike’s orders in 1806, were primarily geographical and topographical

reconnaissances.

[3] This fact, and the names of Nuttall’s patrons, appear in the

dedication.

[4] For full titles of the numerous essays, see the sketch of his

life, referred to in note 1, _ante_.

[5] Wyeth’s expedition was dispatched for the purpose of establishing

trading posts for the Columbia Fishing and Trading Company.

[6] _Histoire des arbres forestiers de l’Amérique du Nord_ (Paris

(?), 4 vols., 1810–13); translation by Augustus L. Hillhouse, _North

American Sylva, or a description of the forest trees of the United

States, Canada and Nova Scotia_ (Paris, 3 vols., 1819).

[7] See the Durand Memorial.

[8] Dana, _Two Years Before the Mast_, quoted by Durand.

[9] Elias Durand, in sketch already cited.

NUTTALL’S JOURNAL OF TRAVELS INTO THE ARKANSA

TERRITORY

OCTOBER 2, 1818–FEBRUARY 18, 1820

Reprint of the original edition: Philadelphia, 1821

[Illustration:

_A Map of the_

ARKANSAS RIVER,

_intended to illustrate the Travels of

THOˢ. NUTTAL_;

Constructed from his original manuscripts by

_H. L. Tanner_

]

[Illustration: Facsimile of title page]

A

JOURNAL

OF

TRAVELS

INTO THE

ARKANSA TERRITORY,

DURING THE YEAR

1819.

WITH OCCASIONAL OBSERVATIONS ON THE MANNERS Of THE

ABORIGINES.

ILLUSTRATED BY A MAP AND OTHER ENGRAVINGS.

BY THOMAS NUTTALL, F. L. S.

HONORARY MEMBER OF THE AMERICAN PHILOSOPHICAL SOCIETY, AND OF

THE ACADEMY OF NATURAL SCIENCES, &C.

PHILADELPHIA:

PRINTED AND PUBLISHED BY THOS. H. PALMER.

1821.

EASTERN DISTRICT OF PENNSYLVANIA, to wit:

[Sidenote: [L. S.]]

BE IT REMEMBERED, That on the sixth day of November, in the

forty-sixth year of the independence of the United States of America,

A.D. 1821, Thomas H. Palmer, of the said District, has deposited in

this office, the title of a book, the right whereof he claims as

proprietor, in the words following, to wit:

“A journal of Travels into the Arkansa Territory, during the year

1819, with occasional observations on the manners of the Aborigines.

Illustrated by a map and other engravings. By Thomas Nuttall, F.L.S.

Honorary member of the American Philosophical Society, and of the

Academy of Natural Sciences, &c.”

In conformity to the act of the Congress of the United States,

entitled, “An Act for the encouragement of learning, by securing the

copies of Maps, Charts, and Books, to the authors and proprietors of

such copies during the times therein mentioned.”--And also to the

Act, entitled, “An Act supplementary to an act, entitled, “An act

for the encouragement of learning, by securing the copies of Maps,

Charts, and Books, to the authors and proprietors of such copies

during the times therein mentioned,” and extending the benefits

thereof to the arts of designing, engraving, and etching historical

and other prints.”

D. CALDWELL,

Clerk of the Eastern District of Pennsylvania.

TO

JOSEPH COREA DE SERRA,

MEMBER OF THE NATIONAL INSTITUTE OF FRANCE, OF THE

ROYAL SOCIETY OF LONDON, &C.

ZACCHEUS COLLINS, ESQ.

MEMBER OF THE AMERICAN PHILOSOPHICAL SOCIETY, AND

VICE-PRESIDENT OF THE ACADEMY OF NATURAL

SCIENCES, &C.

WILLIAM MACLURE, ESQ.

PRESIDENT OF THE ACADEMY OF NATURAL SCIENCES, AND

MEMBER OF THE AMERICAN PHILOSOPHICAL

SOCIETY, &C. &C.

JOHN VAUGHAN, ESQ.

TREASURER AND LIBRARIAN OF THE AMERICAN PHILOSOPHICAL

SOCIETY, MEMBER OF THE ACADEMY

OF NATURAL SCIENCES, &C. &C.

_Gentlemen_,

Permit me to lay before you, the humble narrative of a journey,

chiefly undertaken for the investigation of the natural history of

a region hitherto unexplored. Excuse the imperfect performance of

the gratifying task which your liberality had imposed, but which was

rendered almost abortive by the visitations of affliction.

If, in so tiresome a volume of desultory remarks, you should meet

with some momentary gratification, some transient amusement, or ray

of information, the author will receive the satisfaction of not

having laboured entirely in vain.

PREFACE

To those who vaguely peruse the narratives of travellers for pastime

or transitory amusement, the present volume is by no means addressed.

It is no part of the author’s ambition to study the gratification

of so fastidious a taste as that, which but too generally governs

the readers of the present day; a taste, which has no criterion but

passing fashion, which spurns at every thing that possesses not the

charm of novelty, and the luxury of embellishment. We live no longer

in an age that tolerates the plain “unvarnished tale.” Our language

must now be crowded with the spoils of those which are foreign to its

native idiom; it must be perplexed by variety, and rendered ambiguous

and redundant by capricious ornament. Hermes, no longer the plain

messenger of the gods, exercises all his deceit, and mingles luxury

in the purest of intellectual streams.

Had I solely consulted my own gratification, the present volume

would probably never have been offered to the public. But, as it

may contain some physical remarks connected with the history of

the country, and with that {vi} of the unfortunate aborigines, who

are so rapidly dwindling into oblivion, and whose fate may, in

succeeding generations, excite a curiosity and compassion denied

them by the present, I have considered myself partly excused in

offering a small edition to the scientific part of the community,

just sufficient to defray the expenses of the printer, who kindly

undertook the publication at his own risk. I may safely say, that

hitherto, so far from writing for emolument, I have sacrificed both

time and fortune to it. For nearly _ten_ years I have travelled

throughout America, principally with a view of becoming acquainted

with some favourite branches of its natural history. I have had no

other end in view than personal gratification, and in this I have

not been deceived, for innocent amusement can never leave room for

regret. To converse, as it were, with nature, to admire the wisdom

and beauty of creation, has ever been, and I hope ever will be, to me

a favourite pursuit. To communicate to others a portion of the same

amusement and gratification has been the only object of my botanical

publications; the most remote idea of personal emolument arising from

them, from every circumstance connected with them, could not have

been admitted into calculation. I had a right, however, reasonably

to expect from Americans a degree of candour, at least equal to that

which my labours had met with in Europe. But I have found, what,

indeed, I might have {vii} reason to expect from human nature, often,

instead of gratitude, detraction and envy. With such, I stoop not to

altercate; my endeavours, however imperfect, having been directed to

the public good; and I regret not the period I have spent in roaming

over the delightful fields of Flora, in studying all her mysteries

and enigmas, if I have, in any instance, been useful to her cause, or

opened to the idle wanderer one fruitful field for useful reflexion.

Not wishing to enlarge the present publication, or retard it by the

addition of a voluminous appendix, I reserve for a subsequent volume,

which will shortly be issued, _A general view and description of the

aboriginal antiquities_ of the _western states_, and _some essays

on the languages of the western Indians_, and their connection with

those of other parts of the world, involving, in some measure, _a

general view of language, both oral and graphical_.

The surveys and collections towards a history of the aboriginal

antiquities, have remained unpublished in my possession for several

years, and would have been longer withheld, in hopes of rendering

them more complete, had not an unexpected anticipation obliged the

author to hasten to do justice to himself, and claim, at least, that

which was due to his personal industry.

The aboriginal languages of America, hitherto so neglected and

unjustly consigned to oblivion as the useless relics of barbarism,

are, {viii} nevertheless, perhaps destined to create a new era in the

history of primitive language. In their mazes is infolded a history

of morals, of remote connections, of vicissitudes and emigrations,

which had escaped the circumstantial pen of history; and yet, however

strange it may appear, are more durably impressed than if engraven

upon tablets of brass, and possessed of an intrinsic veracity nothing

short of inspiration.

The literary character of the aboriginal languages of America, have,

of late years, begun to claim the attention of the learned both in

Europe and America. The reports and correspondence of the Historical

committee appointed by the American Philosophical Society, stand

meritoriously preeminent in this research; and it must be highly

gratifying to the public to know, that the same members continue

still to labour in the field with unabated vigour. These various

efforts united, I may venture to predict, will be crowned with

successful discoveries which could not have been anticipated, and

which will ultimately contribute towards the development of that

portion of human history, which, above all others, appeared to be so

impenetrably buried in oblivion.

_Philadelphia, November, 1821._

CONTENTS

CHAP. I.--Departure from Philadelphia. Geological remarks. Route

through Harrisburgh and Carlisle to Cammel’s town. Loudon, and

the adjacent mountain scenery. The North Mountain. Cove Mountain.

Passage of the Juniata, and surrounding scenery. Bedford. Organic

remains. The Alleghany Ridge. Stoy’s-town. First indications of

bituminous coal. Laurel Mountain. Greensburgh. Arrival at Pittsburgh;

manufactures; scenery, and peculiar character of its coal-mines.

CHAP. II.--Departure from Pittsburgh. Autumnal scenery. Georgetown.

The unfortunate emigrant. Steubenville. Picturesque scenery.

Wheeling. Little Grave creek, and the Great Mound. Other aboriginal

remains. Marietta. Belpré settlement. Other ancient remains. Coal.

Galliopolis. Ancient level of the alluvial forest. Misletoe.

Aboriginal remains. Big Sandy creek, and commencement of Cane-land.

Corn-husking. Salt creek. Maysville. Organic remains. Cincinnati.

Lawrenceburgh. The French emigrant. Vevay. Madison. Louisville.

Prevalence of particular winds on the Ohio. Falls of the Ohio.

CHAP. III.--Departure from Shippingsport. Velocity of the current.

Troy. Owensville. Indigence of the hunting emigrants. Mounds.

Evansville. The Diamond island. Shawneetown. Grandeur of the

river, and the uncultivated state of the surrounding country. Fort

Massac. Arrival at the mouth of the Ohio. Delayed by the ice of the

Mississippi. {x} A visit from the Delaware and Shawnee Indians.

Observations on their mutual jealousy and improvidence.

CHAP. IV.--Embark amidst the ice of the Mississippi. Run aground on

Wolf’s island in attempting to land. Relieved from this situation,

but find ourselves again involved in it, and are imposed upon by the

extortion of a neighbouring voyager. Pass the Iron banks. Cypress.

Solitude of the country. New Madrid. Oscillations of the earth still

frequent. Point Pleasant. Vestiges of the great earthquake. The

Little Prairie settlement almost destroyed by it. The Canadian reach.

A dangerous and difficult pass of the river. The first Chickasaw

Bluffs. Additional danger and uncertainty of the navigation.

Stratification of the Bluff. A dangerous accident. The second

Chickasaw Bluffs. Observations on their stratification.

CHAP. V.--Pass the third Chickasaw Bluff. Dangers of the navigation,

and solitude of the country. The fourth Bluff of the Chickasaws.

Lignite prevalent. Chickasaw Indians. St. Francis river. Depopulation

of the neighbouring country. Trees of the alluvial forest.

Destruction of the Big Prairie settlement. Scrub grass. Difficulties

of the navigation. Changes of the soil, produced by the agency of the

river. A visit from three of the Arkansa Indians. A dense fog over

the river; the cause of it. Arrival near the mouth of the Arkansa and

White river.

CHAP. VI.--Proceed up White river for the Arkansa. Suspicious conduct

of one of the boatmen. Pass through the connecting bayou, and proceed

up the Arkansa; its navigation; soil and surrounding scenery. A small

French settlement. Extraordinary mildness of the season. Mounds.

Changes in the alluvial lands produced by the agency of the river.

Land speculators. Vegetation of the alluvial lands. The town or post

of Arkansas. Enormous land {xi} claims. Difficulty of navigating

against the current. The Great Prairie. First settlement on the

Arkansa; its present state. Agricultural advantages arising from the

mildness of the climate. Storax. Aboriginal remains. The Quapaws or

Arkansas. Their traditions and character.

CHAP. VII.--Departure from Arkansas. Indian villages. Mooney’s

settlement. Curran’s settlement. Interview with the Quapaw chief.

The Pine Bluffs. Soil, climate, and productions. The Little Rock.

Roads. Mountains. Vegetation. The Mamelle. Cadron settlement. Tumuli.

Soil and climate. Pecannerie settlement. Mountains. Cherokees. The

Magazine mountain. Dardanelle settlement. Manners and customs of the

Cherokees. The war with the Osages.

CHAP. VIII.--Pass several inconsiderable rivulets, and obtain sight

of the Tomahawk mountain and the Gascon hills. Mulberry creek; that

of Vache Grasse. Lee’s creek. Prairies. Sugarloaf mountain. Arrive at

the garrison of Belle Point. A change in the vegetation. The Maclura

or Bow-wood. The garrison. Cedar prairie. Rare plants.

CHAP. IX.--Journey to Red river. Prairies and mountains of the

Pottoe. Pass the dividing ridge. Kiamesha river. Arrival on the banks

of Red river. The murder of a Cherokee; attempts to obtain redress.

Wild horses. Character, geological structure, and rare vegetable

productions of the prairies. Return to the garrison at Belle Point.

CHAP. X.--Continue my voyage up the Arkansa. Geological remarks.

Pass several lesser rivulets, and the outlet of the Canadian and the

Illinois. Salt springs. Obstructions in the navigation. Indications

of coal. Pass Grand river, and enter the Verdigris.

CHAP. XI.--Character of the surrounding country of the Verdigris

river. Remarks on the Osage Indians.

{xii} CHAP. XII.--An excursion up Grand River to visit the Osage

salt works. Geological observations. Return across the prairie; its

general appearance and phenomena.

CHAP. XIII.--Interviews with the Osages. Occasional observations on

their manners, habits, &c. Sickness in the encampment.

CHAP. XIV.--Journey by land to the Great Salt river of the Arkansa.

Proceed across the prairies to the Little North Fork of the Canadian.

Detained by sickness. Continue up the Little North Fork, arrive at

Salt river, and afterwards at the Arkansa. Molested and pursued

by the Osages. Arrive again at the Verdigris, and proceed to the

garrison. Conclusion of the treaty between the Osages and Cherokees.

CHAP. XV.--Proceed from the garrison to the Pecannerie settlement.

Hot springs of the Washita. Phenomena of the seasons.

CHAP. XVI.--Cadron settlement. Arrive at Arkansas. Continue to the

Mississippi. The wandering fanatics. Pirates. Natchez; stratification

of its site, and remarks on its agricultural productions. The

Choctaws. Fort Adams. Point Coupé. Baton Rouge. Opulent Planters.

New-Orleans.

APPENDIX

SECT. I.--An account of the ancient aboriginal population of the

banks of the Mississippi, and the contiguous country.

SECT. II.--The history of the Natchez.

SECT. III.--Observations on the Chicasaws and Choctaws.

SECT. IV.--Thermometrical observations in the Arkansa Territory,

during the year 1819.

A JOURNEY INTO THE INTERIOR OF

THE ARKANSA TERRITORY

CHAPTER I

Departure from Philadelphia--Geological remarks--Route through

Harrisburgh and Carlisle to Cammel’s-town--Loudon, and

the adjacent mountain scenery--The North Mountain--Cove

Mountain--Passage of the Juniata, and surrounding

scenery--Bedford--Organic remains--The Alleghany

Ridge--Stoy’s-town--First indications of bituminous coal--Laurel

Mountain--Greensburgh--Arrival at Pittsburgh; manufactures;

scenery, and peculiar character of its coal mines.

On the morning of the second of October, 1818, I took my departure

from Philadelphia in the mail stage, which arrived safely in

Lancaster, sixty-three miles distant, a little after sun-set. Though

always pleasingly amused by the incidents of travelling, and the

delightful aspect of rude or rural nature, I could not at this time

divert from my mind the most serious reflections on the magnitude and

danger of the journey which now lay before me, and which was, indeed,

of very uncertain issue.

{10} Scarcely any part of the United States presents a more

beautiful succession of hill and dale, than that which succeeds

between Philadelphia and Lancaster; the valley, however, of Chester

county, including Downingston, exceeds every other, except the

site of Lancaster, in fertility and rural picture. It is about

twenty-five miles in length by one in breadth, and pursues from

hence a north-east direction. The rock throughout this valley is

calcareous, and the soil is consequently of a superior quality. This

lime-stone, which has been assiduously examined by the mineralogists

and naturalists of Philadelphia, though not very dissimilar to that

of the western states, except in the high inclination of the strata

and the predominance of spar, has never yet been found to contain any

kind of organic remains, and scarcely any metals more than traces of

iron, manganese, titanium, and lead.

3d.] From Lancaster, I continued my route on foot, as affording

greater leisure, and better opportunity for making observation.

The rain, however, to-day prevented me from proceeding more than

seventeen miles on the road to Harrisburgh.[1] About twelve miles

east of Middleton, I had again occasion to observe certain ledges of

the prevailing calcareous rock, dipping at an angle scarcely under

that of 45°, traversed by sparry veins, occasionally intermingled

with epidote, in which are also imbedded bright, brown-red rhombic

masses of felspar and amorphous quartz, a circumstance which had

formerly fallen under my notice in a pedestrian tour on this road; I

was now, however, enabled to trace this appearance into a connection

with the transition formation which almost immediately succeeds,

presenting masses of agglomerated rock, chiefly calcareous, of

which the fragments are both angular and arrounded. Beyond this, on

the first succeeding hill, occur layers of the old or transition

sand-stone, not always red, though some of that colour appeared in

the vicinity, interlayed with {11} brown-red slate-clay. Afterwards,

and in connection with this formation, appears the green-stone of the

Germans, and the bottoms of the valleys only are calcareous. Twelve

miles west of Lancaster, we enter the fine fertile tract, once known

to the natives of the Susquehannah by the name of _Pe-quay_, or the

Pleasant Fields.[2]

4th.] To Middleton, grunstein and argillaceous trap, with sand-stone

conglomerate, and Spanish-brown slate-clay alternate and succeed

each other, affording an indifferent soil, and forming lofty hills,

with precipitous declivities and narrow valleys. The sylvan hills of

the Susquehanna are, however, calcareous and underlayed with common

bluish grey and chlorite slate, which as at Lancaster abounds with

scattered or imbedded cubic pyrites.[3] The long bridge of a mile and

a quarter, connecting with a small island, crosses a wide and shallow

part of the river, whose bed is of slate (or argillite).

5th.] About half past seven, I left Harrisburgh, and in the

course of the day proceeded through Carlisle to within five miles

of Shippensburg,[4] a distance of about 31 miles, over a deeply

undulated country, evincing, by the ease and comfort of its scattered

population, no inconsiderable degree of fertility in the soil, which

is calcareous. The first considerable chain of hills, proceeding from

north-east to south-west, clad with unbroken forests, appeared on our

left during most part of the day, and indicated an approach to the

mountains.

6th.] This evening I arrived at Cammels’-town,[5] situated at the

foot of the North Mountain. The intermediate and surrounding country

is deeply undulated with hills of a softish sandstone and slate clay.

The more conspicuous hills of shale, accompanied {12} by organic

remains, commence at Chambersburg,[6] and, as in Virginia, are

characterised by the appearance of Pine (_Pinus inops_), and scrub

oak (_Quercus ilicifolia_); here also occurs the fragrant sumach

(_Rhus aromaticum_).

The road, on which several bands of labourers were employed, was

now nearly completed to Pittsburgh, affording that convenience and

facility to the inland commerce of the state which had been so long

neglected. The states of New-York and Virginia, equally interested in

the advancement of their internal trade, now begin to show themselves

as the serious rivals of Pennsylvania, which, till lately, with the

exception of New-Orleans, enjoyed the most considerable portion of

the commerce of the west.

7th.] To-day I proceeded about 21 miles, over a very poor and

mountainous country. From the little village, or cluster of cabins,

called Loudon,[7] we commence the ascent over the North Mountain, by

an easy and well-levelled turnpike. From its summit appeared a wide

and sterile forest extending across the glen, and, only at small and

distant intervals, obscurely broken by scattered farms. The soil is

here argillaceous, a slate-clay passing into argillaceous trap and

siliceous sandstone, occasionally changing into an almost homogeneous

quartz, predominates. At Loudon, there is a small iron-furnace, and

ore in inconsiderable quantities found in the neighbourhood. Passing

this range, sometimes called the Cove or North Mountain, we descend

to M’Connels’-town,[8] which now presents itself in bird’s-eye view

before us, here the soil is calcareous, but still, to all appearance,

destitute of organic remains. Deep and narrow valleys, steep hills

every where presenting shale devoid of impressions, though often so

far bituminous as to blaze, abound, but no coal is to be met with

nearer than the valley of the Juniata, where organic impressions also

commence. Within the great valley of the {13} North Mountain, are

several other lower and interrupted ranges. The chain also called the

North Mountain, proceeding much to the east in its southern course,

presents in that direction acuminated peaks, and appears interrupted

as towards Staunton in Virginia. From this summit we are distinctly

enabled to mark the direction of the South Mountain, so low where we

crossed it as to afford an almost imperceptible ascent.

What still remained of the old road,[9] appeared here as bad as can

well be imagined; a mere Indian trace, without any choice of level,

over rocky ledges and gullies, threatening at every instant the

destruction of the carriages which ventured over it.

8th.] After travelling about 28 miles, I arrived, in the evening,

at the very pleasant and romantically situated town of Bedford,[10]

hemmed in by a cove of mountains to the south and west, near whose

declivity issue the chalybeate springs, occasionally the resort of

the sick and convalescent. Very little of the road over which I came

to-day was yet turnpike, and as bad as may naturally be supposed

over a succession of mountain ridges, which, though scattered, and

interrupted by the passage of waters, scarcely fall short of the

North Mountain in point of elevation. These ridges, of which in the

above distance there are three or four, are all often confounded in

the name of Cove Mountain.

I crossed the Juniata by a wooden toll-bridge, which, like all

other private accommodations in the United States, does not exempt

the pedestrian traveller. The valley of the river is narrow and

romantic, embosomed by cliffs, rudely decorated with clumps of sombre

evergreens, particularly the tall Weymouth pine and spruce, with the

splendid Rhododendron and the _Magnolia acuminata_. As we approach

towards Bedford the valleys widen, are more fertile, and present

calcareous strata still inclined at a lofty angle, and generally

destitute of organic remains. Every elevation, {14} and most of them

short and steep, presents a predominance of argillaceous earth,

either red or greenish and slatey, as it may happen to contain an

admixture of iron or chlorite; there are, however, no iron furnaces

nor ore in this quarter nearer than the vicinity of Huntingdon.

Seams of coal have been discovered on the banks of the Juniata, but

unworthy of notice or difficult to drain. Fifteen miles from Bedford,

coal begins to appear. Indeed, about a mile from the town I observed

in the siliceous sandstone made use of for repairing the road, and

which was obtained in the vicinity, casts of _orthoceratites?_ or

something resembling them, collected into fascicles or clusters,

and aggregated over the surface of the rocks in which they are

found; the transverse septa or channels are all proximate, and their

circumference is about two inches. Excepting a second impression,

something similar, but much smaller (and which rather resembles some

alcyonite), no other reliquiæ appeared in this stone, which is also

the first occurrence of the kind on my journey to the westward.

The mountain scenery, at first so grand and impressive, becomes at

length monotonous; most of the cimes, terraces, and piles of rocks

lose their effect beneath the umbrageous forest which envelopes them,

and which indeed casts a gloomy mantling over the whole face of

nature.

To judge of the inland commerce carried on betwixt Philadelphia and

Pittsburgh, a stranger has but to view this road at the present

season. All day I have been brushing past waggons heavily loaded with

merchandise, each drawn by five and six horses; the whole road in

fact appears like the cavalcade of a continued fair.

9th.] To-day I proceeded about 20 miles from Bedford on the way

to Pittsburgh, and in the evening lodged at a tavern situated on

the top of the Alleghany ridge. About nine miles from Bedford I

first observed {15} the occurrence of fossil shells, consisting

of terebratulites, and amongst them the _Anomia trigonalis_ of

Martyn, with some other species. They occur in the sandstone

employed for mending the road, with which also alternates much

liver-brown argillaceous shale. From hence the dip of the strata

gradually diminishes, and the hills are no longer so short and steep;

slate-clay with appearances of coal are also visible, but as yet

there are no _zoophytic_, or, as some consider them, _phytolithic_

or vegetable impressions. The ascent to the summit of the Alleghany

from the east is much more gentle than that of the North Mountain,

or the other mountains scattered through this valley. The Alleghany,

here from 10 to 20 miles broad, is apparently the boundary of the

transition, and the long slopes and salient coves of its western

declivity are within the range of the secondary formation. Much of

the _Quercus Primos monticola_ (or mountain chesnut oak) presents

itself on the mountain, together with the _Magnolia acuminata_ and

_Sorbus americana_ or service-berry.

10th.] To-day I walked nine miles to Stoystown,[11] if a handful of

houses like this deserves such an appellation. The declivity of the

surface is much more gentle and inconsiderable than that which I

had passed. Indications of coal were also apparent along the margin

of the road. The valleys are now broader, and the soil of a better

quality. The inhabitants, however, chiefly Irish, are indigent, and

considerably deficient in prudence and cleanliness. I spent most part

of the day in collecting seeds of the _Magnolia acuminata_.

11th.] To-day I proceeded 18 miles to the little hamlet of

Liganier[12] lately begun, and passed through Loughlinstown, equally

inconsiderable, except for dram shops, improperly called taverns,

with which this road abounds. The turnpike is completed nearly

throughout this distance, and also to Greensburgh. Towards evening I

crossed the Laurel Mountain, and found abundantly on {16} its western

declivity the _Circæa alpina_. In the valley on the eastern ascent

I likewise saw the _Betula glauca_, and a profusion of the common

_Rhododendron_, which gives the name of Laurel to this mountain.

Indications of coal, and a continued declension in the dip of the

strata are still obvious. The sandstone, which is almost the only

rock I have seen throughout the course of the day, is remarkable

for the absence of organic reliquiæ. In some places it appears

like grauwacke blended with angular fragments of a soft slate. Near

the western base of the Laurel ridge the usual zoophytes make their

appearance, chiefly _Culmaria striata_[13] (_Striaticulmis_ of

Martyn), also casts of enormous channelled _Culmariæ_ like those of

Bradford, in Yorkshire (England). Vegetation at this advanced season

still appeared very luxuriant on the western descent of the Laurel,

and the valleys bore the appearance of fertility.

12th.] This evening I arrived at Greensburgh,[14] 18 miles west of

Liganier. The last considerable mountain range to the west on this

route is Chesnut Ridge, {17} which I crossed to-day. Here I met

with the _Imperatoria lucida_ of Sprengel, also abundance of the

_Cimicifuga americana_ and _Asplenium angustifolium_. The dip of the

strata becomes now more and more inconsiderable, but organic remains,

except those peculiar to the coal formation, are scarcely to be met

with, and there is a predominance of slaty and argillaceous sandstone.

13th.] The turnpike was now completed through the last 40 miles up to

Pittsburgh, and scarcely any undertaking promises more advantage to

the state in general. It will tend to check the competition of the

inland navigation of the state of New York, as well as that of the

state of Virginia, through which the United States have established a

national road[15] as far as the town of Wheeling on the Ohio.

14th.] West of Greensburg, and indeed east of it, from the base of

the Chesnut Ridge, the surface of the country is deeply undulated,

and laborious to travel. The land upon the height is sterile and

thinly populated; still every five or six miles we meet with some

poor-looking hamlet, which commonly, out of 12 to 20 log cabins

composing it, contains six or seven licensed dram shops, besides

three or four stores for the retailing of merchandise. How much is

a scattered and independent population like that of the honest and

industrious Germans inhabiting the eastern parts of Pennsylvania to

be preferred to these towns whose inhabitants are brought together

by no prospect of general industry or economy. To say that coal is

common throughout this country, and that it is generally employed for

fuel, is repeating a fact familiar to every one who has ever visited

the western country.

15th.] To-day I arrived again in Pittsburgh, and endeavour as I

may to drive away my former prejudices against this very important

commercial and manufacturing city, I find it impossible. Nothing

appears to {18} me to predominate but filth and smoke and bustle.

The rivers and surrounding country are engaging and romantic--its

situation--the Thermopylæ of the west, into which so many thousands

are flocking from every christian country in the world--its rapid

progress, and the enterprising character of its inhabitants, are

circumstances which excite our admiration. In national industry, the

true source of wealth and independence, Pittsburgh is now scarcely

inferior to any of the older and larger towns in the Union. The

shores of the Monongahela were lined with nearly 100 boats of all

descriptions, steam-boats, barges, keels, and arks or flats, all

impatiently and anxiously waiting the rise of the Ohio, which was now

too low to descend above the town of Wheeling. A bridge was at this

time nearly completed across this stream, and one of the piers of

another across the Alleghany was also laid.

The day after my arrival I went through the flint-glass works of Mr.

Bakewell, and was surprised to see the beauty of this manufacture, in

the interior of the United States, in which the expensive decorations

of cutting and engraving (amidst every discouragement incident to

a want of taste and wealth) were carried to such perfection. The

productions of this manufacture find their way to New Orleans, and

even to some of the islands of the West Indies.

The president Monroe, as a liberal encourager of domestic

manufactures, had on his visit to those works given orders for

a service of glass, which might indeed be exhibited as a superb

specimen of this elegant art.

Mr. Bakewell was now beginning to employ the beautiful white and

friable sandstone which had been observed near to a branch of the

Merrimec by Mr. Bradbury[16] and myself, as well as others, in

the winter of 1809. It promises every important requisite for the

production of the purest flint-glass, and exists in inexhaustible

quantities.

{19} 16–19th.] Still at Pittsburgh, waiting for an opportunity to

descend the river, which was now almost impracticable in consequence

of the lowness of the water.

19th.] This morning I took a walk to Grant’s Hill,[17] from whence

there is a delightful view of Pittsburgh, and on the hill itself some

very pleasing rural retirements of the wealthy citizens.

My attention, as usual, was directed to the surrounding minerals and

stratification, which are no unimportant matters in the economy of

this settlement. The coal basin, or rather bed, which has been so

long wrought on this hill, about six feet thick, is almost exactly

horizontal, and consequently worked by a simple parallel drift

without making any inconvenient quantity of water. The coal bassets

out towards the edge of the hill, and so near the summit as to

present scarcely any other overlay than a thin shale, more or less

friable, and no sandstone. The dip, such as it is, is to the north

of east, but scarcely manifest. It is bituminous or inflammable,

and of a very good quality. Beneath this single bed of coal, occurs

a fine grained, micaceous sandstone, rendered greenish from an

admixture of chlorite earth; still lower in the series appears a

compact calcareous rock, in which I did not perceive any reliquiæ.

At the southern extremity of the hill, where it approaches the

Monongahela, the laminated micaceous sandstone, however, exhibits

great clusters of _culmariæ_ (_striaticulmis_ of Martyn), almost

ancipitally compressed, and with the striatures very fine. Here the

calcareous rock beneath the micaceous sandstone exhibits masses

of terebratulites, some of which are very minute, but in great

quantities. Near to the precipitous termination of Grant’s Hill, and

in several other contiguous places, the sandstone appears to have

been disintegrated with violence, and the angular fragments again to

have been cemented by a stalactitial deposition of calcareous spar,

of a fibrous {20} texture, almost similar to Arragonite. Seams of

fibrous gypsum, possessing a silky lustre, have also been discovered

in this vicinity.

In the course of this ramble I found abundance of the _Monarda

hirsuta_, which as well as _M. ciliata_, do not much resemble the

legitimate species of the genus.

FOOTNOTES:

[1] For the early history of the site of Harrisburgh, see

Post’s _Journals_, volume i of our series, note 73.--ED.

[2] In colonial days, the Pequea Indians lived on the creek

of that name, in Lancaster County. A township of this county still

bears the name.--ED.

[3] The chlorite slate of the Wissahickon, near Germantown,

considered as primitive, contains similar pyrites with octahedral

crystals of iron ore.--NUTTALL.

[4] For the early history of Carlisle and Shippensburg, see Post’s

_Journals_, volume i of our series, notes 75, 76.--ED.

[5] Cammels’-town (Campbellstown?); no such town remains. The early

settlers in the region were Scotch-Irish, and the name Campbell

appears among them as early as 1766.--ED.

[6] For the early history of the site of Chambersburg, see Post’s

_Journals_, volume i of our series, note 77.--ED.

[7] For history of fort of same name near Loudon, see _ibid._, note

78.--ED.

[8] M’Connels’-town (now McConnellsburg) is the site of Fort

Lyttleton. See _ibid._, note 80.--ED.

[9] _Ibid._, note 82; also Harris’s _Journal_, in our volume iii,

note 3.--ED.

[10] For the early history of the site of Bedford, see Post’s

_Journals_, volume i of our series, note 81.--ED.

[11] For a sketch of Stoystown, see Flint’s _Letters_, volume ix of

our series, note 33.--ED.

[12] For early history of Ligonier, see Post’s _Journals_, volume i

of our series, note 83; also F. A. Michaux’s _Travels_, in our volume

iii, note 14.--ED.

[13] Although we are as yet unacquainted with the internal and

essential physical structure of these organic remains, which have

been hitherto considered as plants, I have thought it necessary to

assume the above generic name as preferable to the improbable, and

at any rate merely ordinal name of _Phytolithus_. The CULMARIÆ, as I

have termed them, are striated or grooved and somewhat compressed,

cylindric, articulated bodies, gradually attenuating from joint to

joint, mostly undivided, or simple, but occasionally bifid, and at

length terminating in a point. On one of the sides they commonly

possess a deep and central channel, and in some species at the

joints present alternate small protuberances and cavities. Their

soboliferous propagation appeared to originate from these joints,

in the form of wart-like or areolate protuberances, and, unlike

plants, they never seem to have produced any thing similar to leaves,

flowers, or seeds.

The tessellated zoophytes, by others also considered as vegetable

remains, which I have termed STROBILARIÆ are subcylindric and often

somewhat conic, but inarticulated; some of the species protruded, as

occasion required, from the centre of those tessellæ, bodies resembling

hollow spines, or (as would appear from a specimen in my possession

from Bradford, in Yorkshire) suckers or hollow cylinders, with circular

contractile and striated mouths. The whole of these processes, when

exserted mistaken for leaves, could also be withdrawn within the body

of the animal, and indeed most of the casts present this quiescent or

contracted state. These bodies likewise exhibit in some specimens a

complicated internal structure.--NUTTALL.

[14] See sketch of Greensburgh in F. A. Michaux’s _Travels_, volume

iii of our series, note 16.--ED.

[15] On national road, see Harris’s _Journal_, in our volume iii,

note 45.--ED.

[16] Bradbury was Nuttall’s companion on the expedition to the upper

Missouri in 1810; see Preface. For observations on the Merrimec

(Maramec), in that year, see Bradbury’s _Travels_, in our volume v,

note 136.--ED.

[17] For origin of the name Grant’s Hill, and history of the site,

see Harris’s _Journal_, volume iii of our series, note 30.--ED.

A journal of travels into the Arkansa Territory · 第 1 / 10 章