La tumba negra (Spanish Edition)

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It was a confidence boost, reassuring me that I am doing the right things. It was really reassuring to know I was on the right path … It pointed out how to work to your strengths and how to combat your weaknesses and turn them into strengths too.

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Flash reports represent nothing more than a quick snapshot of critical company operating and financial data, which is then used to support the ongoing operations of the business. All types of flash reports are used in business, and they range from a printed circuit board manufacturing company evaluating its book-to-bill ratio on a weekly basis to Wal-Mart reporting daily sales activity during the holiday season to an auto manufacturer evaluating weekly finished goods inventory levels. The goal with all flash reports remains the same in that critical business information is delivered to management for review much more frequently.

Granted, while a flash report that presents sales volumes for the first two weeks of February compared to the similar two-week period for the prior year is reporting new sales information, the format of the report and the presentation of the information in the report should be consistent. Thus, management should be able to quickly decipher the results and determine whether the company is performing within expectations and what to expect on the bottom-line for the entire month.

Established since , hosts more than articles still growing , and has helped millions accounting student, teacher, junior accountants and small business owners, worldwide. The purpose for writing a critique is to evaluate somebodys work a book, an essay, a movie, a painting It can be used to discuss a book, article or even a film. This is to ensure that important details are provided. All the best real money online casinos in the world are available to USA players who love to gamble.

This is an important part of the critical analysis essay because this will be your basis for evaluation. I am one of them having won a lot of cold, hard cash over the years on the same games I used play in Las Vegas. A critical essay can either be summary of the contents of the reviewed material or a personal opinion and analysis of the writer about the content The usual format of a critical essay is in the form of argumentative analysis and it is primarily targeted for academic audiences.

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These Bingo sites frequently have casino-like games and scratch cards as well. If your state is not allowed the site will prevent you from registering automatically. There are big advantages to gambling online as opposed to live games at land-based casinos. Craps, Blackjack, and Roulette can be played at a much faster pace online allowing for more bets in a shorter time.

For instance, if you are hitting consistently on red, you could take advantage of your lucky streak with extra fast bets on even numbers and on red as well. Then, just slow down your betting when your luck turns. For this reason and because they tend to have good odds, many die-hard table game players play online exclusively. Seasoned players know that video poker has very good odds, so playing several hands at once is preferable. The more hands played the more that can be won, and nothing compares to the rate one can play cards online. Some professional gamblers play multi-hand video poker as their sole source of income.

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Narrative essay - 1314 Words

Because of this the majority of American residents still play at offshore websites. This brings fear of tax evasion and the possibility of laundering money from American officials, yet not one arrest has ever been made on a state level. If regulation becomes federal law than it is very likely these large companies will step in and take over all real money casino game manufacturing.

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Most online gambling facilities are based out of state and in places such as Antigua because there are many areas in the U. The opinion or argument that you prove in a research paper is called your thesis. This thesis is usually presented at the end of your introduction. It should consist of a fairly specific and precise announcement. A statement like "In the speeches of John Winthrop and Jonathan Edwards there are many similarities but also differences" is too vague. A better thesis would be: "While John Winthrop's speeches use religious doctrines to defend a democratic social model, Jonathan Edwards employs Scripture primarily to promote a strongly religious behavior among his listeners.

Quotations should not constitute more than twenty per cent of your paper. Especially when you use longer quotations, it is not enough to just give the quotation; you also need to explain to your reader how that quotation illustrates a point you are trying to make. This is done in brackets after closing the quotation marks. When the source of your quotation is apparent from your text, only indicate the page number; otherwise indicate both the source and the page number.

If your quotation is longer than three lines, set it off from the rest of the text by indenting it five spaces and omit the quotations marks. The character inherent in the American people has done all that has been accomplished" If you leave one or more words out from your quotation, indicate this through three periods with one space in between each period. If you add anything to your quotation, indicate this by putting the words which you are adding and which are not in the original text inside square brackets. If you quote from a poem, indicate the end of a line in the original through a slash i.

Further information: If you have any questions about formal aspects of research papers, consult Gibaldi, Joseph. Assume that your reader has read the primary text s about which you are writing. Some students of literary studies tend to give biographical introductions to the primary authors about whom they are writing. Thoreau complains that "this government never of itself furthered any enterprise, but by the alacrity with which it got out of its way. This should only be done if that biographical information is directly relevant for your thesis.

The following paper topics are designed to test your understanding of the novel as a whole and to analyze important themes and literary devices. Gravity and angles make house seem warped or mysterious C. Makes travel from or to the Bundren house difficult C. Following each question is a sample outline to get you started. Topic 1 Nature plays as vital a part in many stories and poems as the characters do. As I Lay Dying relies a great deal on Nature and her forces to move the story line along.

What universal natural symbols does Faulkner rely on and how does he incorporate them into the action of the novel? Causes Cash to break his leg and get kicked by the horse. Causes decomposing body to decay and smell sooner C. Paying careful attention to descriptive phrases, imagery, and adjectives, discuss whether or not Faulkner is successful in drawing his characters. Topic 2 Addie Bundren maintains that words are not important; they go straight up and bear no relation to things that happen. Examine the names and the descriptions of the characters.

The stream gradient becomes nearly flat, and lateral deposition of sediments becomes important as the stream meanders across the valley floor. In all stages of stream erosion, by far the most erosion occurs during times of flood, when more and faster-moving water is available to carry a larger sediment load. In such processes, it is not the water alone that erodes: suspended abrasive particles, pebbles and boulders can also act erosively as they traverse a surface, in a process known as traction.

Bank erosion is the wearing away of the banks of a stream or river. This is distinguished from changes on the bed of the watercourse, which is referred to as scour. Erosion and changes in the form of river banks may be measured by inserting metal rods into the bank and marking the position of the bank surface along the rods at different times. Rapid river channel migration observed in the Lena River of Siberia is due to thermal erosion, as these portions of the banks are composed of permafrost-cemented non-cohesive materials.

Much of this erosion occurs as the weakened banks fail in large slumps. Thermal erosion also affects the Arctic coast, where wave action and near-shore temperatures combine to undercut permafrost bluffs along the shoreline and cause them to fail. Annual erosion rates along a kilometre mile segment of the Beaufort Sea shoreline averaged 5. At extremely high flows, kolks, or vortices are formed by large volumes of rapidly rushing water. Kolks cause extreme local erosion, plucking bedrock and creating pothole-type geographical features called Rock-cut basins.

Examples can be seen in the flood regions result from glacial Lake Missoula, which created the channeled scablands in the Columbia Basin region of eastern Washington. Wind erosion is a major geomorphological force, especially in arid and semi-arid regions. It is also a major source of land degradation, evaporation, desertification, harmful airborne dust, and crop damage—especially after being increased far above natural rates by human activities such as deforestation, urbanization, and agriculture.

Wind erosion is of two primary varieties: deflation, where the wind picks up and carries away loose particles; and abrasion, where surfaces are worn down as they are struck by airborne particles carried by wind. Deflation is divided into three categories: 1 surface creep, where larger, heavier particles slide or roll along the ground; 2 saltation, where particles are lifted a short height into the air, and bounce and saltate across the surface of the soil; and 3 suspension, where very small and light particles are lifted into the air by the wind, and are often carried for long distances.

Wind erosion is much more severe in arid areas and during times of drought. For example, in the Great Plains, it is estimated that soil loss due to wind erosion can be as much as times greater in drought years than in wet years. It moves material from higher elevations to lower elevations where other eroding agents such as streams and glaciers can then pick up the material and move it to even lower elevations. Mass-movement processes are always occurring continuously on all slopes; some mass-movement processes act very slowly; others occur very suddenly, often with disastrous results. Any perceptible down-slope movement of rock or sediment is often referred to in general terms as a landslide.

However, landslides can be classijello much more detailed way that reflects the mechanisms responsible for the movement and the velocity at which the movement occurs. One of the visible topographical manifestations of a very slow form of such activity is a scree slope. Slumping happens on steep hillsides, occurring along distinct fracture zones, often within materials like clay that, once released, may move quite rapidly downhill. They will often show a spoon-shaped isostatic depression, in which the material has begun to slide downhill.

In some cases, the slump is caused by water beneath the slope weakening it. In many cases it is simply the result of poor engineering along highways where it is a regular occurrence. Surface creep is the slow movement of soil and rock debris by gravity which is usually not perceptible except through extended observation. However, the term can also describe the rolling of dislodged soil particles 0. The amount and intensity of precipitation is the main climatic factor governing soil erosion by water. The relationship is particularly strong if heavy rainfall occurs at times when, or in locations where, the soil's surface is not well protected by vegetation.

This might be during periods when agricultural activities leave the soil bare, or in semi-arid regions where vegetation is naturally sparse. Wind erosion requires strong winds, particularly during times of drought when vegetation is sparse and soil is dry and so is more erodible. Other climatic factors such as average temperature and temperature range may also affect erosion, via their effects on vegetation and soil properties. In general, given similar vegetation and ecosystems, areas with more precipitation especially high-intensity rainfall , more wind, or more storms are expected to have more erosion.

The size and velocity of rain drops is also an important factor. Larger and higher-velocity rain drops have greater kinetic energy, and thus their impact will displace soil particles by larger distances than smaller, slower-moving rain drops. In such situations, rainfall amount rather than intensity is the main factor determining the severity of soil erosion by water. The composition, moisture, and compaction of soil are all major factors in determining the erosivity of rainfall. Sediments containing more clay tend to be more resistant to erosion than those with sand or silt, because the clay helps bind soil particles together.

The amount of water present in the soil before the precipitation also plays an important role, because it sets limits on the amount of water that can be absorbed by the soil and hence prevented from flowing on the surface as erosive runoff. Wet, saturated soils will not be able to absorb as much rain water, leading to higher levels of surface runoff and thus higher erosivity for a given volume of rainfall.

Soil compaction also affects the permeability of the soil to water, and hence the amount of water that flows away as runoff. More compacted soils will have a larger amount of surface runoff than less compacted soils. Vegetation acts as an interface between the atmosphere and the soil. It increases the permeability of the soil to rainwater, thus decreasing runoff. It shelters the soil from winds, which results in decreased wind erosion, as well as advantageous changes in microclimate. The roots of the plants bind the soil together, and interweave with other roots, forming a more solid mass that is less susceptible to both water and wind erosion.

The removal of vegetation increases the rate of surface erosion. The topography of the land determines the velocity at which surface runoff will flow, which in turn determines the erosivity of the runoff. Longer, steeper slopes especially those without adequate vegetative cover are more susceptible to very high rates of erosion during heavy rains than shorter, less steep slopes. Steeper terrain is also more prone to mudslides, landslides, and other forms of gravitational erosion processes.

The tillage of agricultural lands, which breaks up soil into finer particles, is one of the primary factors. The problem has been exacerbated in modern times, due to mechanized agricultural equipment that allows for deep plowing, which severely increases the amount of soil that is available for transport by water erosion. Others include mono-cropping, farming on steep slopes, pesticide and chemical fertilizer usage which kill organisms that bind soil together , row-cropping, and the use of surface irrigation.

A complex overall situation with respect to defining nutrient losses from soils, could arise as a result of the size selective nature of soil erosion events. Loss of total phosphorus, for instance, in the finer eroded fraction is greater relative to the whole soil. Extrapolating this evidence to predict subsequent behaviour within receiving aquatic systems, the reason is that this more easily transported material may support a lower solution P concentration compared to coarser sized fractions.

Tillage also increases wind erosion rates, by dehydrating the soil and breaking it up into smaller particles that can be picked up by the wind. Exacerbating this is the fact that most of the trees are generally removed from agricultural fields, allowing winds to have long, open runs to travel over at higher speeds. In this clearcut, almost all of the vegetation has been stripped from surface of steep slopes, in an area with very heavy rains. Severe erosion occurs in cases such as this, causing stream sedimentation and the loss of nutrient rich topsoil.

In an undisturbed forest, the mineral soil is protected by a layer of leaf litter and an humus that cover the forest floor. These two layers form a protective mat over the soil that absorbs the impact of rain drops. They are porous and highly permeable to rainfall, and allow rainwater to slow percolate into the soil below, instead of flowing over the surface as runoff.

However it is the forest floor, more than the canopy, that prevents surface erosion. The terminal velocity of rain drops is reached in about 8 metres 26 feet. Because forest canopies are usually higher than this, rain drops can often regain terminal velocity even after striking the canopy.

However, the intact forest floor, with its layers of leaf litter and organic matter, is still able to absorb the impact of the rainfall. Deforestation causes increased erosion rates due to exposure of mineral soil by removing the humus and litter layers from the soil surface, removing the vegetative cover that binds soil together, and causing heavy soil compaction from logging equipment. Once trees have been removed by fire or logging, infiltration rates become high and erosion low to the degree the forest floor remains intact.

Severe fires can lead to significant further erosion if followed by heavy rainfall. Globally one of the largest contributors to erosive soil loss in the year is the slash and burn treatment of tropical forests. In a number of regions of the earth, entire sectors of a country have been rendered unproductive. For example, on the Madagascar high central plateau, comprising approximately ten percent of that country's land area, virtually the entire landscape is sterile of vegetation, with gully erosive furrows typically in excess of 50 metres ft deep and 1 kilometre 0.

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  • Shifting cultivation is a farming system which sometimes incorporates the slash and burn method in some regions of the world. This degrades the soil and causes the soil to become less and less fertile. Urbanization has major effects on erosion processes—first by denuding the land of vegetative cover, altering drainage patterns, and compacting the soil during construction; and next by covering the land in an impermeable layer of asphalt or concrete that increases the amount of surface runoff and increases surface wind speeds.

    This increased runoff, in addition to eroding and degrading the land that it flows over, also causes major disruption to surrounding watersheds by altering the volume and rate of water that flows through them, and filling them with chemically polluted sedimentation. The increased flow of water through local waterways also causes a large increase in the rate of bank erosion.

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    Studies on soil erosion suggest that increased rainfall amounts and intensities will lead to greater rates of soil erosion. Thus, if rainfall amounts and intensities increase in many parts of the world as expected, erosion will also increase, unless amelioration measures are taken. Soil erosion rates are expected to change in response to changes in climate for a variety of reasons. The most direct is the change in the erosive power of rainfall.

    Other reasons include: a changes in plant canopy caused by shifts in plant biomass production associated with moisture regime; b changes in litter cover on the ground caused by changes in both plant residue decomposition rates driven by temperature and moisture dependent soil microbial activity as well as plant biomass production rates; c changes in soil moisture due to shifting precipitation regimes and evapo-transpiration rates, which changes infiltration and runoff ratios; d soil erodibility changes due to decrease in soil organic matter concentrations in soils that lead to a soil structure that is more susceptible to erosion and increased runoff due to increased soil surface sealing and crusting; e a shift of winter precipitation from non-erosive snow to erosive rainfall due to increasing winter temperatures; f melting of permafrost, which induces an erodible soil state from a previously non-erodible one; and g shifts in land use made necessary to accommodate new climatic regimes.

    Studies by Pruski and Nearing indicated that, other factors such as land use unconsidered, it is reasonable to expect approximately a 1. During the 17th and 18th centuries, Easter Island experienced severe erosion due to deforestation and unsustainable agricultural practices. The resulting loss of topsoil ultimately led to ecological collapse, causing mass starvation and the complete disintegration of the Easter Island civilization. The study investigates global soil erosion dynamics by means of high-resolution spatially distributed modelling ca.

    The geo-statistical approach allows, for the first time, the thorough incorporation into a global soil erosion model of land use and changes in land use, the extent, types, spatial distribution of global croplands and the effects of different regional cropping systems. The loss of soil fertility due to erosion is further problematic because the response is often to apply chemical fertilizers, which leads to further water and soil pollution, rather than to allow the land to regenerate.

    Soil erosion especially from agricultural activity is considered to be the leading global cause of diffuse water pollution, due to the effects of the excess sediments flowing into the world's waterways. The sediments themselves act as pollutants, as well as being carriers for other pollutants, such as attached pesticide molecules or heavy metals.

    The effect of increased sediments loads on aquatic ecosystems can be catastrophic. Silt can smother the spawning beds of fish, by filling in the space between gravel on the stream bed. It also reduces their food supply, and causes major respiratory issues for them as sediment enters their gills. The biodiversity of aquatic plant and algal life is reduced, and invertebrates are also unable to survive and reproduce. While the sedimentation event itself might be relatively short-lived, the ecological disruption caused by the mass die off often persists long into the future.

    One of the most serious and long-running water erosion problems worldwide is in the People's Republic of China, on the middle reaches of the Yellow River and the upper reaches of the Yangtze River. From the Yellow River, over 1. The sediment originates primarily from water erosion in the Loess Plateau region of the northwest. Soil particles picked up during wind erosion of soil are a major source of air pollution, in the form of airborne particulates—"dust". Monitoring and modeling of erosion processes can help people better understand the causes of soil erosion, make predictions of erosion under a range of possible conditions, and plan the implementation of preventative and restorative strategies for erosion.

    However, the complexity of erosion processes and the number of scientific disciplines that must be considered to understand and model them e. Erosion models are also non-linear, which makes them difficult to work with numerically, and makes it difficult or impossible to scale up to making predictions about large areas from data collected by sampling smaller plots.

    It estimates the average annual soil loss A on a plot-sized area as: Despite the USLE's plot-scale spatial focus, the model has often been used to estimate soil erosion on much larger areas, such as watersheds or even whole continents. But because of the complexity of soil erosion and its constituent processes, all erosion models can give unsatisfactory results when validated i. In addition to significantly reducing wind erosion, windbreaks provide many other benefits such as improved microclimates for crops which are sheltered from the dehydrating and otherwise damaging effects of wind , habitat for beneficial bird species, In tropical coastal systems, properties of mangroves have been examined as a potential means to reduce soil erosion.

    Their complex root structures are known to help reduce wave damage from storms and flood impacts while binding and building soils. These roots can slow down water flow, leading to the deposition of sediments and reduced erosion rates. However, in order to maintain sediment balance, adequate mangrove forest width needs to be present. Amazing college essay examples from my own students. Let us know over at collegeessayguy. The problem is that sometimes students have good stories… They have the seed of an idea and the makings of a great story, but the college essay format or structure is all over the place.

    Before we even get to college admission essay format we HAVE to talk about topic. At College Essay Guy, we believe a good college essay should either go deep, discussing one moment that fundamentally changed your life, or go wide, discussing many different elements of your life. The Narrative Structure, will help you go deep, while the Montage Structure will help you go wide. The narrative structure is the basis for the majority of American films today.

    This structure is time-tested and, therefore, pretty reliable. Raise the stakes: Then, the changes get even bigger! This step is important because it raises the dramatic tension. Will you discover a passion that will pull you out of your grief? The moment that will decide whether or not you will make it out of the problem. The juxtaposition of vignettes, anecdotes, or fragments of your life come together to create the overall message you want your reader to walk away with.

    To help you decide, consider beginning by searching for a focusing lens for your college essay format. Ebooks and Manuals

    For one student, it was scrapbooking click here to read that essay. They pass an engagement ring store and she eyes a particular ring. Remember: There is no surefire approach for essay writing. No essay or college essay format will, on its own, get a student into a college. Many different students are accepted to colleges each year with many different types of essays. To see how the Narrative Essay structure works, check out the essay below, which was written for the Common App "Topic of your choice" prompt.

    The job of the essay, simply put, is demonstrate to a college that you will make valuable contributions in college and beyond. We believe these four qualities are essential to a great essay: Core values are the things that are so important to you that you would fight for them. The uncommon connections are often made up of insights that are unusual or unexpected. You might try reading it here first before reading the paragraph-by-paragraph breakdown below. Craft is the sense that you know the purpose of each paragraph, each sentence, each word.

    For each paragraph, each sentence, each word, ask: Do I need this? They covered the precious mahogany coffin with a brown amalgam of rocks, decomposed organisms, and weeds. It was my turn to take the shovel, but I felt too ashamed to dutifully send her off when I had not properly said goodbye. I refused to let go of my grandmother, to accept a death I had not seen coming, to believe that an illness could not only interrupt, but steal a beloved life.

    She also sets up an objective correlative the shovel that will come back later. When my parents finally revealed to me that my grandmother had been battling liver cancer, I was twelve and I was angry--mostly with myself. They had wanted to protect me--only six years old at the time--from the complex and morose concept of death. Hurt that my parents had deceived me and resentful of my own oblivion, I committed myself to preventing such blindness from resurfacing.

    In the second paragraph she flashes back to give us some context i. I became desperately devoted to my education because I saw knowledge as the key to freeing myself from the chains of ignorance. While learning about cancer in school I promised myself that I would memorize every fact and absorb every detail in textbooks and online medical journals.

    And as I began to consider my future, I realized that what I learned in school would allow me to silence that which had silenced my grandmother. However, I was focused not with learning itself, but with good grades and high test scores. I started to believe that academic perfection would be the only way to redeem myself in her eyes--to make up for what I had not done as a granddaughter.

    However, a simple walk on a hiking trail behind my house made me open my own eyes to the truth. In the third paragraph she takes off a hundred miles an hour… Over the years, everything--even honoring my grandmother--had become second to school and grades. As my shoes humbly tapped against the Earth, the towering trees blackened by the forest fire a few years ago, the faintly colorful pebbles embedded in the sidewalk, and the wispy white clouds hanging in the sky reminded me of my small though nonetheless significant part in a larger whole that is humankind and this Earth.

    Before I could resolve my guilt, I had to broaden my perspective of the world as well as my responsibilities to my fellow humans. Ebooks and Manuals

    Volunteering at a cancer treatment center has helped me discover my path. When I see patients trapped in not only the hospital but also a moment in time by their diseases, I talk to them. For six hours a day, three times a week, Ivana is surrounded by IV stands, empty walls, and busy nurses that quietly yet constantly remind her of her breast cancer. I need only to smile and say hello to see her brighten up as life returns to her face. Upon our first meeting, she opened up about her two sons, her hometown, and her knitting group--no mention of her disease.

    Without even standing up, the three of us—Ivana, me, and my grandmother--had taken a walk together. In the second to last paragraph we see how the results of her moment of truth which, admittedly, is somewhat ambiguous led her to take action: volunteering at the local hospital helps her see her larger place in the world. While I physically treat their cancer, I want to lend patients emotional support and mental strength to escape the interruption and continue living. But at the end of the journey, after reaching the summit of Ktaadn, something changes in Thoreau. For the first 32 years of my life, I spent much time hiking, camping, and fishing in the woods and foothills of southern Illinois.

    That he had gone to the woods before and had climbed highpoints to take in the view of the surrounding countryside before, that he had experienced … while coming down this part of the mountain. It was not lawn, nor pasture, nor mead, nor woodland, nor lea, nor arable, nor waste-land. It was the fresh and natural surface of the planet Earth, as it was made forever and ever…. It was Matter, vast, terrific—not his Mother Earth that we have heard of, not for him to tread on, or be buried in—no, it were being too familiar even to let his bones lie there—the home this of Necessity and Fate.

    These are the words of a man whose faith has been shaken. After he returned to Walden, he began to write the narrative of his Ktaadn adventure, understandably, using first person, past tense—the voice of a traveller returned. An important thing to remember when encountering prose set in this point of view, is that the narrator already knows the outcome of everything; he is omnipotent in the universe created by the opening sentence and ending with the last. And while Thoreau relates this information in relatively chronological order, as if the reader were following the same path as the author, the author is in full control of which information the reader sees and when the reader sees it.

    I remember that I was strangely affected when we were returning, by the sight of a ring-bolt well drilled into a rock, and fastened with lead, at the head of this solitary Ambejijis Lake. Up to this point in the narrative, Thoreau had discussed nature always in relationship to the humans who lived in it. Described their attempts to tame it, to utilize its resources, to capitalize on it, and he described those who lived and worked in nature as being superior to those who lived in urban settings.

    But now, here in the Maine backwoods, he finds it startling that humanity can leave such a mark on this place. Ktaadn and true wilderness, we see him carefully point out the mark of humankind on the woods: among other things, a handbill for the Oak Hall wrapped around a pine whose bark has been stripped. Imagine it, miles and miles into this roadless wilderness, Thoreau shows the reader a harbinger of modernity—an advertisement stuck to a barkless trunk, smooth as a telephone pole. On page 64, Nature speaks to the reader, to Thoreau himself, in biblical prose: Some part of the beholder, even some vital part, seems to escape through the loose grating of his ribs as he ascends.

    There is less of substantial thought and fair understanding in him, than in the plains where men inhabit. His reason is dispersed and shadowy, more thin and subtle like the air. Vast, Titanic, in-human Nature has got him at a disadvantage, caught him alone, and pilfers him of some of his divine faculty. She seems to say sternly, why came ye here before your time? Is it not enough that I smile on you in the valleys? I have never made this soil for thy feet, this air for thy breathing, these rocks for thy neighbors. I cannot pity nor fondle thee here, but forever relentlessly drive thee hence to where I kind.

    Why seek me where I have not called thee, and then complain because you find me but a stepmother? Shouldst thou freeze or starve, or shudder thy life away, here is no shrine, nor altar, nor any access to my ear. How does one return from this kind of crisis of faith?

    Here we see that people may live within nature, use it to their benefit, and even for a brief time seem to control it, but at any moment, Nature can send humankind spinning back into the void. As Thoreau walks the thin strip of land that is Cape Cod, it becomes a borderland between the wild, ever-changing sea, and the westward expanding civilization of the United States, a place where he can bring together the extremes of ideology and reality. Some of these timbers, however, were so rotten that I could almost thrust my umbrella through them.

    That like the ship, we are easily transformed back into the elements from which we came. But with this scene, we see a different reaction from Thoreau than we did on the summit of Ktaadn. If this was the law of Nature, why waste any time in awe or pity? Has he lost any sense of compassion for his fellow man? Or has he simply come to view all as a part of Nature?

    We concluded that it was not a house at all, but a sea-side box, now shut up, belonging to some family of Night or Chaos, where they spent their summers by the sea. However, we were glad to sit outside, under the lee of the Humane house, to escape the piercing wind; and there we thought how cold is charity!

    We might consider then, how the landscapes themselves allow for a different perspective. At Walden pond Thoreau finds refuge in the pastoral that lies wild but safe in known world; on Ktaadn, Thoreau experiences a landscape that appears to stand untouched from the beginning of time, for geological time to human eyes appears unmoving, and to enter that landscape one enters eternity.

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