Geology Rocks Quotes

A poet once said, 'The whole universe is in a glass of wine.' We will probably never know in what sense he meant it, for poets do not write to be understood. But it is true that if we look at a glass of wine closely enough we see the entire universe. There are the things of physics: the twisting liquid which evaporates depending on the wind and weather, the reflection in the glass; and our imagination adds atoms. The glass is a distillation of the earth's rocks, and in its composition we see the secrets of the universe's age, and the evolution of stars. What strange array of chemicals are in the wine? How did they come to be? There are the ferments, the enzymes, the substrates, and the products. There in wine is found the great generalization; all life is fermentation. Nobody can discover the chemistry of wine without discovering, as did Louis Pasteur, the cause of much disease. How vivid is the claret, pressing its existence into the consciousness that watches it! If our small minds, for some convenience, divide this glass of wine, this universe, into parts -- physics, biology, geology, astronomy, psychology, and so on -- remember that nature does not know it! So let us put it all back together, not forgetting ultimately what it is for. Let it give us one more final pleasure; drink it and forget it all!

That's Third Thoughts for you. When a huge rock is going to land on your head, they're the thoughts that think: Is that an igneous rock, such as granite, or is it sandstone?

You want fantasy? Here's one... There's this species that lives on a planet a few miles above molten rock and a few miles below a vacuum that'd suck the air right out of them. They live in a brief geological period between ice ages, when giant asteroids have temporarily stopped smacking into the surface. As far as they can tell, there's nowhere else in the universe where they could stay alive for ten seconds. And what do they call their fragile little slice of space and time? They call it real life.

When the climbers in 1953 planted their flags on the highest mountain, they set them in snow over the skeletons of creatures that had lived in the warm clear ocean that India, moving north, blanked out. Possibly as much as twenty thousand feet below the seafloor, the skeletal remains had turned into rock. This one fact is a treatise in itself on the movements of the surface of the earth. If by some fiat I had to restrict all this writing to one sentence, this is the one I would choose: The summit of Mt. Everest is marine limestone.

In your hands The dog, the donkey, surely they know They are alive. Who would argue otherwise? But now, after years of consideration, I am getting beyond that. What about the sunflowers? What about The tulips, and the pines? Listen, all you have to do is start and There’ll be no stopping. What about mountains? What about water Slipping over rocks? And speaking of stones, what about The little ones you can Hold in your hands, their heartbeats So secret, so hidden it may take years Before, finally, you hear them?

Everything dreams. The play of form, of being, is the dreaming of substance. Rocks have their dreams, and the earth changes....

The present is the key to the past.

To a naturalist nothing is indifferent; the humble moss that creeps upon the stone is equally interesting as the lofty pine which so beautifully adorns the valley or the mountain: but to a naturalist who is reading in the face of the rocks the annals of a former world, the mossy covering which obstructs his view, and renders indistinguishable the different species of stone, is no less than a serious subject of regret.

No Geologist worth anything is permanently bound to a desk or laboratory, but the charming notion that true science can only be based on unbiased observation of nature in the raw is mythology. Creative work, in geology and anywhere else, is interaction and synthesis: half-baked ideas from a bar room, rocks in the field, chains of thought from lonely walks, numbers squeezed from rocks in a laboratory, numbers from a calculator riveted to a desk, fancy equipment usually malfunctioning on expensive ships, cheap equipment in the human cranium, arguments before a road cut.

That's the thing about rocks--they don't break easily. When I held them, I wanted to be like them-strong and steady, weathered but not broken.

It is well known that stone can think, because the whole of electronics is based on that fact, but in some universes men spend ages looking for other intelligences in the sky without once looking under their feet. That is because they've got the time-span all wrong. From stone's point of view the universe is hardly created and mountain ranges are bouncing up and down like organ-stops while continents zip backward and forward in general high spirits, crashing into each other from the sheer joy of momentum and getting their rocks off. It is going to be quite some time before stone notices its disfiguring skin disease and starts to scratch, which is just as well.

I went into geology because I like being outdoors, and because everybody in geology seemed, well, they all seemed like free spirits or renegades or something. You know, climbing mountains and hiking deserts and stuff.

Look, I don't know what you are, but you're more than a geologist, if you are one at all. I've met lots of geologists on different projects like this, and they're all tiny sunburned men with fetishes for geodes. They wear floppy hats and carry baggies for soil samples around with them. ... And geologists don't make rocks disappear like you did the other night. They keep them and build little shrines to them.

Perhaps I shall not write my account of the Paleolithic at all, but make a film of it. A silent film at that, in which I shall show you first the great slumbering rocks of the Cambrian period, and move from those to the mountains of Wales, from Ordovician to Devonian, on the lush glowing Cotswolds, on to the white cliffs of Dover... An impressionistic, dreaming film, in which the folded rocks arise and flower and grow and become Salisbury Cathedral and York Minster...

Each yoki-hijo trained in an ancient and powerful art. A deliberate, wondrous artistry requiring the full synergy of body and mind. Geological reorganization on the microscale, requiring acute understanding of gravitational equilibrium. In other words, they stacked rocks.

[L]et us not overlook the further great fact, that not only does science underlie sculpture, painting, music, poetry, but that science is itself poetic. The current opinion that science and poetry are opposed is a delusion. ... On the contrary science opens up realms of poetry where to the unscientific all is a blank. Those engaged in scientific researches constantly show us that they realize not less vividly, but more vividly, than others, the poetry of their subjects. Whoever will dip into Hugh Miller's works on geology, or read Mr. Lewes's “Seaside Studies,” will perceive that science excites poetry rather than extinguishes it. And whoever will contemplate the life of Goethe will see that the poet and the man of science can co-exist in equal activity. Is it not, indeed, an absurd and almost a sacrilegious belief that the more a man studies Nature the less he reveres it? Think you that a drop of water, which to the vulgar eye is but a drop of water, loses anything in the eye of the physicist who knows that its elements are held together by a force which, if suddenly liberated, would produce a flash of lightning? Think you that what is carelessly looked upon by the uninitiated as a mere snow-flake, does not suggest higher associations to one who has seen through a microscope the wondrously varied and elegant forms of snow-crystals? Think you that the rounded rock marked with parallel scratches calls up as much poetry in an ignorant mind as in the mind of a geologist, who knows that over this rock a glacier slid a million years ago? The truth is, that those who have never entered upon scientific pursuits know not a tithe of the poetry by which they are surrounded. Whoever has not in youth collected plants and insects, knows not half the halo of interest which lanes and hedge-rows can assume. Whoever has not sought for fossils, has little idea of the poetical associations that surround the places where imbedded treasures were found. Whoever at the seaside has not had a microscope and aquarium, has yet to learn what the highest pleasures of the seaside are. Sad, indeed, is it to see how men occupy themselves with trivialities, and are indifferent to the grandest phenomena—care not to understand the architecture of the universe, but are deeply interested in some contemptible controversy about the intrigues of Mary Queen of Scots!—are learnedly critical over a Greek ode, and pass by without a glance that grand epic... upon the strata of the Earth!

The strata of sedimentary rock are like the pages of a book, each with a record of contemporary life written on it. Unfortunately, the record is far from complete.

GEOLOGY, n. The science of the earth's crust --to which, doubtless, will be added that of its interior whenever a man shall come up garrulous out of a well. The geological formations of the globe already noted are catalogued thus: The Primary, or lower one, consists of rocks, bones or mired mules, gas-pipes, miners' tools, antique statues minus the nose, Spanish doubloons and ancestors. The Secondary is largely made up of red worms and moles. The Tertiary comprises railway tracks, patent pavements, grass, snakes, mouldy boots, beer bottles, tomato cans, intoxicated citizens, garbage, anarchists, snap-dogs and fools.

The Himalayas are the crowning achievement of the Indo-Australian plate. India in the Oligocene crashed head on into Tibet, hit so hard that it not only folded and buckled the plate boundaries but also plowed into the newly created Tibetan plateau and drove the Himalayas five and a half miles into the sky. The mountains are in some trouble. India has not stopped pushing them, and they are still going up. Their height and volume are already so great they are beginning to melt in their own self-generated radioactive heat. When the climbers in 1953 planted their flags on the highest mountain, they set them in snow over the skeletons of creatures that had lived in a warm clear ocean that India, moving north, blanked out. Possibly as much as 20,000 feet below the sea floor, the skeletal remains had turned into rock. This one fact is a treatise in itself on the movements of the surface of the earth. If by some fiat, I had to restrict all this writing to one sentence; this is the one I would choose: the summit of Mount Everest is marine limestone.

Think of a globe, a revolving globe on a stand. Think of a contour globe, whose mountain ranges cast shadows, whose continents rise in bas-relief above the oceans. But then: think of how it really is. These heights are just suggested; they’re there….when I think of walking across a continent I think of all the neighborhood hills, the tiny grades up which children drag their sleds. It is all so sculptured, three-dimensional, casting a shadow. What if you had an enormous globe that was so huge it showed roads and houses- a geological survey globe, a quarter of a mile to an inch- of the whole world, and the ocean floor! Looking at it, you would know what had to be left out: the free-standing sculptural arrangement of furniture in rooms, the jumble of broken rocks in the creek bed, tools in a box, labyrinthine ocean liners, the shape of snapdragons, walrus. Where is the one thing you care about in earth, the molding of one face? The relief globe couldn’t begin to show trees, between whose overlapping boughs birds raise broods, or the furrows in bark, where whole creatures, creatures easily visible, live our their lives and call it world enough. What do I make of all this texture? What does it mean about the kind of world in which I have been set down? The texture of the world, its filigree and scrollwork, means that there is a possibility for beauty here, a beauty inexhaustible in its complexity, which opens to my knock, which answers in me a call I do not remember calling, and which trains me to the wild and extravagant nature of the spirit I seek.

I shall argue that the distinction between a ‘living planet’ – one that is geologically active – and a living cell is only a matter of definition. There is no hard and fast dividing line. Geochemistry gives rise seamlessly to biochemistry. From this point of view, the fact that we can’t distinguish between geology and biology in these old rocks is fitting. Here is a living planet giving rise to life, and the two can’t be separated without splitting a continuum. Move

At first, you fall in love. You wake in the morning woozy and your twilight is lit with astral violet light. You spelunk down into each other until you come to possess some inner vision of each other that becomes one thing. Us. Together. And time passes. Like the forming of Earth itself, volcanoes rise and spew lava. Oceans appear. Rock plates shift. Sea turtles swim half the ocean to lay eggs on the mother island; songbirds migrate over continents for berries from a tree. You evolve--cosmically and geologically. You lose each other and find each other again. Every day. Until love gathers the turtles and the birds of your world and encompasses them, too.

Ms. Terwilliger didn’t have a chance to respond to my geological ramblings because someone knocked on the door. I slipped the rocks into my pocket and tried to look studious as she called an entry. I figured Zoe had tracked me down, but surprisingly, Angeline walked in. "Did you know," she said, "that it’s a lot harder to put organs back in the body than it is to get them out?" I closed my eyes and silently counted to five before opening them again. “Please tell me you haven’t eviscerated someone.” She shook her head. “No, no. I left my biology homework in Miss Wentworth’s room, but when I went back to get it, she’d already left and locked the door. But it’s due tomorrow, and I’m already in trouble in there, so I had to get it. So, I went around outside, and her window lock wasn’t that hard to open, and I—” "Wait," I interrupted. "You broke into a classroom?" "Yeah, but that’s not the problem." Behind me, I heard a choking laugh from Ms. Terwilliger’s desk. "Go on," I said wearily. "Well, when I climbed through, I didn’t realize there was a bunch of stuff in the way, and I crashed into those plastic models of the human body she has. You know, the life size ones with all the parts inside? And bam!" Angeline held up her arms for effect. "Organs everywhere." She paused and looked at me expectantly. "So what are we going to do? I can’t get in trouble with her." "We?" I exclaimed. "Here," said Ms. Terwilliger. I turned around, and she tossed me a set of keys. From the look on her face, it was taking every ounce of self-control not to burst out laughing. "That square one’s a master. I know for a fact she has yoga and won’t be back for the rest of the day. I imagine you can repair the damage—and retrieve the homework—before anyone’s the wiser.” I knew that the “you” in “you can repair” meant me. With a sigh, I stood up and packed up my things. “Thanks,” I said. As Angeline and I walked down to the science wing, I told her, “You know, the next time you’ve got a problem, maybe come to me before it becomes an even bigger problem.” "Oh no," she said nobly. "I didn’t want to be an inconvenience." Her description of the scene was pretty accurate: organs everywhere. Miss Wentworth had two models, male and female, with carved out torsos that cleverly held removable parts of the body that could be examined in greater detail. Wisely, she had purchased models that were only waist-high. That was still more than enough of a mess for us, especially since it was hard to tell which model the various organs belonged to. I had a pretty good sense of anatomy but still opened up a textbook for reference as I began sorting. Angeline, realizing her uselessness here, perched on a far counter and swing her legs as she watched me. I’d started reassembling the male when I heard a voice behind me. "Melbourne, I always knew you’d need to learn about this kind of thing. I’d just kind of hoped you’d learn it on a real guy." I glanced back at Trey, as he leaned in the doorway with a smug expression. “Ha, ha. If you were a real friend, you’d come help me.” I pointed to the female model. “Let’s see some of your alleged expertise in action.” "Alleged?" He sounded indignant but strolled in anyways. I hadn’t really thought much about asking him for help. Mostly I was thinking this was taking much longer than it should, and I had more important things to do with my time. It was only when he came to a sudden halt that I realized my mistake. "Oh," he said, seeing Angeline. "Hi." Her swinging feet stopped, and her eyes were as wide as his. “Um, hi.” The tension ramped up from zero to sixty in a matter of seconds, and everyone seemed at a loss for words. Angeline jerked her head toward the models and blurted out. “I had an accident.” That seemed to snap Trey from his daze, and a smile curved his lips. Whereas Angeline’s antics made me want to pull out my hair sometimes, he found them endearing.

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.

Light. Space. Light and space without time, I think, for this is a country with only the slightest traces of human history. In the doctrine of the geologists with their scheme of ages, eons and epochs all is flux, as Heraclitus taught, but from the mortally human point of view the landscape of the Colorado is like a section of eternity- timeless. In all my years in the canyon country I have yet see a rock fall, of its own volition, so to speak, aside from floods. To convince myself of the reality of change and therefore time I will sometimes push a stone over the edge of a cliff and watch it descend and wait- lighting my pipe- for the report of its impact and disintegration to return. Doing my bit to help, of course, aiding natural processes and verifying the hypotheses of geological morphology. But am not entirely convinced.

The black rock was sharp-edged, hot, and hard as corundum; it seemed not merely alien but impervious to life. Yet on the southern face of almost every rock the lichens grew, yellow, rusty-brown, yellow-green, like patches of dirty paint daubed on the stone.

As Hiro crests the pass on his motorcycle at five in the morning, the town of Port Sherman, Oregon, is suddenly laid out before him: a flash of yellow loglo wrapped into a vast U-shaped valley that was ground out of the rock, a long time ago, by a big tongue of ice in an epochal period of geological cunnilingus.

Life has made our planet the place it is, interacting with the geology and incorporating itself into the ground rock that makes up Earth. But we must remember that we are quite literally made of stardust and we will, in the far and distant future, when our Sun has taken its final breaths, return to stardust once again

But what the world remembered was her beauty. She was not just beautiful like some people think of beautiful, for her beauty was not just for herself. It was the kind of beauty that didn't kill or isolate. She made everything and everyone that saw her or that she saw, touched or walked over want to live a little longer just from the hope of seeing her again. The world flowered and grew wherever she passed. When she brushed by them, wild orchids and lilies mutated into forms and colors never seen before. Even rocks would sparkle, split and crumble into smaller chunks, then grow their ecstatic fragments back into cliffs, defying time and geology, and all because they felt her sueded feet step upon them.

Carnal, rocks remember when they were mountains.' They stared at the rocks in the garden. 'And what do mountains remember?' 'When they were ocean floors.' Big Angel, Zen master.

Rocks are the ticking clock that measure the age of the Earth.

When I break a rock open with my pick, I'm a prophet. I see the past. I see the future. I know where the world is going, and where it's been. And I always, always want to know more.

Lyell and Poulett Scrope, in this country, resumed the work of the Italians and of Hutton; and the former, aided by a marvellous power of clear exposition, placed upon an irrefragable basis the truth that natural causes are competent to account for all events, which can be proved to have occurred, in the course of the secular changes which have taken place during the deposition of the stratified rocks. The publication of 'The Principles of Geology,' in 1830, constituted an epoch in geological science. But it also constituted an epoch in the modern history of the doctrines of evolution, by raising in the mind of every intelligent reader this question: If natural causation is competent to account for the not-living part of our globe, why should it not account for the living part?

The extreme rarity of transitional forms in the fossil record persists as the trade secret of paleontology. The evolutionary trees that adorn our text- books have data only at the tips and nodes of their branches; the rest is inference, however reasonable, not the evidence of fossils. Yet Darwin was so wedded to gradualism that he wagered his entire theory on a denial of this literal record: "The geological record is extremely imperfect and this fact will to a large extent explain why we do not find interminable varieties, connecting together all the extinct and existing forms of life by the finest graduated steps, He who rejects these views on the nature of the geological record, will rightly reject my whole theory." Darwin's argument still persists as the favored escape of most paleontologists from the embarrassment of a record that seems to show so little of evolution. In exposing its cultural and methodological roots, I wish in no way to impugn the potential validity of gradualism (for all general views have similar roots). I wish only to point out that it was never -seen- in the rocks. Paleontologists have paid an exorbitant price for Darwin's argument. We fancy ourselves as the only true students of life's history, yet to preserve our favored account of evolution by natural selection we view our data as so bad that we never see the very process we profess to study. [Evolution’s Erratic Pace - "Natural History," May, 1977]

The rock I'd seen in my life looked dull because in all ignorance I'd never thought to knock it open. People have cracked ordinary New England pegmatite - big, coarse granite - and laid bare clusters of red garnets, or topaz crystals, chrysoberyl, spodumene, emerald. They held in their hands crystals that had hung in a hole in the dark for a billion years unseen. I was all for it. I would lay about me right and left with a hammer, and bash the landscape to bits. I would crack the earth's crust like a piñata and spread to the light the vivid prizes in chunks within. Rock collecting was opening the mountains. It was like diving through my own interior blank blackness to remember the startling pieces of a dream: there was a blue lake, a witch, a lighthouse, a yellow path. It was like poking about in a grimy alley and finding an old, old coin. Nothing was at it seemed. The earth was like a shut eye. Mother's not dead, dear - she's only sleeping. Pry open the thin lid and find a crystalline intelligence inside, a rayed and sidereal beauty. Crystals grew inside rock like arithmetical flowers. They lengthened and spread, adding plane to plane in awed and perfect obedience to an absolute geometry that even the stones - maybe only the stones - understood.

But Geology carries the day: it is like the pleasure of gambling, speculating, on first arriving, what the rocks may be; I often mentally cry out 3 to 1 Tertiary against primitive; but the latter have hitherto won all the bets.

The mountains in the background were cut from the same cloth as the sky: a slightly darker shade, that was the only difference. Had we the capacity to analyse it there would almost certainly be a geology of the air as well as of rock.

With each integer on the Richter scale, there is a tenfold increase in the number of earthquakes that occur annually. On average, there is one magnitude 8 event, ten magnitude 7 events, a hundred magnitude 6 events, and so on, each year. If we consider this from an energy standpoint, the smaller earthquakes account for a significant fraction of the total seismic energy released each year. The one million magnitude 2 events (which are too small to be felt except instrumentally) collectively release as much energy as does one magnitude 6 earthquake. Although the larger events are certainly more devastating from a human perspective, they are geologically no more important than the myriad less newsworthy small ones.

Little by little, over more than two centuries, the local stories told by rocks in all parts of the world have been stitched together into a great global tapestry - the geologic timescale. This "map" of Deep Time represents one of the great intellectual achievements of humanity, arduously constructed by stratigraphers, paleontologists, geochemists, and geochronologists from many cultures and faiths. It is still a work in progress to which details are constantly being added and finer and finer calibrations being made.

Another day I walked out of town to do a bit of climbing in the mountains behind the airport. I scrambled up and down slopes that contained some of the oldest rocks in the world, isotope-dated at 3,800 billion years, remnants, so the geological rumor goes, of the earth's earliest terrestrial crust.

Within those margins is Denali, a 144-square-mile mass of rock, snow, and ice that rises abruptly from a 2,000-foot plateau, soaring 18,000 feet from base to summit, the greatest vertical relief of any mountain on Earth, with the exception of the Hawaiian seamount Mauna Kea, the bulk of which lies beneath the Pacific Ocean. In comparison, Mount Everest, though 29,029 feet above sea level, rests on the 17,000-foot-high Tibetan Plateau and rises just 12,000 feet from base to summit. A similar plateau boosts the Andes; without those geologic booster seats, those peaks all would lie in Denali’s shadow.

To my surprise, I found that geology demanded a type of whole-brain thinking I hadn't encountered before. It creatively appropriated ideas from physics and chemistry for the investigation of unruly volcanoes and oceans and ice sheets, It applied scholarly habits one associates with the study of literature and the arts - the practice of close reading, sensitivity to allusion and analogy, capacity for spatial visualization - to the examination of rocks. Its particular form of inferential logic demanded mental versatility and a vigorous but disciplined imagination. And its explanatory power was vast; it was nothing less than the etymology of the world.

I was teaching introductory geology at Caltech for the first time. I’m not a geologist. I’ve never taken a single class in geology. If you gave me a handful of different types of rocks, chances are I could identify only a small number of them. I still get confused by the meanings of strike and dip. Luckily, most of my students didn’t realize this.

He reached into the box to pick up a smooth, curiously shaped object that I thought looked like the end of a leg bone. I was disappointed when he said, “This is a sandstone concretion. Not a bone.” “How do you know?” I asked. “I have a PhD in paleontology and a master's degree in geology, Mike. I know bones and rocks.” - Exchange between Mike and Pick

It is almost impossible to understand the extent to which upheaval agitated, and by that very fact had temporarily enriched, the mind of M. de Charlus. Love in this way produces real geological upheavals of thought. In the mind of M. de Charlus, which only several days before resembled a plane so flat that even from a good vantage point one could not have discerned an idea sticking up above the ground, a mountain range had abruptly thrust itself into view, hard as rock--but mountains sculpted as if an artist, instead of taking the marble away, had worked it on the spot, and where there twisted about one another, in giant and swollen groupings, Rage, Jealousy, Curiosity, Envy, Suffering, Pride, Astonishment, and Love.

Sorgan tried his very best not to think about how long it must have taken for a stream that small to eat its way down through solid rock to form its current bed. Sorgan knew exactly what the word “hundred” meant, but when numbers wandered off toward “thousand”—or even “million”—and the people who used those terms were talking about years, Sorgan’s mind shied back in horror.

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.

When you die, the surface of the moon will not change. The difference between the landscape and lighting of that barren little world from a moment where you exist, to a moment where you do not, will be minimal, and unrelated to your passing. From a car window driving on a highway, looking up at a moon framed by incidental clouds, the surface will be the same muddle of mystery and distance it always is. And even a methodical study of your absence as it pertains to moon geology and cartography will find nothing. Searching through a powerful telescope, and analyzing with computer algorithms built around your nonexistence – even that study will find that all craters and rocks appear to be where we left them a few years back, that it is the same distance, orbiting at the same rate, and that the researches feel just the way they did about the moon as they did before you died. Nothing will change about the moon when you die. It will be the same – still the moon, still there. Still the moon.

In the case of those solids, whether of earth, or rock, which enclose on all sides and contain crystals, selenites, marcasites, plants and their parts, bones and the shells of animals, and other bodies of this kind which are possessed of a smooth surface, these same bodies had already become hard at the time when the matter of the earth and rock containing them was still fluid. And not only did the earth and rock not produce the bodies contained in them, but they did not even exist as such when those bodies were produced in them.

While Azelio and Tarquinia debated the merits of different landing sites, Ramiro clung to a rope beside the window and gazed down at the starlit world below. How could he understand Esilio? Of all the sciences he’d studied as a child, geology had been the least developed – and at the time, he’d imagined, the least likely ever to be of use to him. Of the little that he remembered, he remained unsure what he should trust. The ancestors had had no idea what a rock was actually made of, while their successors, with all their superior knowledge, had never set eyes on a planet.

Glaciers used to be fun, even thrilling. It’s hard to believe now, but there was a time when geology was much like genetics today, the cutting-edge inquiry that routinely delivered breathtaking insights that captivated the educated world. Many of those insights, starting in the mid-1700s, had to do with the age of the Earth, as people looking closely at rocks found evidence that our planet was a lot older than the 6,000 years suggested by the Old Testament—​perhaps many millions of years older. For this reason, the nineteenth century is said to have discovered “deep time,” the astronomical and geological time scales that reach into pasts so distant that our minds struggle to imagine them.

Geologists think the mountains were formed by several distinct tectonic events over the course of 500 million years, a span of time that represents a thick slice of the planet's geological record. The Appalachians once soared as high as the Rockies or even higher. They were most recently thrust upward about 290 million years ago, which makes these mountains older than the bones of the first dinosaurs. They predate the appearance of deciduous trees. They are older than flowers. There were mountains here before the Earth had ever seen anything as fantastic as grass. Some of the rocks were formed in the Precambrian Era, in that gray epoch when life was pondering a wholesale leap from one cell to many.

A far cicada rings high and clear over the river’s heavy wash. Morning glory, a lone dandelion, cassia, orchids. So far from the nearest sea, I am taken aback by the sight of a purple land crab, like a relict of the ancient days when the Indian subcontinent, adrift on the earth’s mantle, moved northward to collide with the Asian landmass, driving these marine rocks, inch by inch, five miles into the skies. The rise of the Himalaya, begun in the Eocene, some fifty million years ago, is still continuing: an earthquake in 1959 caused mountains to fall into the rivers and changed the course of the great Brahmaputra, which comes down out of Tibet through northeastern India to join the Ganges near its delta at the Bay of Bengal.

Push up some mountains. Cut them down. Drown the land under the sea. Push up some more mountains. Cut them down. Push up a third set of mountains, and let the river cut through them. “Unconformity” is the geologic term for an old, eroded land surface buried under younger rock layers. Put your outspread hand over the Carlin Canyon, Nevada unconformity and your fingers span roughly forty million years- the time that it took to bevel down the first set of mountains and deposit the younger layers on top. What is forty million years? Enough time for a small predatory dinosaur to evolve into a bird. Enough time for a four-legged, deer-like mammal to evolve into a whale. And far more than enough time to turn an ape-like creature in eastern Africa into a big-brained biped who can marvel at such things. The Grand Canyon’s Great Unconformity divides 1.7 billion-year-old rock from 550 million-year-old rock, a gap of more than one billion years. One billion years. I earn my salary studying the Earth and teaching its history, but I admit utter helplessness in comprehending such a span. A billion pages like those of this book would stack up more than forty miles. I had lived one bullion seconds a few days before my thirty-second birthday. A tape measure one billion inches long would stretch two-thirds of the way around the Earth. Such analogies hint at what deep time means- but they don’t get us there. “The human mind may not have evolved enough to be able to comprehend deep time," John McPhee once observed, “it may only be able to measure it.

Unkar Delta at Mile 73 The layers of brick red sandstone, siltstone, and mudstone of the Dox formation deposited a billion years ago, erode easily, giving the landscape an open, rolling character very different that the narrow, limestone walled canyon upstream, both in lithology and color, fully fitting Van Dyke’s description of “raspberry-red color, tempered with a what-not of mauve, heliotrope, and violet.” Sediments flowing in from the west formed deltas, floodplains, and tidal flats, which indurated into these fine-grained sedimentary rocks thinly laid deposits of a restful sea, lined with shadows as precise as the staves of a musical score, ribboned layers, an elegant alteration of quiet siltings and delicious lappings, crinkled water compressed, solidified, lithified.

Even more difficult to explain, than the breaking-up of a single mass into fragments, and the drifting apart of these blocks to form the foundations of the present-day continents, is the explanation of the original production of the single mass, or PANGAEA, by the concentration of the former holosphere of granitic sial into a hemisphere of compressed and crushed gneisses and schists. Creep and the effects of compression, due to shrinking or other causes, have been appealed to but this is hardly a satisfactory explanation. The earth could no more shrug itself out of its outer rock-shell unaided, than an animal could shrug itself out of its hide, or a man wriggle out of his skin, or even out of his closely buttoned coat, without assistance either of his own hands or those of others.

We tend to imagine stone as inert matter, obdurate in its fixity. But here in the rift it feels instead like a liquid briefly paused in its flow. Seen in deep time, stone folds as strata, gouts as lava, floats as plates, shifts as shingle. Over aeons, rock absorbs, transforms, levitates from seabed to summit. Down here, too, the boundaries between life and not-life are less clear. I think of the discovery of the bones in Aveline’s, shining with calcite, lying promiscuously, almost converted into stone . . . I slip out the whalebone owl, feel the Braille of its back, the arcs of its wings, thinking of how it had taken flight from a whale’s beached ribs. We are part mineral beings too – our teeth are reefs, our bones are stones – and there is a geology of the body as well as of the land. It is mineralization – the ability to convert calcium into bone – that allows us to walk upright, to be vertebrate, to fashion the skulls that shield our brains.

Half a century ago Ostwald (1910) distinguished classicists and romanticists among the scientific investigators: the former being inclined to design schemes and to use consistently the deductions from working hypotheses; the latter being more fit for intuitive discoveries of functional relations between phenomena and therefore more able to open up new fields of study. Examples of both character types are Werner and Hutton. Werner was a real classicist. At the end of the eighteenth century he postulated the theory of “neptunism,” according to which all rocks including granites, were deposited in primeval seas. It was an artificial scheme, but, as a classification system, it worked quite satisfactorily at the time. Hutton, his contemporary and opponent, was more a romanticist. His concept of 'plutonism' supposed continually recurrent circuits of matter, which like gigantic paddle wheels raise material from various depths of the earth and carry it off again. This is a very flexible system which opens the mind to accept the possible occurrence in the course of time of a great variety of interrelated plutonic and tectonic processes.

I still have no choice but to bring out Minerva instead.” “But Minerva doesn’t care about men,” young Charlotte said helpfully. “She prefers dirt and rocks.” “It’s called geology,” Minerva said. “It’s a science.” “It’s certain spinsterhood, is what it is! Unnatural girl. Do sit straight in your chair, at least.” Mrs. Highwood sighed and fanned harder. To Susanna, she said, “I despair of her, truly. This is why Diana must get well, you see. Can you imagine Minerva in Society?” Susanna bit back a smile, all too easily imagining the scene. It would probably resemble her own debut. Like Minerva, she had been absorbed in unladylike pursuits, and the object of her female relations’ oft-voiced despair. At balls, she’d been that freckled Amazon in the corner, who would have been all too happy to blend into the wallpaper, if only her hair color would have allowed it. As for the gentlemen she’d met…not a one of them had managed to sweep her off her feet. To be fair, none of them had tried very hard. She shrugged off the awkward memories. That time was behind her now. Mrs. Highwood’s gaze fell on a book at the corner of the table. “I am gratified to see you keep Mrs. Worthington close at hand.” “Oh yes,” Susanna replied, reaching for the blue, leatherbound tome. “You’ll find copies of Mrs. Worthington’s Wisdom scattered everywhere throughout the village. We find it a very useful book.” “Hear that, Minerva? You would do well to learn it by heart.” When Minerva rolled her eyes, Mrs. Highwood said, “Charlotte, open it now. Read aloud the beginning of Chapter Twelve.” Charlotte reached for the book and opened it, then cleared her throat and read aloud in a dramatic voice. “’Chapter Twelve. The perils of excessive education. A young lady’s intellect should be in all ways like her undergarments. Present, pristine, and imperceptible to the casual observer.’” Mrs. Highwood harrumphed. “Yes. Just so. Hear and believe it, Minerva. Hear and believe every word. As Miss Finch says, you will find that book very useful.” Susanna took a leisurely sip of tea, swallowing with it a bitter lump of indignation. She wasn’t an angry or resentful person, as a matter of course. But once provoked, her passions required formidable effort to conceal. That book provoked her, no end. Mrs. Worthington’s Wisdom for Young Ladies was the bane of sensible girls the world over, crammed with insipid, damaging advice on every page. Susanna could have gleefully crushed its pages to powder with a mortar and pestle, labeled the vial with a skull and crossbones, and placed it on the highest shelf in her stillroom, right beside the dried foxglove leaves and deadly nightshade berries. Instead, she’d made it her mission to remove as many copies as possible from circulation. A sort of quarantine. Former residents of the Queen’s Ruby sent the books from all corners of England. One couldn’t enter a room in Spindle Cove without finding a copy or three of Mrs. Worthington’s Wisdom. And just as Susanna had told Mrs. Highwood, they found the book very useful indeed. It was the perfect size for propping a window open. It also made an excellent doorstop or paperweight. Susanna used her personal copies for pressing herbs. Or occasionally, for target practice. She motioned to Charlotte. “May I?” Taking the volume from the girl’s grip, she raised the book high. Then, with a brisk thwack, she used it to crush a bothersome gnat. With a calm smile, she placed the book on a side table. “Very useful indeed.

Through the spectacles of geology, terra firms becomes terra mobilis, and we are forced to reconsider our beliefs of what is solid and what is not. Although we attribute to stone great power to hold back time, to refuse its claims (cairns, stone tablets, monuments, statuary), this is true only in relation to our own mutability. Looked at in the context of the bigger geological picture, rock is as vulnerable to change as any other substance. Above all, geology makes explicit challenges to our understanding of time. It giddies the sense of here-and-now. The imaginative experience of what the writer John McPhee memorably called 'deep time' - the sense of time whose units are not days, hours, minutes or seconds but millions of years or tens of millions of years - crushes the human instant; flattens it to a wafer. Contemplating the immensities of deep time, you face, in a way that is both exquisite and horrifying, the total collapse of your present, compacted to nothingness by the pressures of pasts and futures too extensive to envisage. And it is a physical as well as a cerebral horror, for to acknowledge that the hard rock of a mountain is vulnerable to the attrition of time is of necessity to reflect on the appalling transience of the human body.

To not be cut off, however, we need to be moving in a rhythm that is syncopated with that of the oaks and willows, heartbeats and touch. We must recall the original cadence of the soul. One of my most memorable teachings about slowing down came from my mentor, Clarke Berry, a Jungian analyst with whom I apprenticed, following licensure. I was young, and I knew I was in need of a mentor, someone who could teach me the art of sitting with others in therapy. The Jung Institute in San Francisco referred me to Clarke along with other analysts, but when I met him, I knew I was in the right place. Our first meeting, over thirty years ago, was unforgettable. When we sat down, Clarke reached to his left, placed his hand on a large rock lying on a table, and said, “This is my clock. I operate at geologic speed. And if you are going to work with the soul, you need to learn this rhythm, because this is how the soul moves.” Then he pointed to a small clock also sitting there and added, “It hates this.” What an amazing thing to tell this young therapist. It is the single most important thing I ever learned about therapy, about working with the soul. I share this story with every person I work with; I use it as a means of calming the urgency to change and helping patients return to a rhythm that enables them to listen once again to their own soul.

It seems to Marithe that her life has undergone two changes: one, when her father left. And two, about a year ago, when she turned thirteen, when her life and the way she felt about it and the way she viewed it suddenly tilted; like the deck of a ship in a storm. At first it seemed to her that her house, her family, her dogs, her accordion, her books, her room with its geology samples, its display of feathers, its pictures of foxes and wolves, all took on an unreal aspect. Everything felt like a stage set: she kept viewing herself as if from the outside. Instead of just acting, just doing, just running or speaking or playing or collecting, she would feel this sense of externalisation: and so, a voice inside her head would comment, you are running. Do you need to run? Where are you going? You're picking up that rock but do you want it, do you really need it, are you going to carry it home? [...] And her body! Some mornings she woke and it was as if lead weights had been attached to her limbs by some ill-meaning fairy. Even if she had the urge to walk across the paddock to feed the neighbours' horses -- which she hardly ever did any more, she didn't know why -- she wouldn't have the energy, the sap in her to do it. She wanted it returned to her, Marithe did, that sense of security in her life, of certainty, of knowing who she was and what she was about. Would it ever come back?

The cave was cool and silent- thoroughly carpeted- with the most luxuriant mantle of mosses Alma Whittaker had ever seen. The cave was not merely mossy; it throbbed with moss. It was not merely green; it was frantically green. It was so bright in its verdure that the color nearly spoke, as though- smashing through the world of sight- it wanted to migrate into the world of sound. The moss was a thick, living pelt, transforming every rock surface into a mythical, sleeping beast. Improbably, the deepest corners of the cave glittered the brightest; they were absolutely studded, Alma realized with a gasp, with the jewellike filigree of 'Schistotega pennata.' Goblin's gold, dragon's gold, elfin gold- 'Schistotega pennata' was that rarest of cave mosses, that false gem that gleams like a cat's eye from within the permanent twilight of geologic shade, that unearthly sparkling plant that needs but the briefest sliver of light each day to sparkle like glory forever, that brilliant trickster whose shining facets have fooled so many travelers over the centuries into believing that they have stumbled upon hidden treasure. But to Alma, this 'was' treasure, more stunning than actual riches, for it bedecked the entire cave in the uncanny, glistering, emerald light that she had only ever before seen in miniature, in glimpses of moss seen through a microscope... yet now she was standing fully within it.

It starts with a thwack, the sharp crack of hard plastic against a hot metal surface. When the ladle rolls over, it deposits a pale-yellow puddle of batter onto the griddle. A gentle sizzle, as the back of the ladle sparkles a mixture of eggs, flour, water, and milk across the silver surface. A crepe takes shape. Next comes cabbage, chopped thin- but not too thin- and stacked six inches high, lightly packed so hot air can flow freely and wilt the mountain down to a molehill. Crowning the cabbage comes a flurry of tastes and textures: ivory bean sprouts, golden pebbles of fried tempura batter, a few shakes of salt, and, for an extra umami punch, a drift of dried bonito powder. Finally, three strips of streaky pork belly, just enough to umbrella the cabbage in fat, plus a bit more batter to hold the whole thing together. With two metal spatulas and a gentle rocking of the wrists, the mass is inverted. The pork fat melts on contact, and the cabbage shrinks in the steam trapped under the crepe. Then things get serious. Thin wheat soba noodles, still dripping with hot water, hit the teppan, dancing like garden hoses across its hot surface, absorbing the heat of the griddle until they crisp into a bird's nest to house the cabbage and crepe. An egg with two orange yolks sizzles beside the soba, waiting for its place on top of this magnificent heap. Everything comes together: cabbage and crepe at the base, bean sprouts and pork belly in the center, soba and fried egg parked on top, a geologic construction of carbs and crunch, protein and chew, all framed with the black and white of thickened Worcestershire and a zigzag of mayonnaise. This is okonomiyaki, the second most famous thing that ever happened to Hiroshima.

The ridge of the Lammer-muir hills... consists of primary micaceous schistus, and extends from St Abb's head westward... The sea-coast affords a transverse section of this alpine tract at its eastern extremity, and exhibits the change from the primary to the secondary strata... Dr HUTTON wished particularly to examine the latter of these, and on this occasion Sir JAMES HALL and I had the pleasure to accompany him. We sailed in a boat from Dunglass ... We made for a high rocky point or head-land, the SICCAR ... On landing at this point, we found that we actually trode [sic] on the primeval rock... It is here a micaceous schistus, in beds nearly vertical, highly indurated, and stretching from S.E. to N. W. The surface of this rock... has thin covering of red horizontal sandstone laid over it, ... Here, therefore, the immediate contact of the two rocks is not only visible, but is curiously dissected and laid open by the action of the waves... On us who saw these phenomena for the first time, the impression will not easily be forgotten. The palpable evidence presented to us, of one of the most extraordinary and important facts in the natural history of the earth, gave a reality and substance to those theoretical speculations, which, however probable had never till now been directly authenticated by the testimony of the senses... What clearer evidence could we have had of the different formation of these rocks, and of the long interval which separated their formation, had we actually seen them emerging from the bosom of the deep? ... The mind seemed to grow giddy by looking so far into the abyss of time; and while we listened with earnestness and admiration to the philosopher who was now unfolding to us the order and series of these wonderful events, we became sensible how much farther reason may sometimes go than imagination can venture to follow.

Lunar Geology Rocks.

There is strong geological evidence that the period from 380 million to 365 million years ago is the critical time. The younger rocks in that range, those about 360 million years old, include diverse kinds of fossilized animals that we would all recognize as amphibians or reptiles ... But in rocks that are about 385 million years old, we find whole fish that look like, well, fish ... it is probably no great surprise that we should focus on rocks about 375 million years old to find evidence of the transition between fish and land-living animals.

…so far, the rocks haven’t provided enough information for geological detectives to distinguish events that may have happened over thousands of years from those that happened over millions.

molten rock and a few miles below a vacuum that’d suck the air right out of them. They live in a brief geological period between ice ages, when giant asteroids have temporarily stopped smacking into the surface. As far as they can tell, there’s nowhere else in the universe where they could stay alive for ten seconds. And what do they call their fragile little slice of space and time? They call it real life. In a universe where it’s known that whole galaxies can explode, they think there’s things like “natural justice” and “destiny.” Some of them even believe in democracy.… I’m a fantasy writer, and even I find it all a bit hard to believe.

out of the ground at nearly two times the global average. Throughout the Basin and Range, heat pours out of the crust at rates that average 50 percent higher than typical for the rest of the Earth. This tells us that hot mantle lies close to the surface below the Basin and Range. Since hot rock is inclined to rise buoyantly, it seems likely that the mantle under the Basin and Range is bulging and spreading like a growing mushroom. This hot, rising mantle both stretches the crust and sustains the high elevations. Taking advantage of the thinned and broken crust above, mantle-derived magmas have jetted upward to stain the Basin and Range landscape with innumerable lava flows and volcanic cones. So, an immense—and ongoing—outpouring of mantle heat appears to have made the Basin and Range and kept it standing high. But what made the heat? For that we turn to the Farallon Plate. IN CHAPTER 7 we saw how the subduction of the Farallon Plate

One million arid acres stretch out in the afternoon sun. The mile-high crust, layers of umber, russet, charcoal, goldenrod, burn sienna, and ochre, exposes two billion years of geologic history. We stand awe-smacked. We're the newest things on earth. Everything at the rim—all of the particles that big-banged themselves through the universe to be alive in just these forms—has been set in motion. Our lives are the vestiges of these events, events that seem to happen ceaselessly. As tired and grief-stricken as I am, there's still a part of me that knows that Richard's loss of memory, the death of his identity, his coming back as a new man, it all has its place in the order of things, or perhaps the chaos of things—just like these ancient, awesome rock formations.

Three dominant hypotheses explain what drives plate tectonic motion. Each one relies on the convention of the mantle — the movement of heated rock materials beneath earth’s crust — but each one focuses on a different piece of the cycle: Mantle convection hypothesis: This hypothesis proposes that heated materials inside the earth move up and down in a circular motion (like the wax in a lava lamp) and the continental plates resting on this mat-erial are moved in the direction of the circular motion. Ridge-push hypothesis: This hypothesis states that the creation of new rock materials along mid-ocean ridges continually pushes oceanic crustal plates upward and outward, so that the far edges are forced into collisions with other plates. Slab-pull hypothesis: This hypothesis is the opposite of the ridge-push model. It proposes that the heavy, dense outer edges of crustal plates sink into the mantle at plate boundaries and pull the rest of the plate along with them.

Grateful for a cop who recognized rocks as evidence, who treated them with the same respect given to fingerprints or cigarette butts or bloodstains or what have you.

If we extrapolate this rate of overturn back in geologic time, the ocean floor has apparently been rejuvenated at least two dozen times since the Earth formed. When Earth was younger and hotter, however, the pace of convection may have been faster, and the ocean floor may have been resurfaced more frequently. But this leads to a conundrum: If convection had been faster in the past, as most geoscientists think it was, ocean crust would have arrived at subduction zones at a younger average age, still too hot and buoyant to be assimilated back into the mantle. This suggests that true plate tectonics, with rigid crustal slabs, efficient recycling of ocean crust via subduction, and water-assisted production of low-temperature melts, may not have occurred on the early Earth. Instead, plate tectonics could begin only when the Earth had reached a degree of thermal maturity, probably about 2.5 billion years ago (around the close of the Archean eon and the beginning of the Proterozoic). Before this, Earth's mixer settings—and the extent to which surface water was stirred back into the interior—were probably different. We can look to rocks formed in these distant times, Earth's record of its childhood and youth, for clues.

One of the reasons I enjoy being with Finlay is his ability to read landscapes back into being, and to hold multiple eras of history in plain sight simultaneously. To each feature and place name he can attach a story - geological, folkloric, historical, gossipy. He moves easily between different knowledge systems and historical eras, in awareness of their discrepancies but stimulated by their overlaps and rhymes. Scatters of stones are summoned up and reconstituted in his descriptions into living crofts. He took me to a green knoll in Baile n Cille in mid-Lewis, and recalled for me the scene in 1827 when a Reverend Dr MacDonald had gathered 7,000 people around the knoll for a mass conversion to Calvinism. A crag-and-tail outcrop of gneiss in the moor drew him back into the Holocene and an explanation of how, after the glaciers had retreated from the Western Isles around 12,000 years ago, the peat began to deepen in the lees of the exposed rock-backs. To Finlay, geography and history are consubstantial. Placeless events are inconceivable, in that everything that happens must happen somewhere, and so history issues from geography in the same way that water issues from a spring: unpredictably but site-specifically.

In your high school geology class you probably were taught that all life on earth exists in a paper-thin shell called the biosphere, which is trapped between thousands of miles of dead rock underfoot, and cold dead radioactive empty space above. Companies that sell OSes exist in a sort of technosphere. Underneath is technology that has already become free. Above is technology that has yet to be developed, or that is too crazy and speculative to be productized just yet. Like the earth’s biosphere, the technosphere is very thin compared to what is above and what is below.

It draws its name from rocks that are characteristic of the Permian geologic age, which ended with the “great extinction” that wiped out most living creatures about 250 million years ago.

a vast U-shaped valley that was ground out of the rock, a long time ago, by a big tongue of ice in an epochal period of geological cunnilingus.

Readers with a background in geology might note at this stage that when you find gold in rock, it doesn’t come in smooth nuggets.

From the Bridge” by Captain Hank Bracker Pebbles, Rocks & Mountains Rocks can be formed in many different ways and are found in just about every corner of our planet, the Moon, up in space and who knows where else. Now pebbles are the mini-me’s of rocks and generally are about one to three inches in size. Geologists will tell you that they are about 5 millimeters in diameter, but who’s counting? In fact there are two beaches that are made up entirely of pebbles such as the Shingle Beach in Somerset, England. Generally pebbles are found along rivers, streams and creeks whereas mountains are usually a part of a chain that was created along geothermal fault lines. The process of Mountain formation is associated with movements of the earth's crust, which is referred to as plate tectonics. See; now that I looked it up, I know these things! What I’m about to say has absolutely nothing to do with geology and everything to do about human nature. In the course of events we never trip over mountains and seldom over rocks, but tripping over pebbles is another thing. Marilyn French, a writer and feminist scholar is credited with saying, “Men (she should have included Women) stumble over pebbles, never over mountains.” She was the lady (I should have said woman) whose provocative 1977 novel, “The Women's Room” captured the frustration and fury of a generation of women fed up with society's traditional conceptions of their roles (and this is true). However, this has nothing to do with the feminist movement and is simply a metaphor. Of course we’re not going to trip over mountains, not unless we are bigger than the “Jolly Green Giant!” and so it’s usually the little things that trip us up and cause us problems. What comes to mind is found on page 466 of The Exciting Story of Cuba. This is a book that won two awards by the “Florida Authors & Publishers Association” and yet there are small mistakes. They weren’t even caused by me or my team and yet there they are, getting bigger and bigger every time I look at them. Now I’m not about to tell you what they are, since that would take the fun out of it, but if you look hard enough in the book, you’ll succeed in discovering them! I will however tell you that one of these mistakes was caused by a computer program called “Word.” It’s wonderful that this program has a spell check and can even correct my grammar, but it can’t read my mind. In its infernal wisdom, the program was so insistent that it was right and that I was wrong that it changed the spelling of, in this case, the name of a person in the middle of the night. It happened while I was sleeping! I would have seen it if it had been as big as a mountain, however being just a little pebble it escaped my review and even escaped the eagle eyes of Lucy who still remains the best proof reader and copy editor that I know. When you discover what I missed please refrain from emailing me, although, normally, I would really enjoy hearing from you! I unfortunately already know most of the errors in the book, for which I take full responsibility. The truth of it is that my mistakes leave me feeling stupid and frustrated. Now, you may disagree with me however I don’t think that I am really all that stupid, but when you write hundreds of thousands of words, a few of them might just slip between the cracks. None of us are infallible and we all make mistakes. I sometimes like to say that “I once thought that I had made a mistake, but then found out that I was mistaken.” And so it is; if you think about it, it’s the pebbles that create most of our problems, not the rocks and certainly not the mountains. I’ll let you know as soon as my other books, Suppressed I Rise – Revised Edition; Seawater One…. And Words of Wisdom, “From the Bridge” are available. It’s Seawater One that has the naughty bits in it… but that just spices it up. Now with that book you can really tell me what you think….

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.

Plastic does take one form, recently discovered, that may in fact last if not forever then for a significant amount of geological time. Some washes up on beaches and ends up in bonfires. In 2006, a strange new kind of rock was discovered on some Hawaiian beaches containing melted plastic binding together bits of rock, sand, shell, and other materials. Some of this tough material, now called plastiglomerate, will become buried and last for many millions of years, a new rock type that has suddenly appeared in Earth’s strata, marking the time when people built things of plastic, scattered them widely, and sometimes burned them on beaches for celebration or warmth. The plastic

Our disagreement rises with the timing of the formation of these rock layers! Where the evolutionists say the fossiliferous rock layers “were laid down slowly over millions of years without any major catastrophes,” the creationists say that “most of these rock layers were deposited by the Flood of Noah’s day.” So it is the same evidence based on the same observations, but we simply have two different interpretations of that evidence. Creationists start with God’s Word, which informs us of the global Flood (e.g., Genesis 7:19–201) that was a major catastrophe about 4,300 years ago

Two different geologists (who simply do not have a hand in this debate since they are secular), who were searching for oil deposits, have mapped the regions that include the mountains of Ararat and beyond extensively.10 What we find are layers intrinsic to the formation of the mountains of Ararat (Armenia and Anatolia regions) that include: 1. Permian 2. Lower-Middle Triassic 3. Middle Triassic-Middle Cretaceous 4. Paleocene-Lower Eocene 5. Lower Eocene 6. Middle Eocene 7. Middle-Upper Miocene For much of this, the Eocene and Miocene rock layers are inverted and pushing up the Cretaceous and Triassic rock layers. In other words, without the Eocene and Miocene rock layers, the mountains of Ararat cannot exist! What can we glean from this? It means that Miocene and Eocene rock layers existed by day 150 in the mountains of Ararat. These layers are tertiary sediments much higher than the K/T boundary. What we can know is that these Eocene and Miocene rock layers were formed prior to the post-Flood period.

the overburden like that they’ve turned the geology upside down. Topsoil is on the bottom and rock that was on the bottom is now on top. Native plants and trees won’t grow in it. So they introduce non-native plantings that are royally screwing up the ecosystem.

vast U-shaped valley that was ground out of the rock, a long time ago, by a big tongue of ice in an epochal period of geological cunnilingus.

Those amazing sheer rock faces, stacked up in layers, as if they were God’s archives, a geological history of the Hebrides. Seams of rock like the rings of a tree, but taking you right back to the very beginnings of time.

There is always some trace, Roger tells me, of the history of things, the impressions humans have left on them. The term for the study of rock layers in geology is stratigraphy, but it is also used in archaeology to describe the technique of seeking out the contexts of rocks, discovering the events that have left detectable traces on their surfaces – in the same way we might scan one another’s bodies, looking for those distinctive lines and marks which tell us something unspoken about the stranger opposite us on the train, or the friend we grew up with but have not seen for years, or the person we are falling in love with. A geologist’s task is to see beyond the ways in which time tries to smooth out difference, examining layers in order to isolate each shift to our world, to feel every fault line. We discuss how hard this is to do this with people, to imagine our lives not as one continuous line, but comprised of hundreds of versions stacked up behind us, and hundreds more ahead of us too, like those pairs of facing mirrors that make your reflection curl up infinitely on either side of you.

Mamo, the Italian word for marble, comes from the Greek marmairein, meaning “to shine”. Geologically speaking, marble is limestone transformed by the heat and pressure of the earth’s crust into a medium-hard, crystalline rock. Cold to the touch, marble yields willingly to the sculptor’s chisel. Over time, white statuary acquires an ivory patina remarkably evocative of the warmth of human flesh.

The decisions made in the next few years by the energy industry and the governments that regulate them will leave a record in the rocks that will last for hundreds of millions of years.

Geology is not the study of stones. It is the study of time. Rocks are the ticking clocks that measure the age of Earth.

It certainly would be if the earth and moon shared the same geologic makeup, but studies of moon rocks had already concluded that that is not the case.

Let your imagination change what you know. Suddenly a gray rock becomes ashen or clouded with dream. A ring round a rock is luck. To find a red rock is to discover earthblood. Blue rocks make you believe in them. Patterns and flecks on rocks are bits of different countries and terrains, speckled questions. Conglomerates are the movement of land in the freedom of water, smoothed into a small thing you can hold in your hand, rub against your face. Sandstone is soothing and lucid. Shale, of course, is rational. Find pleasure in these ordinary palm worlds. Help yourself prepare for a life. Recognize when there are no words for the pain, when there are no words for the joy, there are rocks. Fill all the clear drinking glasses in your house with rocks, no matter what your husband or lover thinks. Gather rocks in small piles on the counters, the tables, the windowsills. Divide rocks by color, texture, size, shape. Collect some larger stones, place them along the floor of your living room, never mind what the guests think, build an intricate labyrinth of inanimates. Move around your rocks like a curl of water. Begin to detect smells and sounds to different varieties of rock. Give names to some, not geological, but of your own making. Memorize their presence, know if one is missing or out of place. Bathe them in water once each week. Carry a different one in your pocket every day. Move away from normal but don’t notice it. Move towards excess but don’t care. Own more rocks than clothing, than dishes, than books. Lie down next to them on the floor, put the smaller ones in your mouth occasionally. Sometimes, feel lithic, or petrified, or rupestral instead of tired, irritable, depressed. At night, alone, naked, place one green, one red, one ashen on different parts of your body. Tell no one.

Loren held out her hand. "It's been fun listening to your stories, Mr...." The old cook smiled. "Cussler, Clive Cussler. Mighty nice to have met you, ma'am." When they were on the road again, the Pierce Arrow and its trailer smoothly rolling toward the border crossing, Pitt turned to Loren. "For a moment there, I thought the old geezer might have given me a clue to the treasure site." "You mean Yaeger's far-out translation about a river running under an island?" "It still doesn't seem geologically possible." Loren turned the rearview mirror to reapply her lipstick. "If the river flowed deep enough it might conceivably pass under the Gulf." "Maybe, but there's no way in hell to know for certain without drilling through several kilometers of hard rock." "You'll be lucky just to find your way to the treasure cavern without a major excavation." Pitt smiled as he stared at the road ahead. "He could really spin the yarns, couldn't he?" "The old cook? He certainly had an active imagination." "I'm sorry I didn't get his name." Loren settled back in the seat and gazed out her window as the dunes gave way to a tapestry of mesquite and cactus. "He told me what it was." "And?" "It was an odd name." She paused, trying to remember. Then she shrugged in defeat. "Funny thing...I've already forgotten it.

But after geological ages of rock-bound slumber, we’re now releasing—all at once—the same carbon dioxide responsible for the difference between the tropical greenhouse of the Devonian and the wintry climes of the Late Paleozoic Ice Age that followed. We do so at our peril.

Rocks are time made manifest.

Burrator Reservoir, in south-west England’s Dartmoor National Park, is a good place to start. My university department takes its new geology students to this spot every autumn to give them their first taste of intrusive volcanic rocks – rocks formed when molten magma flows through the Earth’s cool upper crust slowly enough to solidify before it breaks through to the surface. The uplands of Dartmoor exist only because the resulting granite, deposited near the beginning of the Permian Period 290 million years ago, is more resistant to erosion than the softer rocks of the surrounding, low-lying countryside. Our students first see the granite in a small abandoned quarry, just south of Burrator Reservoir, and this location illustrates nicely many crucial components of the Earth’s climate system. The geological processes operating in this area act like a thermostatically controlled air conditioning system and, together with similar processes occurring in many places across the world, help keep temperatures on our planet roughly constant and, hence, suitable for life.

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.

Oil and gas wells produce from hydrocarbon-bearing geologic reservoirs deep under the surface of the earth which are either characterized as conventional reservoirs or unconventional reservoirs. For all oil and gas reservoirs, there are three important geologic characteristics that oil and gas companies consider when exploring for oil and natural gas: porosity, hydrocarbon saturation, and permeability. In plain English, porosity describes the capacity for a rock formation to hold liquids or gases, hydrocarbon saturation describes the percentage of total pore volume occupied by hydrocarbons, and permeability describes the ability for liquids or gases to flow through the rock pore space.

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.