What is malaria? And why is it most intense in hot climates? |
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Africa ague Army in India ascribed atmosphere attacked autumn Avicenna barren become Bengal cachexia cause of malarious climatic influences coast cold season Commission on Sanitary cooler damp deadly decomposing vegetable districts dysentery effect elevation epidemic equable especially European exhalations exist exposed exposure to climatic feet flax forests frequently healthy heat hepatitis hills Hong Kong hot climates hot season humid intense intermittent fever Ionian Islands Jeeva jungle Kamptee Madras Topographical Reports malaria malarious disease malarious fevers marsh poison mentions Minorca moisture monsoon months Mysore nightly observes organic matter paludal Peshawur plains prevalent produce Punjab quinine rain rainy season Regiment remittent fever Report of Royal river rocks Royal Commission says sepoys sickness Sir J. R. Martin soil soldiers specific poison stagnant water station sudden suffered supposed surface Surgeon swamps Terai tion trees troops Tropical Climates unhealthy vegetable vegetable matter winds writers
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หน้า 187 - Director of the Medical Clinic of the University of Tubingen. Translated from the Eighth German Edition, by special permission of the Author, By GEORGE H. HUMPHREYS, MD...
หน้า 173 - To him marsh miasmata, which so infallibly destroy our white soldiers, are in fact no poison. The warm, moist, low, and leeward situations, where these pernicious exhalations are generated and concentrated, prove to him congenial in every respect. He delights in them, for he there...
หน้า 10 - Pathology. —In these forms of fever a malarial poison of an unknown kind, generated in paludal regions or littoral districts, is absorbed, and affects the blood, as cholera, typhus, and other miasmatic poisons do. The poison, in the absence of any better name, is known as "malaria...
หน้า 59 - That cryptogamic spores and other minute bodies are mainly elevated above the surface during the night. That they rise and are suspended in the cold, damp exhalations from the soil, after the sun has set, and fall again to the earth soon after the sun rises.