Short Geology Quotes

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A million years is a short time - the shortest worth messing with for most problems. You begin tuning your mind to a time scale that is the planet's time scale. For me, it is almost unconscious now and is a kind of companionship with the earth.
John McPhee (Basin and Range)
How fleeting are the wishes and efforts of man! How short his time! Consequently how poor will his products be, compared with those accumulated by nature during whole geological periods. Can we wonder, then, that nature’s productions should be far “truer” in character than man’s productions; that they should be infinitely better adapted to the most complex conditions of life, and should plainly bear the stamp of far higher workmanship?
Charles Darwin (The Origin of Species)
In general, we imagine rivers to be subject to a kind of dynamic equilibrium, largely stable geologic features, with processes like regional incision or subtle shifts in mountain building causing short- and medium-term variation around some slowly changing mean condition, but in fact it is far more common to see dramatic change over short periods, with long periods of stability between in what geologists refer to as 'dynamic metastable equilibrium.' It is the same with families, memory, the history of a person's life, what we believe to be true.
Katharine Haake (That Water, Those Rocks: (A Novel) (Western Literature and Fiction Series))
Originally, geological history was divided into four spans of time: primary, secondary, tertiary and quaternary.
Bill Bryson (A Short History of Nearly Everything)
We don’t think in economic cycles, we don’t think in election cycles … in this [oil] industry, we think in earth time. Geologic time. There’s no short-term problem we can’t wait out.
Lydia Kiesling (Mobility)
Altogether, according to John McPhee, [geological ages] number in the „tens of dozens.” Fortunately, unless you take up geology as a career, you are unlikely ever to hear any of them again.
Bill Bryson (A Short History of Nearly Everything)
This is a point known to geology as the KT boundary1 and it marks the time, 65 million years ago, when the dinosaurs and roughly half the world’s other species of animals abruptly vanish from the fossil record.
Bill Bryson (A Short History of Nearly Everything)
Charles Darwin announced that the geological processes that created the Weald, an area of southern England stretching across Kent, Surrey and Sussex, had taken, by his calculations, 306, 662, 400 years to complete.
Bill Bryson (A Short History of Nearly Everything)
The world moves at a geological pace, no pun intended. That is, there’s lots of standing still, doing nothing much, and then the occasional short, sharp yank. Once in a while, there’s a huge kaboom, and nothing is quite the same afterward.
Garon Whited (Sunset (Nightlord, #1))
Yet it would be nearly impossible to overstate Lyell’s influence. The Principles of Geology went through twelve editions in his lifetime and contained notions that shaped geological thinking far into the twentieth century. Darwin took a first edition with him on the Beagle voyage and wrote afterwards that ‘the great merit of the Principles was that it altered the whole tone of one’s mind, and therefore that, when seeing a thing never seen by Lyell, one yet saw it partially through his eyes22.’ In short, he thought him nearly a god, as did many of his generation. It is a testament to the strength of Lyell’s sway that in the 1980s, when geologists had to abandon just a part of his theory to accommodate the impact theory of extinctions, it nearly killed them. But that is another chapter.
Bill Bryson (A Short History of Nearly Everything)
Nowadays, and speaking very generally, geological time is divided first into four great chunks known as eras: Precambrian, Palaeozoic (from the Greek meaning “old life”), Mesozoic (“middle life”) and Cenozoic (“recent life”). These four eras are further divided into anywhere from a dozen to twenty subgroups,
Bill Bryson (A Short History of Nearly Everything)
Crutzen wrote up his idea in a short essay, “Geology of Mankind,” that ran in Nature. “It seems appropriate to assign the term ‘Anthropocene’ to the present, in many ways human-dominated, geological epoch,” he observed. Among the many geologic-scale changes people have effected, Crutzen cited the following: • Human activity has transformed between a third and a half of the land surface of the planet. • Most of the world’s major rivers have been dammed or diverted. • Fertilizer plants produce more nitrogen than is fixed naturally by all terrestrial ecosystems. • Fisheries remove more than a third of the primary production of the oceans’ coastal waters. • Humans use more than half of the world’s readily accessible fresh water runoff. Most significantly, Crutzen said, people have altered the composition of the atmosphere. Owing to a combination of fossil fuel combustion and deforestation, the concentration of carbon dioxide in the air has risen by forty percent over the last two centuries, while the concentration of methane, an even more potent greenhouse gas, has more than doubled. “Because of these anthropogenic emissions,” Crutzen wrote, the global climate is likely to “depart significantly from natural behavior for many millennia to come.
Elizabeth Kolbert (The Sixth Extinction: An Unnatural History)
In 1802, five years after Hutton’s death, Playfair produced a simplified exposition of the Huttonian principles, entitled Illustrations of the Huttonian Theory of the Earth. The book was gratefully received by those who took an active interest in geology, which in 1802 was not a large number. That, however, was about to change. And how.
Bill Bryson (A Short History of Nearly Everything)
the aforementioned Murchison, who spent the first thirty or so years of his life galloping after foxes, converting aeronautically challenged birds into puffs of drifting feathers with buckshot, and showing no mental agility whatever beyond that needed to read The Times or play a hand of cards. Then he discovered an interest in rocks and became with rather astounding swiftness a titan of geological thinking.
Bill Bryson (A Short History of Nearly Everything)
This may be the era of the Anthropocene – the geological epoch in which human action is transforming the planet. But it is also one in which the human animal is less than ever in charge. Global warming seems to be in large part the result of the human impact on the planet, but this is not to say humans can stop the process. Whatever is done now, human expansion has triggered a shift that will persist for thousands of years.
John Gray (The Soul of the Marionette: A Short Inquiry into Human Freedom)
So it came as a surprise when, in 1859 in On the Origin of Species, Charles Darwin announced that the geological processes that created the Weald, an area of southern England stretching across Kent, Surrey, and Sussex, had taken, by his calculations, 306,662,400 years to complete. The assertion was remarkable partly for being so arrestingly specific but even more for flying in the face of accepted wisdom about the age of the Earth.
Bill Bryson (A Short History of Nearly Everything)
H. Huxley disliked Darwin’s insistence on huge amounts of geological time because he was a saltationist, which is to say a believer in the idea that evolutionary changes happen not gradually but suddenly. Saltationists (the word comes from the Latin for “leap”) couldn’t accept that complicated organs could ever emerge in slow stages. What good, after all, is one-tenth of a wing or half an eye? Such organs, they thought, only made sense if they appeared in a finished state.
Bill Bryson (A Short History of Nearly Everything)
Darwin was often honored in his lifetime, but never for On the Origin of Species or Descent of Man. When the Royal Society bestowed on him the prestigious Copley Medal it was for his geology, zoology, and botany, not evolutionary theories, and the Linnaean Society was similarly pleased to honor Darwin without embracing his radical notions. He was never knighted, though he was buried in Westminster Abbey—next to Newton. He died at Down in April 1882. Mendel died two years later.
Bill Bryson (A Short History of Nearly Everything)
The idea is that just as mammals bided their time for a hundred million years until the dinosaurs cleared off and then seemingly burst forth in profusion all over the planet, so too perhaps the arthropods and other triploblasts waited in semimicroscopic anonymity for the dominant Ediacaran organisms to have their day. Says Fortey: “We know that mammals increased in size quite dramatically after the dinosaurs went—though when I say quite abruptly I of course mean it in a geological sense. We’re still talking millions of years.
Bill Bryson (A Short History of Nearly Everything)
The Chemical Society of London was not founded until 1841 and didn’t begin to produce a regular journal until 1848, by which time most learned societies in Britain—Geological, Geographical, Zoological, Horticultural, and Linnaean (for naturalists and botanists)—were at least twenty years old and often much more. The rival Institute of Chemistry didn’t come into being until 1877, a year after the founding of the American Chemical Society. Because chemistry was so slow to get organized, news of Avogadro’s important breakthrough of 1811 didn’t begin to become general until the first international chemistry congress, in Karlsruhe, in 1860.
Bill Bryson (A Short History of Nearly Everything)
Because the British were the most active in the early years of the discipline, British names are predominant in the geological lexicon. Devonian is of course from the English county of Devon. Cambrian comes from the Roman name for Wales, while Ordovician and Silurian recall ancient Welsh tribes, the Ordovices and Silures. But with the rise of geological prospecting elsewhere, names began to creep in from all over. Jurassic refers to the Jura Mountains on the border of France and Switzerland. Permian recalls the former Russian province of Perm in the Ural Mountains. For Cretaceous (from the Latin for chalk) we are indebted to a Belgian geologist with the perky name of J. J. d’Omalius d’Halloy.
Bill Bryson (A Short History of Nearly Everything)
We know that Earth’s magnetic field changes in power from time to time: during the age of the dinosaurs, it was up to three times as strong as now. We also know that it reverses itself every 500,000 years or so on average, though that average hides a huge degree of unpredictability. The last reversal was about 750,000 years ago. Sometimes it stays put for millions of years—37 million years appears to be the longest stretch—and at other times it has reversed after as little as 20,000 years. Altogether in the last 100 million years it has reversed itself about two hundred times, and we don’t have any real idea why. It has been called “the greatest unanswered question in the geological sciences.
Bill Bryson (A Short History of Nearly Everything)
In an extremely short period of geologic time the Earth has been saturated with several billion pounds of nonbiodegradable, often biologically unique pharmaceuticals designed to kill bacteria. Many antibiotics (literally meaning “against life”) do not discriminate in their activity, but kill broad groups of diverse bacteria whenever they are used. The worldwide environmental dumping, over the past 65 years, of such huge quantities of synthetic antibiotics has initiated the most pervasive impacts on the Earth’s bacterial underpinnings since oxygen-generating bacteria supplanted methanogens 2.5 billion years ago. As bacterial researcher Stuart Levy comments . . . It has stimulated evolutionary changes that are unparalleled in recorded biologic history.4
Stephen Harrod Buhner (Plant Intelligence and the Imaginal Realm: Beyond the Doors of Perception into the Dreaming of Earth)
His ignorance was as remarkable as his knowledge. Of contemporary literature, philosophy and politics he appeared to know next to nothing. Upon my quoting Thomas Carlyle, he inquired in the naivest way who he might be and what he had done. My surprise reached a climax, however, when I found incidentally that he was ignorant of the Copernican Theory and of the composition of the Solar System. That any civilized human being in this nineteenth century should not be aware that the earth travelled round the sun appeared to be to me such an extraordinary fact that I could hardly realize it. “You appear to be astonished,” he said, smiling at my expression of surprise. “Now that I do know it I shall do my best to forget it.” “To forget it!” “You see,” he explained, “I consider that a man’s brain originally is like a little empty attic, and you have to stock it with such furniture as you choose. A fool takes in all the lumber of every sort that he comes across, so that the knowledge which might be useful to him gets crowded out, or at best is jumbled up with a lot of other things so that he has a difficulty in laying his hands upon it. Now the skilful workman is very careful indeed as to what he takes into his brain-attic. He will have nothing but the tools which may help him in doing his work, but of these he has a large assortment, and all in the most perfect order. It is a mistake to think that that little room has elastic walls and can distend to any extent. Depend upon it there comes a time when for every addition of knowledge you forget something that you knew before. It is of the highest importance, therefore, not to have useless facts elbowing out the useful ones.” “But the Solar System!” I protested. “What the deuce is it to me?” he interrupted impatiently; “you say that we go round the sun. If we went round the moon it would not make a pennyworth of difference to me or to my work.” I was on the point of asking him what that work might be, but something in his manner showed me that the question would be an unwelcome one. I pondered over our short conversation, however, and endeavoured to draw my deductions from it. He said that he would acquire no knowledge which did not bear upon his object. Therefore all the knowledge which he possessed was such as would be useful to him. I enumerated in my own mind all the various points upon which he had shown me that he was exceptionally well-informed. I even took a pencil and jotted them down. I could not help smiling at the document when I had completed it. It ran in this way— SHERLOCK HOLMES—his limits. 1. Knowledge of Literature.—Nil. 2. Philosophy.—Nil. 3. Astronomy.—Nil. 4. Politics.—Feeble. 5. Botany.—Variable. Well up in belladonna, opium, and poisons generally. Knows nothing of practical gardening. 6. Geology.—Practical, but limited. Tells at a glance different soils from each other. After walks has shown me splashes upon his trousers, and told me by their colour and consistence in what part of London he had received them. 7. Chemistry.—Profound. 8. Anatomy.—Accurate, but unsystematic. 9. Sensational Literature.—Immense. He appears to know every detail of every horror perpetrated in the century. 10. Plays the violin well. 11. Is an expert singlestick player, boxer, and swordsman. 12. Has a good practical knowledge of British law.
Arthur Conan Doyle (A Study in Scarlet (Sherlock Holmes, #1))
Each scenario is about fifteen million years into the future, and each assumes that the Pacific Plate will continue to move northwest at about 2.0 inches per year relative to the interior of North America. In scenario 1, the San Andreas fault is the sole locus of motion. Baja California and coastal California shear away from the rest of the continent to form a long, skinny island. A short ferry ride across the San Andreas Strait connects LA to San Francisco. In scenario 2, all of California west of the Sierra Nevada, together with Baja California, shears away to the northwest. The Gulf of California becomes the Reno Sea, which divides California from Nevada. The scene is reminiscent of how the Arabian Peninsula split from Africa to open the Red Sea some 5 million years ago. In scenario 3, central Nevada splits open through the middle of the Basin and Range province. The widening Gulf of Nevada divides the continent form a large island composed of Washington, Oregon, California, Baja California, and western Nevada. The scene is akin to Madagascar’s origin when it split form eastern Africa to open the Mozambique Channel.
Keith Meldahl
Bell treated his friend and colleague Watson generously. Though he had no legal obligations to do so, he awarded Watson 10 percent of the company, allowing Watson to retire rich at the age of just twenty-seven. Able to do anything he wanted, Watson devoted the rest of his life to just that. He traveled the world, read widely, and took a degree in geology at MIT for the simple satisfaction of improving his brain. He then started a shipyard, which quickly grew to employ four thousand men, producing a scale of stress and obligation way beyond anything he wished for, so he sold the business, converted to Islam, and became a follower of Edward Bellamy, a radical philosopher and quasi communist who for a short period in the 1880s enjoyed phenomenal esteem and popularity. Tiring of Bellamy, Watson moved to England in early middle age and took up acting, for which he showed an unexpected talent. He proved particularly adept at Shakespearean roles and performed many times at Stratford-upon-Avon before returning to America and a life of quiet retirement. He died, contented and rich, at his winter home on Pass-Grille Key, Florida, just shy of his eighty-first birthday in 1934.
Bill Bryson (At Home: A Short History of Private Life)
In the winter of 18077, thirteen like-minded souls in London got together at the Freemasons Tavern at Long Acre, in Covent Garden, to form a dining club to be called the Geological Society. The idea was to meet once a month to swap geological notions over a glass or two of Madeira and a convivial dinner. The price of the meal was set at a deliberately hefty 15 shillings to discourage those whose qualifications were merely cerebral. It soon became apparent, however, that there was a demand for something more properly institutional, with a permanent headquarters, where people could gather to share and discuss new findings. In barely a decade membership grew to 400 – still all gentlemen, of course – and the Geological was threatening to eclipse the Royal as the premier scientific society in the country. The members met twice a month from November until June8, when virtually all of them went off to spend the summer doing fieldwork. These weren’t people with a pecuniary interest in minerals, you understand, or even academics for the most part, but simply gentlemen with the wealth and time to indulge a hobby at a more or less professional level. By 1830 there were 745 of them, and the world would never see the like again. It is hard to imagine now, but geology excited the nineteenth century – positively gripped it – in a way that no science ever had before or would again.
Bill Bryson (A Short History of Nearly Everything)
Born in 1821, Croll grew up poor, and his formal education lasted only to the age of thirteen. He worked at a variety of jobs—as a carpenter, insurance salesman, keeper of a temperance hotel—before taking a position as a janitor at Anderson’s (now the University of Strathclyde) in Glasgow. By somehow inducing his brother to do much of his work, he was able to pass many quiet evenings in the university library teaching himself physics, mechanics, astronomy, hydrostatics, and the other fashionable sciences of the day, and gradually began to produce a string of papers, with a particular emphasis on the motions of Earth and their effect on climate. Croll was the first to suggest that cyclical changes in the shape of Earth’s orbit, from elliptical (which is to say slightly oval) to nearly circular to elliptical again, might explain the onset and retreat of ice ages. No one had ever thought before to consider an astronomical explanation for variations in Earth’s weather. Thanks almost entirely to Croll’s persuasive theory, people in Britain began to become more responsive to the notion that at some former time parts of the Earth had been in the grip of ice. When his ingenuity and aptitude were recognized, Croll was given a job at the Geological Survey of Scotland and widely honored: he was made a fellow of the Royal Society in London and of the New York Academy of Science and given an honorary degree from the University of St. Andrews, among much else. Unfortunately,
Bill Bryson (A Short History of Nearly Everything)
After Us, the Salamanders!, The Future belongs to the Newts, Newts Mean Cultural Revolution. Even if they don't have their own art (they explained) at least they are not burdened with idiotic ideals, dried up traditions and all the rigid and boring things taught in schools and given the name of poetry, music, architecture, philosophy and culture in any of its forms. The word culture is senile and it makes us sick. Human art has been with us for too long and is worn-out and if the newts have never fallen for it we will make a new art for them. We, the young, will blaze the path for a new world of salamandrism: we wish to be the first newts, we are the salamanders of tomorrow! And so the young poetic movement of salamandrism was born, triton - or tritone - music was composed and pelagic painting, inspired by the shape world of jellyfish, fish and corals, made its appearance. There were also the water regulating structures made by the newts themselves which were discovered as a new source of beauty and dignity. We've had enough of nature, the slogans went; bring on the smooth, concrete shores instead of the old and ragged cliffs! Romanticism is dead; the continents of the future will be outlined with clean straight lines and re-shaped into conic sections and rhombuses; the old geological must be replaced with a world of geometry. In short, there was once again a new trend that was to be the thing of the future, a new aesthetic sensation and new cultural manifestoes; anyone who failed to join in with the rise of salamandrism before it was too late felt bitterly that he had missed his time, and he would take his revenge by making calls for the purity of mankind, a return to the values of the people and nature and other reactionary slogans. A concert of tritone music was booed off the stage in Vienna, at the Salon des Indépendents in Paris a pelagic painting called Capriccio en Bleu was slashed by an unidentified perpetrator; salamandrism was simply victorious, and its rise was unstoppable.
Karel Čapek (War with the Newts)
At that time the North American continent was host to many large mammals, mammoths, mastodons, camels, horses, giant ground sloths and beavers the size of today’s black bears, saber-toothed cats, savage short-faced bears, cheetahs, lions and dire wolves. Scores of other large species roamed the continent as well. They all vanished about 12,000 years ago in a geological eye blink. Twenty- seven different mammalian genera were destroyed completely from North America.[473]
David Flynn (The David Flynn Collection)
With a detonation that dashed rocks and huge sods of rain-sodden soil bursting in every direction, the ground behind the monastery seemed at first to be giving birth to some kind of rounded hill, as though I were witnessing in the short space of mere seconds the geological outcome of centuries: a small mountain emerging purposefully out of the ground. The next thing I noticed was the sides - the sides that were moving, heaving, breathing! Still, it wasn’t until the demonic face of it appeared that I realized I was seeing the humped, bristled back of that ungodly conjuration. The face it bore was that of a gargantuan hog! And yet, though that was my first thought upon seeing it, it was so much more than just that, so much worse! There were too many teeth, too many hooks and horns, its jaws bristled and barbed and jutted by tusks, its pallid, smoking snout writhing with black hair that seemed to be separately, insidiously alive and dancing in the deluging rain. Dark, scaly skin surrounded glowing eyes like obsidian-sloped volcanos in the face of an almighty Underworld Un-God. Over its shoulders sprouted and stretched black, web-skin wings more massive than the canvases a sail fleet could account for, and those wings extended to blot out all the heavy-keening heavens - all but for the Blood Cloud above the Beast which still floated halo-like above the Demons birthplace, and which seemed to me the volitant reservoir of every wound ever suffered in the world.
Avalon Brantley (The House of Silence)
Worse yet, scientific models, like people and cattle and insect species and mountains and all things known, have a lifespan. Mountains may survive geological eras, but scientific maps, like people and birds, have short lives. None has ever lasted more than a few hundred years, at present. To believe in any such mask with the fervor of Gross and Levitt contradicts all known facts of scientific history. Every theory they worship will someday get junked.
Robert Anton Wilson (Cosmic Trigger III: My Life After Death)
Ocean acidification is one of the largest unique geological events that the Earth has undergone in the last fifty million years. And it introduces another concept to which we connect poorly: time itself. Although time is properly called linear, imagining that the ocean will change more in the next hundred years than it has in the last fifty million years is a challenge. The time since Iceland’s settlement is very short, not more than twelve times my Grandma’s life: eleven hundred years. The history of Iceland is, in a sense, a continuous story of twelve women like my Grandma. Twelve girls who were born and lived lives that each felt like a flash. Twelve women in their nineties stretching out their hands as if they’re doing water aerobics, touching flat palms together. Their eyes gleam because time passes so fast that their eyes don’t realise they’re nearly a hundred years old. Time runs so fast that Jesus was born around twenty-one grandmas ago. They’d all fit in a single city bus, even if you added all their husbands. The earliest written records of humans date back five thousand years, events that happened practically yesterday. Humanity first emerged the day before that, in comparison to the ocean’s fifty-millionyear history.
Andri Snær Magnason (On Time and Water)
Sometimes religion fails to serve its meaning-making function at moments of catastrophic disruption or cultural change. For example, many elite and middle class Christian adherents were shaken by a Victorian spiritual crisis as intellectual challenges converged. Between 1840 and 1900 some lost faith in the face of Darwinian biology and the new geology, which challenged biblical claims about the origin and age of the universe; the new historical and literary study of the Bible, called Higher Criticism, which challenged the claim that scripture was divinely inspired; and the new comparative study of religions, which challenged the uniqueness and superiority of Christianity. Those doubters now looked out on a different ocean, as does the narrator in Matthew Arnold's poem "Dover Beach," who once found comfort as waves in "the sea of faith" drew near, but who now hears only "its melancholy, long, withdrawing roar.
Thomas A Tweed (Religion: A Very Short Introduction (Very Short Introductions))
For many geologists, the most important consequence of the recognition of plate tectonics was that it brought confirmation of continental drift. As important, plate tectonics allowed continental drift to be determined with considerable precision. This became immediately clear to Clark Burchfiel, now at Massachusetts Institute of Technology (MIT), who in 1968 had carried out fieldwork in Yugoslavia, and returned home to discover Le Pichon’s paper. By knowing the relative motions between Africa and North America and between Europe and North America, Le Pichon had predicted the motion between Africa and Europe for the previous 80 million years, a history that included not only the present-day convergence between Africa and Europe, but also periods when these two regions moved in different directions relative to one another, including a period when they diverged from one another. This history of relative plate motion wrote a complex history on the rock record of the region affected by the relative movement of Africa and Europe. Nevertheless, Burchfiel had inferred from the geologic history of this rock the times of major changes and had inferred what tectonic processes (convergence, divergence, and directions of relative movement) might be occurring at these times. Le Pichon’s calculated plate motions, from data solely in the Atlantic Ocean, predicted many of Burchfiel’s observations and inferences. A new idea becomes believable when it predicts something that has not yet been measured or explained, especially when the idea is really trying to explain other facts.
Péter Molnár (Plate Tectonics: A Very Short Introduction (Very Short Introductions))
Bone beds turn up sporadically elsewhere, with spectacular examples in the Dinosaur National Monument in the USA and in Mongolia’s Gobi desert. In eastern England there are several within the early Cretaceous strata, which include, as well as bones, structures termed coprolites, some of which represent the petrified faeces of dinosaurs or marine reptiles. In the middle of the 19th century, when England’s population was booming and the farmers were struggling to feed everybody, it was discovered that these fragments (which, being bone, are phosphate-rich) made a superb fertilizer when crushed and acid-treated. A thriving and highly profitable industry formed to quarry away these ‘coprolite beds’. Some considerable figures were involved in this industry. John Henslow, Charles Darwin’s beloved mentor of his time at Cambridge, seems to have first encouraged the farmers of eastern England to use such fossil manure. William Buckland also became involved. An extraordinary combination of early savant of geology at Oxford and Dean of Westminster, he was the first to scientifically describe a dinosaur ( Megalosaurus); carried out his fieldwork in academic gown; reputedly ate his way through the entire animal kingdom; and coined the term ‘coprolite’, using these petrified droppings to help reconstruct the ecology of ancient animals. Later, he energetically collaborated with the celebrated German chemist Justus Liebig (who had worked out how to chemically treat these fossil phosphates to make fertilizer) to show how they could be used by agriculturalists, once demonstrating their efficacy by exhibiting, in Oxford’s Ashmolean Museum, a turnip, a yard in circumference, that he had grown with such prehistoric assistance. It is related strata (geologically rare phosphate-rich deposits, usually biologically formed) that are still a mainstay—if a rapidly depleting one—of modern agriculture. In a very real sense, these particular rocks are keeping us all alive.
Jan Zalasiewicz (Rocks: A Very Short Introduction (Very Short Introductions))
It was one of the reasons he fell in love with her shortly afterward and why they’d stayed in love for nearly seven years of monogamy. Nita, Nita . . . The mind’s picture was always of her seated behind their house at dusk, where the cries of children were drowned in the whistle of a night train for Suez; where cinders came to lodge in pores beginning to widen under the stresses of some heart’s geology (“Your complexion is going from bad to worse,” he’d say: “I’ll have to start paying more attention to the lovely young French girls who are always making eyes at me.” “Fine,” she’d retort, “I’ll tell that to the baker when he comes to sleep with me tomorrow, it’ll make him feel better”);
Thomas Pynchon (V.)
Punctuated equilibrium,” Lin said, “is a theory proposed in 1972 by Niles Eldredge and Stephen Jay Gould. Before that time, evolutionary biologists had debated how new species developed. Most thought it happened gradually over time—what we call phyletic gradual evolution. But the fossil record doesn’t support that. It shows that when a species emerges, it is generally stable, with little genetic change, for long stretches of time. When evolution does occur, it happens rapidly—new species branch off in a relatively short period of time. On a geological scale,
A.G. Riddle (Genome (The Extinction Files, #2))
Punctuated equilibrium,” Lin said, “is a theory proposed in 1972 by Niles Eldredge and Stephen Jay Gould. Before that time, evolutionary biologists had debated how new species developed. Most thought it happened gradually over time—what we call phyletic gradual evolution. But the fossil record doesn’t support that. It shows that when a species emerges, it is generally stable, with little genetic change, for long stretches of time. When evolution does occur, it happens rapidly—new species branch off in a relatively short period of time. On a geological scale, anyway.
A.G. Riddle (Genome (The Extinction Files, #2))
In their important masterpiece entitled When the Earth Nearly Died, Allan and Delair write: In Europe immense herds of diverse animals utterly vanished off the face of the earth for no obvious biological reason Coincident with this dreadful slaughter upon the land was the deposition of myriads of contemporary marine shells, and the stranding at great elevations of marine mammals, porpoises, walruses and seals In Siberia, the picture is everywhere one of appalling disorder, carnage and wholesale destruction, with countless animals and plants frozen in positions of death ever since the day they perished. As a result, their remains are amazingly fresh-looking and are frequently indistinguishable from those of animals and plants that have died mere weeks ago The magnitude of the biological extinctions achieved by the Deluge almost transcends the imagination. It annihilated literally billions of biological units of both sexes and every age indiscriminately. Only incredibly powerful flood waters operating world-wide could have achieved such results, and only a flood produced by the means previously suggested could have operated globally They comment on the preposterous Ice Age theories of their predecessors. Although these theories hold little water, they are accepted by supposedly intelligent people. ...it is astonishing that such an unscientific explanation ever came to be formulated, yet in a short time both it and the concept of immense thick ice-sheets descending from a hypothetical northern mountain system, to cover all of northern and eastern North America and western and northern Eurasia, was enthusiastically embraced...as virtually established fact The evidence is perfectly unambiguous. Along with the removal of an “Ice Age” like that which has been hitherto commonly envisaged, the evidence suggests that there is something seriously amiss with the last phases of standard geological chronology Evidence thus converges from numerous directions to support the conclusion that, on the testimony of radio-carbon and other dating techniques, immense physical and climatic changes occurred on earth some 11,000 years or so ago – when an Ice Age that probably never existed came to an end, and an apparently uniformitarian regime was abruptly terminated The gigantic worldwide tectonic disturbances of the ‘late Pleistocene’ times occurred almost simultaneously on a nearly unimaginable scale – precisely what could be expected from a powerful external influence but not from the ‘Ice Age’ conditions conventionally believed to have existed then They note the change in the magnetic fields that occurred during the cataclysmic period of Earth’s recent history: Significantly, a drop in the strength of the earth’s magnetic field appears to have occurred sometime between 13,750 and 12,350 years ago...attended by various other important changes, including earthquakes, vulcanism, water table fluctuations and large scale climatic variations. Of these, severe earthquakes in particular may even induce axial wobble, and polarity reversals
Michael Tsarion (Atlantis, Alien Visitation and Genetic Manipulation)
Fast-forward to March 17, 2014, when the Los Angeles Times was the first news company to break a story about a nearby earthquake. Their edge? The article was written entirely by a robot—a computer program that scans streams of data, like that from the U.S. Geological Survey, and puts together short pieces faster than any newsroom chain of command could. This program earned the paper a few minutes of lead time at most, but today, those minutes are critical.
Stanley McChrystal (Team of Teams: New Rules of Engagement for a Complex World)