How to Conjugate the Verb Stare in Italian

â€Å"Stare† is used to talk about all things, from how you’re doing to where you’re at in Italy, so it’s best if you feel comfortable using this word in all its forms. What’s more, it’s an irregular verb, so it doesn’t follow the typical -are verb ending pattern. Below, you’ll find all of its conjugation tables as well as examples, so you can become more familiar with using stare. Definitions of Stare To beTo stayTo remainTo standTo be situatedTo liveTo be about to Stare in Italian It’s an intransitive verb, so it does not take a direct object.The infinito is â€Å"stare.†The participio passato is â€Å"stato.†The gerund form is â€Å"stando.†The past gerund form is â€Å"essendo stato.† Indicativo/Indicative​ Il presente io sto noi stiamo tu stai voi state lui, lei, Lei sta loro, Loro stanno Esempi: Sto bene, e tu? I’m good, and you? Maria sta buttando la pasta, ti fermi a pranzo con noi? Maria is about to cook pasta, are you going to have lunch with us? Il passato prossimo io sono stato/a noi siamo stati/e tu sei stato/a voi siete stati/e lui, lei, Lei à ¨ stato/a loro, Loro sono stati/e Esempi: Sono stata a Bologna ieri sera. I was in Bologna last night. Marco e Giulio sono stati davvero carini! Marco and Giulio were extremely nice! L’imperfetto io stavo noi stavamo tu stavi voi stavate lui, lei, Lei stava loro, Loro stavano Esempi: Che stavi facendo? What were you doing? Stavamo per partire quando ci ha chiamato Giulia. We were about to leave when Giulia called us. Il trapassato prossimo io ero stato/a noi eravamo stati/e tu eri stato/a voi eravate stati/e lui, lei, Lei era stato/a loro, Loro erano stati/e Esempi: Ho vissuto in Italia per 12 anni e non ero mai stato a Roma. I lived in Italy for 12 years and I had never been to Rome. Ero stato anche all’aeroporto, ma era già   partita. I also was at the airport, but she had already left. Il passato remoto io stetti noi stemmo tu stesti voi steste lui, lei, Lei stette loro, Loro stettero Esempi: Nel 1996, stetti a Londra per due settimane. In 1996, I stayed in London for two weeks. Stettrero ospiti a casa di Sandra durante il loro soggiorno a Milano. They stayed at Sandra’s during their stay in Milan. Il trapassato remoto io fui stato/a noi fummo stati/e tu fosti stato/a voi foste stati/e lui, lei, Lei fu stato/a loro, Loro furono stati/e This tense is rarely used, so don’t worry too much about mastering it. You’ll find it only in very sophisticated writing. Il futuro semplice io starà ² noi staremo tu starai voi starete lui, lei, Lei starà   loro, Loro staranno Esempi: Sà ¬, infatti, lui à ¨ malato, perà ² starà   bene fra un paio di giorni. Yes, in fact, he is sick, but he will be better in a couple of days. Starà ² pià ¹ attento, te lo prometto. I will pay more attention, I promise. Il futuro anteriore Io sarà ² stato/a noi saremo stati/e tu sarai stato/a voi sarete stati/e lui, lei, Lei sarà   stato/a loro, Loro saranno stati/e Esempi: Ho dimenticato di prenotare i biglietti? Sarà ² stato davvero stanco ieri sera. I forgot to book the tickets? I must have been really tired last night. Dov’era Giulia a sabato? Sarà   stata con suoi amici. Where was Giula on Saturday? She must have been with her friends. Congiuntivo/Subjunctive​ ï » ¿Il presente che io stia che noi stiamo che tu stia che voi stiate che lui, lei, Lei stia che loro, Loro stiano Esempi: Non so perchà © lui stia qua. I don’t know why he is here. Non penso che tu stia preparando abbastanza piatti. I don’t think you’re preparing enough dishes. Il passato io sia stato/a noi siamo stati/e tu sia stato/a voi siate stati/e lui, lei, Lei sia stato/a loro, Loro siano stati/e Esempi: Penso sia stato meglio cosà ¬. I think it was for the best. Credo proprio che siano stati accompagnati in taxi all’aereoporto. I really think they had been taken by taxi to the airport. L’imperfetto io stessi noi stessimo tu stessi voi steste lui, lei, Lei stesse loro, Loro stessero Esempi: Non pensavo che lui stesse alla festa. I didn’t know that he was at the party. Pensavo che stesse a dormire a casa tua. Sarei stato molto pià ¹ tranquillo! I thought she was sleeping at your place. I would have been a lot more relaxed! Il trapassato prossimo Io fossi stato/a noi fossimo stati/e tu fossi stato/a voi foste stati/e lui, lei, Lei fosse stato/a loro, Loro fossero stati/e Esempi: Se quel giorno fossi stato con lui, non sarebbe stato cosà ¬ triste. If I had been with him that day, he wouldn’t have been so sad. Se fossimo stati amici in quel periodo, ci saremmo divertiti un sacco! If we had been friends during that time, we would have had so much fun! Condizionale/Conditional​​ Il presente io starei noi staremmo tu staresti voi stareste lui, lei, Lei starebbe loro, Loro starebbero Esempi: Se io abitassi in Italia, starei meglio. If I were to live in Italy, I would be better. Se aveste finito i vostri compiti a quest’ora stareste al mare! If you had finished your homework, by this time you would be at the seaside! Il passato io sarei stato/a noi saremmo stati/e tu saresti stato/a voi sareste stati/e lui, lei, Lei sarebbe stato/a loro, Loro sarebbero stati/e Esempi: Sarei stata contenta se lui mi avesse regalato dei fiori. I would have been happy if he had given me some flowers. Non sarebbe stato possibile senza l’aiuto di Giulia. It wouldn’t have been possible without Giulia’s help. Imperativo/Imperative​​ Presente -- stiamo sta/stai/sa’ state stia stiano Stai zitto! Be quiet (informal)! Stia attenta! Pay attention (formal)!

Kill The Indian Save The Man Essay - 1089 Words

After reading Kill the Indian, Save the Man: The Genocidal Impact of American Indian Residential Schools by Ward Churchill, I have come to realization of some matters. First of all, while your goal might had been to civilize the Indians by teaching them English, manners, and change their whole appearance, the outcome was totally different. Your goal might have been successful to you, in the end you got what you wanted: to kill the Indian and Save the Man. But also, you stole those kid’s identities by taking them away from their families. You traumatized them, and making them go through so many forms of abuse. â€Å"Kill the Indian, save the men† or like U.S. Indian Commissioner William A. Jones said in 1903, the goal was to â€Å"exterminate the†¦show more content†¦How do you deal with a trauma that’s not really yours? It’s heartbreaking to see how these communities get up on the aftermath. How some people that went to these boarding schools st ill tear up every time they talk about it. Most communities, or families are broken. Many people turned to substances to drown the bad memories. How many people today still carry depression, anxiety, substance addiction, suicide thoughts, and mental instability. How many Natives did you turned against their own culture? It is sad to see how the language and the culture is declining. For example, let’s take the Navajo’s, not many people speak it anymore. Why? Because of the people that underwent through these boarding schools, they were forbidden to speak in their dialect and forced to learn how to speak English. Causing younger generations to not speak it since parent generations lost the language, and therefore can’t really teach it to their kids. Culture loss, how many people aren’t as traditional as before. All because they had to change their appearance, weren’t allowed to perform any type of prayers or any traditions they had. The population decreased, traditions weren’t practiced by youngsters, and the adults grew old. 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The Formation of Rocks in Ireland free essay sample

It is the most widespread type of intrusive igneous rock at the earth’s surface. Igneous rocks form when molten rock is erupted at a volcano and then cools and hardens to form solid rock (Holden, 2012). Granite rock is created when magma is forced between other rocks deep within the earths crust. The magma then cools due to the drop in temperature and crystallizes in caverns deep within the earth. The molten rock cools quite slowly over time, which allows the crystals to grow and develop inside the molten rock. Granite is transported to the surface of the earth by plate tectonics. The collision of continental plates moves the granite from deep within the crust of the earth to the surface. Granite is found in Ireland in the Wicklow Mountains. (http://www. talktalk. co. uk/reference/encyclopaedia/hutchinson/m0015252. html) Granite is distinguished by three features. Firstly, granite is composed of large mineral grains that bind tightly together. Secondly, granite always contains the minerals of quartz and feldspar. (http://www. windows2universe. org/earth/geology/ig_granite. html) These minerals give granite a light complexion, generally a pink or white colour. Thirdly, almost all granite is igneous and plutonic. This is because it formed from a fluid state, which was magma and it formed in a huge, deeply buried body also known as a pluton (http://geology. about. com/od/more_igrocks/a/granite. htm). Basalt Basalt is a common extrusive igneous rock. Basalt is commonly dark in colour. It has a fine-grained mineral texture which is due to the rapid cooling of the molten rock after it is erupted at a volcano. The rapid cooling occurs due to being exposed to the cooling air or water on the surface of the earth. Holden, 2012) Basalt is formed generally in three different environments: Oceanic divergent plate boundaries, oceanic hotspots and at hotspots and mantle plumes beneath continents. Basalt forms at oceanic divergent plate boundaries at mid-ocean ridges. At mid-ocean ridges convection currents pull the plates apart creating a rift valley. This allows hot rock from deep within the earths mantle to melt and erupt onto the seafloor forming bas alt. (Honan, 2011) At oceanic hotspots basalt is also formed. Hotspots are areas in the cente of tectonic plates where hot plumes of magma force there way to the surface. Basalt is formed at these hotspots when an eruption occurs on the ocean floor. If the eruptions are repeated enough times the basalt can build the volcanic cone larger and larger to form an island. The Hawaiian Islands are an example of this. (http://geology. com/rocks/basalt. shtml) Basalt is also formed in a continental environment where mantle plumes or hotspots can deliver large quantities of magma up to the earths surface. These eruptions generally form from fissures or vents and they produce some of the largest basalt flows on the continents. (http://geology. com/rocks/basalt. html) Basalt can be found in Ireland in the Giant’s Causeway in County Antrim. Limestone Limestone is a sedimentary rock. Sedimentary rocks are created by the processes of chemical or physical weathering . The sediment which is created from the processes of weathering can accumulate over time and eventually build up and harden to form solid rock. (Holden, 2012) Limestone in Ireland formed about 300 to 350 million years in warm shallow seas when Ireland lay close to the equator. Over millions of years the bodies of dead marine creatures such as shellfish and coral fell to the seafloor and built up on the seabed. Mud and sand particles from rivers also fell to the seafloor and added to the sediment. Over time the weight of the accumalting sediment compressed the sediment. Water and air was pushed from the pore spaces and calcium carbonate from the sediment binded the rock together. The process by which loose grains of sediment are compressed to form solid rock is called lithification. (Honan, 2011) Chemical weathering and eroison of limestone rock produced unusual landscapes in Ireland called karst landscapes. An example of a karst landscape in Ireland is the Burren in County Clare. Honan and Mulholland , 2007) Sandstone Sandstone is an inorganically formed sedimentary rock. It forms when particles of igneous, metamorphic and other types of sedimentary rocks are transported by rivers and gather on the seafloor or in lakes. The sediment layers then become compacted and over time cemented together by silica to form sandstone rock. (Honan S. , 2011) Sandstone in Ireland was formed 400-350 millio n years ago when Ireland was situated 30 degrees south of the equator. During this period Ireland was experiencing some very dry desert conditions. Many large rivers flowed across the dry landscape carrying the sediments which over time formed Old Red Sandstone which can now be found in the Cork and Kerry Mountains. (Honan and Mulholland , 2007) Schist Schist is a metamorphic rock. Metamorphic rocks are produced from existing sedimentary or igneous rocks usually as a result of partial melting and recrystallization. The changes normally occur where there is high pressure such as under hundreds of metres of bedrock or where rock is crushed at the meeting point of tectonic plates. Many metamorphic rocks have a layered structure due to this intense external pressure. Metamorphic rocks are often harder and more resistant than sedimentary rocks. (Holden, 2012) Schist in Ireland was formed through regional metamorphism. This is when large areas of rock covering many thousands of square kilometres are metamorphsed. Schist in Ireland was formed about 400 million years ago during the Caledonian folding period. The rocks changed due to huge pressure on the rocks created by plate movement. This deformed the rocks and forced them deep into the earth’s crust where they were heated to temperatures up to 1,000 degrees.