scholarly journals The Compleat geographer, or, The chorography and topography of all the known parts of the earth to which is premis'd an introduction to geography, and a natural history of the earth and the elements ... to which are added maps of every country, fairly engraven on copper, according to the latest

1709 ◽  
Keyword(s):  
2021 ◽  
Vol 15 (4) ◽  
pp. 327-347
Author(s):  
Jean Francesco A.L. Gomes

Abstract The aim of this article is to investigate how Abraham Kuyper and some late neo-Calvinists have addressed the doctrine of creation in light of the challenges posed by evolutionary scientific theory. I argue that most neo-Calvinists today, particularly scholars from the Vrije Universiteit Amsterdam (VU), continue Kuyper’s legacy by holding the core principles of a creationist worldview. Yet, they have taken a new direction by explaining the natural history of the earth in evolutionary terms. In my analysis, Kuyper’s heirs at the VU today offer judicious parameters to guide Christians in conversation with evolutionary science, precisely because of their high appreciation of good science and awareness of the nonnegotiable elements that make up the orthodox Christian narrative.


2021 ◽  
Vol 43 (1) ◽  
pp. 130-136
Author(s):  
Valeriy SNAKIN

Anatolij Nikiforovich Tyuryukanov (1931-2001), Dr.Sci (Biol.), professor was a remarkable Russian natural scientist, who made a signifi contribution to soil science and the theory of the biosphere. Investigation of Tyuryukanov’s works shows both evolution of the author’s scientifi interests and development of natural history in Russia in 20th century. He formulated the biosphere natural history principle founded on a new fundamental category of sciences foundation in 20th century. Th principle is based on genetic soil science, biogeocenology, landscape geochemistry and main branches of the Earth biosphere and vitasphere study. Interesting and sometimes unexpected assertions of A.N. Tyuryukanovs provide food for thought about both further studies of nature, development of biosphere study and refl on the human and biosphere relationships.


1794 ◽  
Vol 3 (2) ◽  
pp. 77-85 ◽  
Author(s):  
James Hutton

Since reading the paper upon the theory of the earth, I have been employed in examining many parts of this country, in order to enquire into the natural history of granite. In this undertaking, I have succeeded beyond my most flattering expectations; and I am now to communicate to this Society the result of my observations.In the paper just referred to, it was maintained, from many different arguments, that all the solid strata of the earth had been consolidated by means of subterraneous heat, softening the hard materials of those bodies; and that in many places, those consolidated strata had been broken and invaded by huge masses of fluid matter similar to lava, but, for the most part, perfectly distinguishable from it. Granite also was considered there as a body which had been certainly consolidated by heat; and which had, at least in some parts, been in the state of perfect fusion, and certain specimens were produced, from which I drew an argument in support of this conclusion.


1695 ◽  
Vol 19 (217) ◽  
pp. 115-124

V. An account of books. I. An essay toward a natural history of the earth, and terrestrial bodies, especially minerals: As also of the sea, rivers, and springs. With an account of the universal deluge, and of the effects that it had upon the earth. By John Woodward, M. D. Professor of Physick in Gresham College, and Fellow of the Royal Society. Printed for Ric. Wilkin at the King's Head in St. Paul's Church-yard. 1695. Octavo. 2. An account of a paper, entituled, archibaldi pitcarnii, M. D. dissertatio de Febribus, &c. The Author of this Book having with great Industry, and no less Success, made Enquiry into many considerable Parts of Nature, hath thought fit here to set forth an Account of several of his Observations, and of certain Conclusions which he hath drawn from them, whereof many are indeed of great weight and moment, but all in a compendious manner, as intending this Discourse only as a Prœlude to one-much larger, and to comply with the Importunities of some Persons of Worth, who .requested a brief Account of these things from him, for their present Satisfaction, until his Affairs should permit the compleating of his Greater Work, which he promiseth, with a further Proof both of these, and of others not yet proposed.


1998 ◽  
Vol 17 (2) ◽  
pp. 84-91 ◽  
Author(s):  
Kenneth Taylor

A conceptual and methodological tension can be discerned among Enlightenment advocates of earth science, as regards extraterrestrial events and processes. True to the fundamental traditions of Theories of the Earth, many scientific thinkers exhibited clear recognition of the Earth's planetary status, as a member of a celestial family. To some this legitimated integration of a geological perspective into that of cosmology and astronomy. In extreme instances it even entailed an ideal of establishing earth science by deduction from principles of celestial mechanics. However, this integrative aspect of Theories of the Earth ran counter to another important element in the geological thinking of this era, one which asserted the overriding value of empirical investigation. In the minds of many empirical-minded champions of a natural history of the Earth, a true geology could only be built up through inductive discovery focussed exclusively on accessible terrestrial phenomena. Sometimes explicitly, often by merely tacit exclusion of extraterrestrial considerations, much geological investigation before 1800 tended to identify the integrity of the emerging science with the distinctively Earth-bound nature of the objects of study. The ideal of an autonomous geological science thus tended to be intertwined with a concept of terrestrial autonomy.


Author(s):  
Bill Jenkins

The dominant school of geology in Edinburgh in the early nineteenth century was that of the followers of the German mineralogist Abraham Gottlob Werner. His most important disciple in the English-speaking world was Edinburgh’s professor of natural history, Robert Jameson. The Wernerians believed that the history of the earth was fundamentally directional; they believed the earth started out as a ball of hot fluid from which the different rocks that now form the crust of the planet gradually precipitated out over geological time. It is argued in this chapter that this directional model of the geological history of the earth was peculiarly compatible with a progressive model of the history of life on earth. The changes in the physical condition of the earth over geological time were seen by some Wernerian geologists as driving the evolution of life.


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