THE INFLUENCE OF THE Climate of Colorado ON THE NERVOUS SYSTEM. BY CHARLES DENISON, M.D., Denver, Colorado. RBPKtNTKB FBOM THE "ARCHIVES OP BLECTROLOOY ANT) NEUROLOGY* FOR NOVEMBER. 1874. DENVER, COL.; RICHARDS, PUBLISHER. 1875. THE ARCHIVES OF Electrology and Neurology, A JOURNAL OF ELECTRO-THERAPEUTICS AND NERVOUS DISEASES. EDITED BY GEORGE M. BEARD, A.M., M.D. THIS JOURNAL IS NOW THOROUGHLY AND PERMANENTLY ESTABLISHED. $2.50 a Year, in advance. $3 a Year, after January 1,1875. The second number of the first volume, for November, 1874, is now ready, with the following TABLE OF CONTENTS. I. Disorders of Nutrition and Displacements of the Womb, and their Treatment by Faradization. By Dr. A. Tripier, of Paris. 11. The Elements of Electro-Therapeutics. A Series of Letters addressed to Inquiring Practitioners. By George M. Beard, M.D. HI. The Effects of Lightning-Stroke on the Nervous System. By Byron W. Munson, M.D., of Amity, Ct. IV. Cases of Hydrocele. Recovery under Electrolytic and Galvano-Caustic Treatment. By T. F. Frank, M.D., Titusville, Pa. V. Municipal Law, and its Relations to the Constitution of Man. By R. S. Guernsey, Counselor-at-Law, New-York City. VI. The Influence of the Climate of Colorado on the Nervous System. By Charles Denison, M.D., Denver, Col. VII. On the Treatment of Vomiting hy Electricity. By Frederick D. Lente, M.D., of Cold Spring. Member of the Council of the New-York Neuro- logical Society. VIII. Description of a Portable Medical Battery devised by Prof. George W. Rains, M.D., of the Medical Department of the University of Georgia. IX. Galvanism in Ocular and Aural Affections. By W. W. Seely, M.D., Cincinnati. X. Chronic Alcoholism. By George M. Beard, M.D. XL The Relations of the Nervous System to Diseases of the Skin. By L. Duncan Bulkley, A.M., M.D., New-York. Miscellaneous Editorial Notes : The Duty of Vivisection—Camp-Life for the Nervous—Additions to the Cod-Liver Oil Emulsion—Cold Powder—lodoform in Nervous Diseases—Hay Fever Researches—“ Mind Reading”—The Nervous System and Skin-Diseases —ln Memoriam of Prof. Jeffries Wyman and Dr. Anstie. THE INFLUENCE OF THE Climate of Colorado ON THE NERVOUS SYSTEM. BY CHARLES DENISON, M.D., Denver, Colorado. Reprinted prom the “Archives op Elbctrology and Neurology” for November. 1874 DENVER, COL. : RICHARDS, PUBLISHER. 1875. THE Influence of the Climate of Colorado ON THE NEKYOUS SYSTEM. To the Editor of the Archives of Electrology and Neurology : In attempting to comply with your request, only lately received, I must explain that the field of investigation you propose for me is so new, and also, from a seeming conflict of data, so difficult, that the time to which I am limited is too short, even had I nothing else to engage my attention. Besides, I confess to an ignorance of the' subtle forces to be considered, which, perhaps, ought to preclude my attempting such an article as you desire for your estimable journal. You have elsewhere very pertinently asked, u Shall we wait until our knowledge becomes absolute before we reveal it ? Does it not rather become those of us who are seeking truth, as often as may be, to take account of stock of our discoveries ? Is it not well now and then to take an inventory of our igno- rance, and see how little we know?”* As I would answer these questions in the affirmative, I will gladly try to contribute the little I can in answer to your queries, hoping at a later date to furnish the profession, and a * " Atmospheric Electricity and Ozone.” Popular Science Monthly, Feb. 1, 1874. 4 INFLUENCE OF THE CLIMATE OP COLORADO large class of their patients (consumptives), more valuable infor- mation of this climate and its peculiar adaptation to the needs of special classes of invalids. GENERAL NATURE OF THE CLIMATE OF COLORADO. Colorado covers such a large and various area, including an unexplored region to the west, the Rocky Mountain range, about a hundred miles wide, running through the centre, and the broad plains to the east, that we wish to be understood as referring in this paper to a belt of land, say thirty miles wide, lying north and south, along the eastern base of the Rocky Mountains, and including the foot-hills, unless some other locality is specified. This region is interesting, for much of it can be irrigated (which is almost a universal necessity out here) by the streams which flow down the mountain canons. It is here the bulk of Colorado’s population is, and may be expected to be. This belt of land is about 6000 feet above sea-level at the north, a little more than 5000 at Denver, 8000 on the Divide, thirty miles south of Denver, and some less than 5000 at Pueblo, in the valley of the Arkansas river, over a hundred miles south of Denver, from which point the elevation gradually increases to 6000 feet at Trinidad. Opening into this belt of land are rugged canons, the only passes to parks and points of interest in the mountains. These parks are extensive elevated plains, surrounded by lofty mountains, and interspersed with hills of no small dimen- sions for a less mountainous country. The southernmost is the San Louis Park, which includes an extensive valley of the Rio Grande, at an average elevation of about 7500 feet, in which is the new town of Del Norte. The next to the north of this is South Park, with an average eleva- tion of 9000 feet, in the west of which, beautifully nestled under the mountains, is the little- town of Fairplay and several mining towns. Still farther to the north-west is a collection of valleys called Middle Park, the streams of which are tributary to the Colorado, which finds its way to the Pacific. In one of these valleys are some hot sulphur springs, which are of a temperature of from 110 to 116 degrees, and I judge The average elevation of this “ Park” is 8600 feet. ON THE NERVOUS SYSTEM. 5 will prove beneficial in eradicating constitutional taints of blood. North and east of this are North and Estes Parks, of nearly as great altitude, the latter noted for its rugged scenery. The average elevation of the whole territory is about 6500 feet. The Pocky Mountain range, the backbone of the Ame- rican continent, reaches its highest elevation in Central Colo- rado, the passes over it, both to the north and south of us, being- lower and less difficult; while in this part of the territory they have an elevation of 11,000 to 13,000 feet, the peaks reaching from 13,500 to over 14,000 feet above sea-level. The climate of these mountain regions compares unfavorably with that of the plains to the east during the colder portion of the year ; while in summer, the cooler and bracing atmosphere of the mountains is a grateful relief to those who are enervated by the continuous warmth of the plains. The soil of the plains along these mountain-slopes is a dry, sandy loam, the washings for centuries from the mountainous regions beyond. It is chiefly of an alkaline nature, and some- times the deposit of alkali is considerable, affecting vegetation and drinking-water. The products of the soil, especially the cereals, are remarkable for their richness. The wheat of Colo- rado is unsurpassed. The plains are covered with a short, fine, prairie grass, which cures as it grows. On this cattle feed all the year round and seem to thrive. There are no trees except on the banks of streams, on the Divide, or those cultivated by irrigation. The pine forests on the Divide are in pleasant contrast with the ap- parent barrenness of most of the region east of the mountains. In the mountains timber is abundant, especially yellow pine and spruce, which grow between the altitudes of eight and eleven thousand feet. There are four remarkable features of this climate which dis- tinguish it from the eastern part of the United States, and make it a most desirable change for certain classes of invalids. These are its altitude, with the increased amount of atmo- spheric electricity and ozone due to the same, a large proportion of clear days, a small relative humidity of atmosphere, and a small annual rainfall. The wind does not blow here as much as one would expect in such a light, airy region. Usually 6 INFLUENCE OF THE CLIMATE OF COLORADO before a storm, however, the mountain breezes swing down upon us in playful gusts, and at times the commotion is quite general, constituting a wind, or, more properly, a dust storm, which may last from one to five hours. There have been four of these (“ right smart ” ones, the Westerners would say) during the past year. It is generally understood that a rise of about 300 feet in alti- tude gives one degree colder temperature. Did this rule hold strictly here, this climate would be colder than it is. Among other causes of a considerable difference (in our favor for the colder portions of the year) is chiefly to be mentioned our inland location, and the protection of the mountains on the west.. The average temperature of this immediate vicinity is about the sarnetfs that of New-York city, Southern Pennsylvania, Central Ohio, Indiana, and Illinois; but it does not seem so cold, because of the dryness of the air, the small amount of snow, and the usually sunny days. The nights, when people are indoors, are generally cold in winter, and during the rest of the year much cooler than the days. This diurnal variation, which is here about 15 degrees between the temperature at 2 p.m. and that at 7 a.m. or 9 p.m., increases with the altitude; as in this rarefied atmosphere the intensity of the sun’s rays in- creases with each decided elevation, while the capacity of the air to retain the heat thus imparted proportionately decreases. So that, on the tops of our highest mountains, as a Signal Ser- vice observer on Pike’s Peak informed me, the heat of the sun at midday is “ almost scorching,” while the thermometer after sundown is in the neighborhood of zero. This climate, then, is only “ the most equable of the Western Hemisphere ” when compared with others of the same alti- tude. Let those who think kn equable temperature is the all- important element of a healthy atmosphere, stay near the sea, where the air at night can hold fast its heat as well as its moist- ure. To such, the results of the experiment made by the own- ers of the Mammoth Cave in Kentucky will prove useful. In the equable temperature of this dungeon they imagined was the panacea for the unfortunate consumptive, and the reputation of that health-resort would become world-renowned. I shall never forget the dismal aspect of those cold stone ON THE NERVOUS SYSTEM. 7 houses, erected down in that abyss of darkness. Here, in this extremely equable climate, I was informed over a dozen unfor- tunate consumptives were domiciled. Of course they all suffer- ed for it. One died in the cave, and four more within four weeks after they were brought out. It is strange how similarly foolish thousands of invalids (or their advisers) are throughout our land, who house themselves in dungeons of man’s construc- tion, pining away to consumptives' graves, when there is plenty of invigorating air and life-giving sunshine “ lying around loose,” if they will only go where it is. The sunshine of this inland region is one of its greatest boons for the consumptive, too little appreciated by many who seek health among us. ISTo less important, especially to those whose respiratory organs are at fault, is altitude, which is here a happy medium foT the majority of such patients, while the same may be easily varied to any desired elevation. A most important element of a healthy climate ’is the rela- tive humidity of its atmosphere. Indeed, from a somewhat extended study of the subject, my conviction is strengthened that this element is the most essential ingredient of the con- sumptive’s home, since from a low ratio of humidity a large pro- portion of sunny days and a of rainfall can be inferred ; for had there been much rain or cloudy weather, the air would have been near “ saturation,” and the relative hu- midity, which is the percentage of saturation, would have been affected thereby. In this connection, I must object to the extravagant state- ment some have made, that “ the atmosphere is entirely free from humidity.” We are not quite so badly off as that. Such a report would not seem so ridiculous coming from south-western Arizona; but here, if the hydrometer ever indicates zero, i.e., if there is not enough evaporation in the air to affect it, it is only occasionally for two or three hours in the warmest and most enervating part of the day. Below is a weather report for the past year, which has been kindly prepared for me by P. J, Huneke, U. S. Signal Officer, stationed at Denver. 8 INFLUENCE OF THE CLIMATE OF COLORADO Monthly average.. 1878, October “ November... “ December.... 1874, January “ February “ March “ April ‘ ‘ May “ June “ -July ‘ ‘ August “ September... . 05° MOStSQOMOSiSMMCCi-iffi obtocioooooooo Maximum temperature. bi Ol OD csoia^»KR bi Minimum temperature. O 00 Q O W CO Q CJ K to o Ql bbbbb’KbHbi^oM Average daily temperature. P CO Average daily humidity, per cent. H-L 1—*• <* H-iOOSH^lOi^OOOOOO coc5Coto^