Alfred, Lord Tennyson Poems

The poet laureate of Great Britain and Ireland, Tennyson developed his talent as a poet at Trinity College, when he was befriended by Arthur Hallam and members of the Apostles literary club. When his friend Hallam died suddenly at the age of 24, Tennyson wrote one of his longest and most moving poems In Memoriam. That poem became a favorite of Queen Victorias.   Here are some of Tennysons best-known poems, with an excerpt from each one.   The Charge of the Light Brigade Perhaps Tennysons most famous poem, The Charge of the Light Brigade contains the quotable line Rage, rage against the dying of the light. It tells the historical story of the Battle of Balaclava during the Crimean War, where the British Light Brigade suffered heavy casualties.The poem begins: Half a league, half a league,Half a league onward,All in the valley of DeathRode the six hundred. In Memoriam Written as a eulogy of sorts for his great friend Arthur Hallam, this moving poem has become a staple of memorial services. The famous line Nature, red in tooth and claw, makes its first appearance in this poem, which begins: Strong Son of God, immortal Love,Whom we, that have not seen thy face,By faith, and faith alone, embrace,Believing where we cannot prove A Farewell Many of Tennysons works are focused on death; in this poem, he ponders how everyone dies, but nature will continue after were gone. Flow down, cold rivulet, to the seaThy tribute wave deliver:No more by thee my steps shall beFor ever and for ever Break, Break, Break This is another Tennyson poem where the narrator is struggling to express his grief about a lost friend. The waves break relentlessly on the beach, reminding the narrator that time moves on. Break, break, break,On thy cold gray stones, O Sea!And I would that my tongue could utterThe thoughts that arise in me. Crossing the Bar This 1889 poem uses the analogy of the sea and the sand to represent death. Its said that Tennyson requested this poem be included as the final entry in any collections of his work after his death.   Sunset and evening star,And one clear call for me!And may there be no moaning of the bar,When I put out to sea, Now Sleeps the Crimson Petal This Tennyson sonnet is so lyrical that many songwriters have tried to put it to music. It ponders, through the use of natural metaphors (flowers, stars, fireflies) what it means to remember someone.   Now sleeps the crimson petal, now the white;Nor waves the cypress in the palace walk;Nor winks the gold fin in the porphyry font:The fire-fly wakens: waken thou with me. The Lady of Shalott Based on an Arthurian legend, this poem tells the story of a lady who is under a mysterious curse. Heres an excerpt: On either side the river lieLong fields of barley and of rye,That clothe the wold and meet the sky;And thro’ the field the road runs by The Splendour Falls on Castle Walls This rhyming, lyrical poem is a somber reflection on how one is remembered. After hearing a bugle call echo around a valley, the narrator considers the echoes that people leave behind.    The splendor falls on castle wallsAnd snowy summits old in story;The long light shakes across the lakes,And the wild cataract leaps in glory. Ulysses Tennysons interpretation of the mythological Greek king finds him wanting to return to traveling, even after many years away from home. This poem contains the famous and oft-quoted line   To strive, to seek, to find, and not to yield. Here is the opening to Tennysons Ulysses. It little profits that an idle king,By this still hearth, among these barren crags,Match’d with an aged wife, I mete and doleUnequal laws unto a savage race

Fact Pattern # 1 Tom Rogers - 923 Words

Fact Pattern #1 Tom Rogers is a career criminal, who got his second offense for armed robbery. He robbed an 80 year old widow in the Kroger parking lot. The Fayette County District Attorney wants the maximum sentence, but the public defender is asking for mercy since Tom’s elderly mother is sick and needs him to care for her at home. Being that I am the Judge, I will give Mr. Rogers the maximum sentence for his second offense for armed robbery. The maximum sentence will be twenty years of imprisonment3, without parole or probation. I chose the maximum because this is not the defendant first offense of armed robbery. Also because he robbed an eighty year old widow. Yes, I understand that is his mother is sick and needs him to take care of her, but he is unstable to take care of his mother. The defendant mother can be taken to a nursing home, where she can get a trained licensed nurse to give her quality care. The nurses at the nursing home is more stable and equipped to take ca re of the defendant mother, then he is capable of doing himself. I chose this punishment for the defendant, because he is a known robber, who will more than likely continue to rob if he is not stopped. Fact Pattern #2 John Smith fell at work and hurt his back. He was prescribed OxyContin for the pain. John got hooked on the pills, so he started buying extra off the streets. He eventually got caught and is charged with possession. Being that I am the District Attorney, I will first see if the fallShow MoreRelatedUse of Language in a Clockwork Orange2093 Words   |  9 Pagessome editions include a glossary to explain the various words, this was an unnecessary concession to lazy readers; the sense is apparent, and the ease with which the reader adjusts to the new speech patterns is a testimony to the authors skill. 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Natural Science Volcanoes Free Essays

The relentless motions of tectonic plates, the uplift and the erosion of mountain ranges, and the evolution of living organisms are processes which can only be fully appreciated across the deep time of geology. But some of the processes at work in our planet can manifest all too suddenly, changing the landscape and destroying lives on a very human timescale: volcanoes. Superimpose a map of active volcanoes on a world map showing the boundaries of the tectonic plates and their association is obvious. We will write a custom essay sample on Natural Science: Volcanoes or any similar topic only for you Order Now The ring of fire around the Pacific, for example, is clearly associated with the plate boundaries. But where is the molten rock that feeds them coming from? Why are volcanoes different from each other, with some producing gentle eruptions and regular trickles of molten lava, whilst others erupt in devastating explosions? And why are some volcanoes, such as those of Hawaii, in the middle of the Pacific, far from any obvious plate boundary? The molten rock The key to understanding volcanoes comes from understanding how rocks melt. For a start, they do not have to melt completely, so the bulk of the mantle remains solid even though it gives rise to a fluid, molten magma. That means that the melt does not have the same composition as the bulk of the mantle. As long as the so-called dihedral angles, the angles at which the mineral grains in mantle rock meet, are large enough, the rock behaves like a porous sponge and the melt can be squeezed out. Calculations show how it will tend to flow together and rise quite rapidly in a sort of wave, producing lava at the surface in the sort of quantities seen in typical eruptions (The University of Sydney, 2006). Melting does not necessarily involve increasing the temperature. It can result from decreasing the pressure. So a plume of hot, solid mantle material will begin to melt as it rises and the pressure upon it reduces. In the case of a mantle plume, that can happen at considerable depths (McKenzie, 1984, p. 717). Beneath the mid-ocean ridge system, the melting takes place at much shallower depths. Here there is little or no mantle lithosphere and the hot asthenosphere comes close to the surface. The lower pressures here can result in a larger proportion of the rock melting, perhaps 20 or 25%, supplying magma at about the right rate to sustain sea floor spreading and produce an ocean crust 7 kilometres thick. Most of the ocean ridge eruptions pass unnoticed as they take place more than 2,000 metres underwater as rapidly quenched pillow lavas (Basin Topography, 2006). But seismic studies have revealed magma chambers a few kilometres beneath the sea floor in parts of the ridges, particularly in the Pacific and Indian oceans, though there is also some evidence of magma chambers beneath the mid-Atlantic ridge. Where a mantle plume coincides with an ocean ridge system, as in the case of Iceland, more magma is generated and the ocean crust is thicker, in this case rising above the sea to form Iceland (Scarth, 1994, p.14-17). Hawaii The Big Island of Hawaii has welcoming people and friendly volcanoes. The town of Hilo is probably more at risk from tsunamis triggered by distant earthquakes than from the great 4,000-metre volcano of Mauna Loa that looms behind it. To the north and west lie the other Hawaiian islands and the Emperor seamount chain, tracing the long journey of the Pacific plate across the hot spot of an underlying mantle plume (Scarth, 1994, p.42). To the south of the Big Island of Hawaii is Loihi, the newest of the Hawaiian volcanoes. As yet it has not broken the surface of the Pacific, but it has already built a high mountain of basalt on the ocean floor and will almost certainly become an island above water before long (14). Because Hawaiian lava is very fluid, it can spread over a wide area and does not tend to form very steep slopes. Such volcanoes are sometimes known as shield volcanoes, and they can flood basalt over a wide area. Often, a particular flow will develop a tunnel around it as the outer crust solidifies but the lava continues to flow inside. When the supply of lava ceases, the tunnel can drain and be left hollow (41-42). How to cite Natural Science: Volcanoes, Papers