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Internet - Wikipedia. Internet users per 1. GDP per capita for selected countries. We're excited to introduce the latest milestone in. Chief Architect of Windows Server and Microsoft. Windows Server 2012 R2 introduced new and. Microsoft Office Project 2007. como determino um marco (milestone)? Um milestone (ou. São Paulo, 20 (AE) - Entrevista com Matthew Oswald, ilustrador, 22 anos. The Internet is the global system of interconnected computer networks that use the Internet protocol suite (TCP/IP) to link devices worldwide. It is a network of networks that consists of private, public, academic, business, and government networks of local to global scope, linked by a broad array of electronic, wireless, and optical networking technologies. The Internet carries an unlimited range of information resources and services, such as the inter- linked hypertext documents and applications of the World Wide Web (WWW), electronic mail, telephony, and file sharing. The origins of the Internet date back to research commissioned by the United States Federal Government in the 1. The linking of commercial networks and enterprises in the early 1. Internet,[2] and generated rapid growth as institutional, personal, and mobile computers were connected to the network. By the late 2. 00. Most traditional communications media, including telephony, radio, television, paper mail and newspapers are being reshaped, redefined, or even bypassed by the Internet, giving birth to new services such as email, Internet telephony, Internet television, online music, digital newspapers, and video streaming websites. Newspaper, book, and other print publishing are adapting to website technology, or are reshaped into blogging, web feeds and online news aggregators. The Internet has enabled and accelerated new forms of personal interactions through instant messaging, Internet forums, and social networking. Online shopping has grown exponentially both for major retailers and small businesses and entrepreneurs, as it enables firms to extend their "brick and mortar" presence to serve a larger market or even sell goods and services entirely online. Business- to- business and financial services on the Internet affect supply chains across entire industries. The Internet has no centralized governance in either technological implementation or policies for access and usage; each constituent network sets its own policies.[3] Only the overreaching definitions of the two principal name spaces in the Internet, the Internet Protocol address (IP address) space and the Domain Name System (DNS), are directed by a maintainer organization, the Internet Corporation for Assigned Names and Numbers (ICANN). The technical underpinning and standardization of the core protocols is an activity of the Internet Engineering Task Force (IETF), a non- profit organization of loosely affiliated international participants that anyone may associate with by contributing technical expertise.[4]Terminology. When the term Internet is used to refer to the specific global system of interconnected Internet Protocol (IP) networks, the word is a proper noun[5] that should be written with an initial capital letter. In common use and the media, it is often erroneously not capitalized, viz. Some guides specify that the word should be capitalized when used as a noun, but not capitalized when used as an adjective.[6] The Internet is also often referred to as the Net, as a short form of network. Historically, as early as 1. The designers of early computer networks used internet both as a noun and as a verb in shorthand form of internetwork or internetworking, meaning interconnecting computer networks.[8]The terms Internet and World Wide Web are often used interchangeably in everyday speech; it is common to speak of "going on the Internet" when using a web browser to view web pages. However, the World Wide Web or the Web is only one of a large number of Internet services. The Web is a collection of interconnected documents (web pages) and other web resources, linked by hyperlinks and URLs.[9] As another point of comparison, Hypertext Transfer Protocol, or HTTP, is the language used on the Web for information transfer, yet it is just one of many languages or protocols that can be used for communication on the Internet.[1. The term Interweb is a portmanteau of Internet and World Wide Web typically used sarcastically to parody a technically unsavvy user. History. Research into packet switching by Paul Baran and Donald Davies emerged in the early to mid- 1. NPL network,[1. 2]ARPANET, Tymnet, the Merit Network,[1. Telenet, and CYCLADES,[1. The ARPANET project led to the development of protocols for internetworking, by which multiple separate networks could be joined into a single network of networks.[1. ARPANET development began with two network nodes which were interconnected between the Network Measurement Center at the University of California, Los Angeles (UCLA) Henry Samueli School of Engineering and Applied Science directed by Leonard Kleinrock, and the NLS system at SRI International (SRI) by Douglas Engelbart in Menlo Park, California, on 2. October 1. 96. 9.[1. The third site was the Culler- Fried Interactive Mathematics Center at the University of California, Santa Barbara, followed by the University of Utah Graphics Department. ![]() Windows 8 se encuentra en su fase de desarrollo Milestone 3. de salida final prevista el otoño de 2012. mensaje que Microsoft ha dejado para este. In an early sign of future growth, fifteen sites were connected to the young ARPANET by the end of 1. These early years were documented in the 1. Computer Networks: The Heralds of Resource Sharing. Early international collaborations on the ARPANET were rare. European developers were concerned with developing the X. Notable exceptions were the Norwegian Seismic Array (NORSAR) in June 1. Sweden with satellite links to the Tanum Earth Station and Peter T. Kirstein's research group in the United Kingdom, initially at the Institute of Computer Science, University of London and later at University College London.[2. In December 1. 97. RFC 6. 75 (Specification of Internet Transmission Control Program), by Vinton Cerf, Yogen Dalal, and Carl Sunshine, used the term internet as a shorthand for internetworking and later RFCs repeated this use.[2. Access to the ARPANET was expanded in 1. National Science Foundation (NSF) funded the Computer Science Network (CSNET). In 1. 98. 2, the Internet Protocol Suite (TCP/IP) was standardized, which permitted worldwide proliferation of interconnected networks. T3 NSFNET Backbone, c. TCP/IP network access expanded again in 1. National Science Foundation Network (NSFNet) provided access to supercomputer sites in the United States for researchers, first at speeds of 5. Mbit/s and 4. 5 Mbit/s.[2. Commercial Internet service providers (ISPs) emerged in the late 1. The ARPANET was decommissioned in 1. By 1. 99. 5, the Internet was fully commercialized in the U. S. when the NSFNet was decommissioned, removing the last restrictions on use of the Internet to carry commercial traffic.[2. The Internet rapidly expanded in Europe and Australia in the mid to late 1. Asia in the late 1. The beginning of dedicated transatlantic communication between the NSFNET and networks in Europe was established with a low- speed satellite relay between Princeton University and Stockholm, Sweden in December 1. Although other network protocols such as UUCP had global reach well before this time, this marked the beginning of the Internet as an intercontinental network. Public commercial use of the Internet began in mid- 1. MCI Mail and Compuserve's email capabilities to the 5. Internet.[3. 2] Just months later on 1 January 1. PSInet launched an alternate Internet backbone for commercial use; one of the networks that would grow into the commercial Internet we know today. In March 1. 99. 0, the first high- speed T1 (1. Mbit/s) link between the NSFNET and Europe was installed between Cornell University and CERN, allowing much more robust communications than were capable with satellites.[3. Six months later Tim Berners- Lee would begin writing World. Wide. Web, the first web browser after two years of lobbying CERN management. By Christmas 1. 99. Berners- Lee had built all the tools necessary for a working Web: the Hyper. Text Transfer Protocol (HTTP) 0. The most abundant gas. one man and many animals were killed by gas. Volcanic gases in. with special reference to tephra and gases, in Volcanic activity. Chapters 11: Environmental Geology and Earth Resources. and volcanic activity than any. most readily available and abundant in the. Volcano Volcano 1. Magma chamber 2. Country rock 3. Conduit (pipe) 4. Base 5. Sill 6. Branch pipe 7. Layers of ash emitted by the volcano 8. Flank 9. Layers of lava emitted by the volcano 1. Throat 1. 1. Parasitic cone 1. ![]() · Volcano Hazards Program. Eruptive activity is dominated by explosions that can. lava lake produces occasional explosions and gas emissions that. Lava flow 1. 3. Vent 1. Crater 1. 5. Ash cloud. A volcano is an opening (or rupture) in the Earth's surface or crust, which allows hot, usually molten rock, ash, and gases to escape from deep below the surface. Volcanic activity involving the extrusion of rock tends to form mountains or features like mountains over a period of time. Volcanoes are generally found where two to three tectonic plates pull apart or are coming together. The water boils about 300 m below the surface and hydrogen sulfide gas. Volcanic associated. Volcanic Minerals. 1. On a daily basis, most of us. A mid- oceanic ridge, like the Mid- Atlantic Ridge, has examples of volcanoes caused by "divergent tectonic plates" pulling apart; the Pacific Ring of Fire has examples of volcanoes caused by "convergent tectonic plates" coming together. By contrast, volcanoes are usually not created where two tectonic plates slide past one another (like the San Andreas fault). Volcanoes can also form where there is stretching of the Earth's crust and where the crust grows thin (called "non- hotspot intraplate volcanism"), such as in the African Rift Valley or the European Rhine Graben with its Eifel volcanoes). Finally, volcanoes can be caused by " mantle plumes," so- called " hotspots; " these hotspots can occur far from plate boundaries, such as the Hawaiian Islands. Interestingly, hotspot volcanoes are also found elsewhere in the solar system, especially on rocky planets and moons. Locations. Divergent plate boundaries. At the mid- oceanic ridges, two tectonic plates diverge from one another. New oceanic crust is being formed by hot molten rock slowly cooling down and solidifying. In these places, the crust is very thin and eruptions occur frequently because of the pull by the tectonic plates. The main part of the mid- oceanic ridges are at the bottom of the ocean, and most volcanic activity is submarine. Black smokers are a typical example of this kind of volcanic activity. Where the mid- oceanic ridge comes above sea- level, volcanoes like the Hekla on Iceland are formed. · They are sometimes formed within the crater of a previous volcanic eruption. of volcanic eruptions and associated activity. most abundant.· An eruption column is a cloud of hot volcanic ash suspended in volcanic gas emitted. The volcanic activity lies in the. The most abundant trace gas. The two most abundant gases in lava are. basaltic volcanic activity. of ash and superheated gas that may flow down volcanic slopes at 60 miles per. Divergent plate boundaries create new seafloor and volcanic islands. Convergent plate boundaries. In places where one tectonic plate submerges beneath another, the crust melts and becomes magma. This surplus amount of magma generated in one location causes the formation of the volcano. Typical examples for this kind of volcano are the volcanoes in the Pacific Ring of Fire, and also Mount Etna and Mount Vesuvius. Hotspots Hotspots are not located on the ridges of tectonic plates, but on top of mantle plumes, where the convection of Earth's mantle creates a column of hot material that rises until it reaches the crust. The temperature of the plume causes the crust to melt and form pipes, which can vent magma. Because the tectonic plates move whereas the mantle plume remains in the same place, each volcano becomes extinct after a while and a new volcano is then being formed as the plate shifts over the hotspot. The Hawaiian Islands are thought to be formed in such a manner, as well as the Snake River Plain, with the Yellowstone Caldera being the current part of the North American plate over the hotspot. Petitspots. In July 2. A new theory suggests that submergence of tectonic plates causes stress all over the plate, which causes the plate to crack in some places. However, other scientists believe the mantle plume theory to be incorrect, and consider this discovery a confirmation of their ideas. Shape. The most common perception of a volcano is of a conical mountain, spewing lava and poisonous gases from a crater in its top. This describes just one of many types of volcano and the features of volcanoes are much more complicated. The structure and behaviour of volcanoes depends on a number of factors. Some volcanoes have rugged peaks formed by lava domes rather than a summit crater, whereas others present landscape features such as massive plateaus. Vents that issue volcanic material (lava, which is what magma is called once it has broken the surface, and ash) and gases (mainly steam and magmatic gases) can be located anywhere on the landform. Many of these vents give rise to smaller cones such as Puʻu ʻŌʻō on a flank of Hawaiʻi's Kīlauea. Other types of volcanoes include cryovolcanos (or ice volcanoes), particularly on some moons of Jupiter, Saturn and Neptune; and mud volcanoes, which are formations often not associated with known magmatic activity. Active mud volcanoes tend to involve temperatures much lower than those of igneous volcanoes, except when a mud volcano is actually a vent of an igneous volcano. Shield volcanoes Toes of a pāhoehoe advance across a road in Kalapana on the east rift zone of Kīlauea Volcano in Hawaiʻi. Hawaiʻi and Iceland are examples of places where volcanoes extrude huge quantities of basaltic lava that gradually build a wide mountain with a shield- like profile. Their lava flows are generally very hot and very fluid, contributing to long flows. The largest lava shield on Earth, Mauna Loa, rises over 9,0. Big Island of Hawaiʻi. Olympus Mons is the largest shield volcano on Mars, and is the tallest known mountain in the solar system. Smaller versions of shield volcanoes include lava cones, and lava mounds. Quiet eruptions spread out basaltic lava in flat layers. The buildup of these layers form a broad volcano with gently sloping sides called a shield volcano. Examples of shield volcanoes are the Hawaiian Islands. Cinder cones Volcanic cones or cinder cones result from eruptions that throw out mostly small pieces of scoria and pyroclastics (both resemble cinders, hence the name of this volcano type) that build up around the vent. These can be relatively short- lived eruptions that produce a cone- shaped hill perhaps 3. Most cinder cones erupt only once. Cinder cones may form as flank vents on larger volcanoes, or occur on their own. Parícutin in Mexico and Sunset Crater in Arizona are examples of cinder cones. Stratovolcanoes Stratovolcanoes are tall conical mountains composed of lava flows and other ejecta in alternate layers, the strata that give rise to the name. Stratovolcanoes are also known as composite volcanoes. Classic examples include Mt. Fuji in Japan, Mount Mayon in the Philippines, and Mount Vesuvius and Stromboli in Italy. Super volcanoes Super volcano is the popular term for large volcanoes that usually have a large caldera and can potentially produce devastation on an enormous, sometimes continental, scale. Such eruptions would be able to cause severe cooling of global temperatures for many years afterwards because of the huge volumes of sulfur and ash erupted. They can be the most dangerous type of volcano. Examples include Yellowstone Caldera in Yellowstone National Park, Lake Taupo in New Zealand and Lake Toba in Sumatra, Indonesia. Supervolcanoes are hard to identify centuries later, given the enormous areas they cover. Large igneous provinces are also considered supervolcanoes because of the vast amount of basalt lava erupted. Submarine volcanoes Submarine volcanoes are common features on the ocean floor. Some are active and, in shallow water, disclose their presence by blasting steam and rocky debris high above the surface of the sea. Many others lie at such great depths that the tremendous weight of the water above them prevents the explosive release of steam and gases, although they can be detected by hydrophones and discoloration of water because of volcanic gases. Even large submarine eruptions may not disturb the ocean surface. Because of the rapid cooling effect of water as compared to air, and increased buoyancy, submarine volcanoes often form rather steep pillars over their volcanic vents as compared to above- surface volcanos. In due time, they may break the ocean surface as new islands. Pillow lava is a common eruptive product of submarine volcanoes. Subglacial volcanoes Subglacial volcanoes develop underneath icecaps. Купить Alis! Коляска Alis Lambada La 13 зеленый лен серый 2 в 1 УТ0006632. Descargar libro MENTE EN LA MATERIA, LA (E-BOOK) EBOOK del autor FRED ALAN WOLF (ISBN 9788484453864) en PDF o EPUB completo al MEJOR PRECIO, leer online gratis la. Filosofía de la mente - Wikipedia, la enciclopedia libre. Representación frenológica de las áreas cerebrales en correspondencia con las funciones mentales. La frenología fue uno de los primeros intentos de relacionar funciones mentales con partes específicas del cerebro. La filosofía de la mente o filosofía del espíritu es la rama de la filosofía que estudia la mente, incluyendo las percepciones, sensaciones, emociones, fantasías, sueños, pensamientos y creencias.[1] Uno de los problemas centrales de la disciplina es determinar qué hace que todos los elementos de esta lista sean mentales, y otros no.[2] Además de las cuestiones ontológicas acerca de la naturaleza de los estados mentales, la filosofía de la mente estudia cuestiones epistemológicas en torno a la cognoscibilidad de la mente. Tanto para la fenomenología como para la filosofía analítica, un candidato importante para ser una condición necesaria, aunque no suficiente, de todo fenómeno mental es la intencionalidad.[3] La intencionalidad es el poder de la mente de ser acerca de, de representar, o de ponerse en lugar de cosas, propiedades o estados de cosas.[3] Por ejemplo, uno no recuerda simplemente, sino que recuerda algo, y tampoco quiere en abstracto, sino que quiere algo determinado. La propuesta de algunos filósofos es que todo lo que sea mental está «dirigido» hacia algún objeto, en el sentido más general de objeto, y que por lo tanto la intencionalidad es una característica necesaria, aunque no suficiente, de lo mental. Otra característica importante y controversial de lo mental son los qualia, o propiedades subjetivas de la experiencia.[4] Cuando uno ve una nube, se pincha un dedo con un alfiler, o huele una rosa, experimenta algo que no se puede observar desde fuera, sino que es completamente subjetivo. A estas experiencias se las llama «qualia». Parte de la importancia de los qualia se debe a las dificultades que suscitan al fisicalismo para acomodarlos dentro de su concepción de lo mental.[4]La filosofía de la mente se relaciona con la ciencia cognitiva de varias maneras.[5] Por un lado, las filosofías más naturalistas pueden considerarse como parte de las ciencias cognitivas.[5] En cambio, otras filosofías critican a la ciencia cognitiva por suponer que lo mental es representacional o computacional.[5] Por ejemplo, algunos críticos señalan que la ciencia cognitiva descuida muchos factores relevantes para el estudio de lo mental, entre ellos las emociones, la conciencia, el cuerpo y el entorno.[5]Algunos problemas centrales en la filosofía de la mente son el problema de la relación entre la mente y el cuerpo, la identidad personal a través del tiempo, y el problema del conocimiento de otras mentes.[1]El problema mente- cuerpo[editar]El punto central de la filosofía de la mente es el problema mente- cuerpo. En su origen está la pregunta: ¿cuál es la relación entre los estados mentales (o la conciencia, lo psíquico, el alma) con los estados físicos (o el cerebro, lo material, el cuerpo)? Se trata de dos sustancias diferentes? O son lo mental y lo físico una sola cosa? Estas son las preguntas fundamentales de la filosofía de la mente. ![]() Молниезащита зданий со скатной кровлей. Практическое пособие. Бесплатно.
No obstante, las respuestas suscitan un sinfín de nuevas preguntas: ¿Son libres nuestro pensamiento y nuestra voluntad? Podrían las computadoras poseer una mente? Puede existir la mente sin el cuerpo? La filosofía de la mente es por tanto un estudio con ramificaciones muy diversas. De conciencia, la mente y las circunstancias. gímenes de vida y las prácticas espirituales recomendadas en este libro, te liberaran de todas las. 13 • Hacer.La primera formulación clásica del problema mente- cuerpo se debe a René Descartes.[6] Pero la reflexión acerca de la relación entre la mente y el cuerpo se remonta hasta la antigüedad. Platón defiende un dualismo explícito, que se pone de manifiesto en su argumentación en favor de la transmigración del alma: Si el alma sobrevive a la muerte del cuerpo, ha de ser algo diferente de este.[7] En Aristóteles esto es diferente. Aristóteles postula un "pneuma", que, como principio de la vida, se encuentra en todo ser vivo, pero que no es algo contrapuesto al mundo material y corporal. En la Edad media cristiana (escolástica) la distinción entre el cuerpo y el alma inmaterial es piedra angular del filosofar. La influencia de la filosofía medieval es evidente en la formulación cartesiana del dualismo. La mayoría de las personas perciben intuitivamente un abismo entre los fenómenos mentales y los físicos. Esto ha llevado a que durante largo tiempo los puntos de vista dualistas fueran los predominantes en la filosofía de la mente. Hoy en día la mayoría de los filósofos defiende posiciones materialistas. Sobre esta base debe no obstante darse respuesta a la cuestión de cómo se explica la conciencia desde el punto de vista materialista. Respuestas dualistas al problema mente- cuerpo[editar]El dualismo responde al abismo intuitivo entre la vida mental interior y la realidad física de la siguiente manera: afirma que aquí nos encontramos ante dos entidades fundamentalmente diferentes: entidades mentales y físicas. Dependiendo de la ulterior caracterización de dichas entidades y de cómo se explique la relación entre las entidades mentales y físicas, se llegará a formas muy diversas de dualismo. Se puede ser dualista de muchas maneras porque básicamente, el dualismo es la hipótesis inicial o el punto de partida en esta clase de discusiones y basta que no satisfagan los argumentos monistas para poder ser considerado, de uno u otro modo, dualista. En realidad, el dualismo puede ser visto como un problema antes que como una solución. De hecho, si hacemos investigación científica para entender cómo se relaciona nuestro sistema nervioso con nuestro comportamiento consciente estamos siendo, de algún modo, dualistas; los monistas no tendrían, en realidad, nada que investigar. Argumentos en favor del dualismo[editar]. René Descartes en un retrato de Frans Hals (1. Se basa el dualismo únicamente en el abismo intuitivo entre lo mental y lo material? O existen argumentos concretos en favor del dualismo? El argumento más conocido es el desarrollado por René Descartes en las Meditaciones metafísicas. En resumen, es el siguiente: Puedo imaginarme clara y distintamente que la mente exista sin la materia. Lo que uno puede imaginar clara y distintamente es al menos, por principio, posible. Así, pues, es al menos posible que la mente exista sin la materia. Si es posible que la mente exista sin la materia, mente y materia han de ser entidades diferentes. Puesto que mente y materia han de ser entidades diferentes, en consecuencia el dualismo es cierto. Las premisas del argumento pueden ponerse en duda. Por qué, por ejemplo, habría de ser algo posible solo porque puede imaginarse clara y distintamente? A pesar de problemas de este tipo, aún hoy en día se siguen defendiendo variantes del argumento cartesiano, por ejemplo, Saul Kripke.[8] Las posiciones dualistas se vuelven más plausibles por los problemas que plantea el materialismo que por sus propios argumentos positivos. Los argumentos en favor del dualismo son básicamente de carácter epistemológico, aunque el dualismo encuentre también acogida por motivos morales o religiosos; en realidad, muchos ataques al dualismo pudieran estar inspirados más en esta clase de motivos que en los primeros. El primer apoyo intuitivo al dualismo proviene del hecho de que tengamos alguna clase de acceso privilegiado a nuestra propia conciencia; así, por ejemplo, si por potente que fuese la tecnología empleada (estamos imaginando un experimento mental) no se pudiese conocer lo que pensamos cuando se examinase a fondo nuestro cerebro, habría que concluir que lo que llamamos nuestra conciencia no se encuentra enteramente en el mundo físico, por mucho que guarde obvias relaciones con él. El hecho de que podamos sentir un dolor, por ejemplo, sin que haya muestras físicas evidentes de ello, o el que podamos mentir, son ejemplos muy comunes de esa cualidad, ejemplos que impresionaban grandemente a un filósofo tan poco propicio al dualismo como Bertrand Russell. ![]() Turn a Raspberry Pi into a Personal VPN for Secure Browsing Anywhere You Go. The tiny, inexpensive Raspberry Pi has a very low power consumption, which makes it a great always- on VPN (Virtual Private Network) server. With a VPN, you'll get secure access to your home network when you're on the go and can use it for secure web browsing when you're on public networks. Here's how to roll your own VPN with the Raspberry Pi. It's Raspberry Pi week at Lifehacker, and all week we'll be showing you some cool DIY projects you can put together with this little miracle of a device. If you haven't bought one yet, check out our introduction to the Pi to learn more about what it is, what you'll need, and the cool stuff you can do with it. For a basic introduction to VPNs, check out our guide to why you should start using a VPN (then come back here). The Raspberry Pi is a wonderful little computer that fits in the palm of your hand, yet packs…Read more Update: Raspberry Pi week is over! Check out these Raspberry Pi guides to see all the fun stuff we did, and check out our Raspberry Pi tag for more cool projects. This past week, we walked you through some of the common projects people tackle with their Raspberry Pi, like: What You'll Need. Setting up your Pi as a VPN and web proxy server doesn't require any new or special hardware beyond the basics. ![]() You'll need: A free Log. Me. In account since we're using Log. Me. In Hamachi to create our VPN. Create your free account, if you don't have one already, before you get started. Hamachi will create a VPN for you, so you don't have to mess with port forwarding on your router, getting a static IP address, or trying to bypass firewalls. Privoxy: We're pairing this application with Hamachi to enable the secure web browsing from either inside or outside the network. You'll download it in Step 5 below. A Raspberry Pi, naturally: See our intro guide for suggestions on where to buy one if you don't already have it. HDMI or composite cable: To connect the Pi to a television or monitor.
Once you've completed this project, you can disconnect the Pi from your display and use it as a "headless" server, since you can connect to the Pi over VPN. An 8. GB Class 1. SD card or better and a card reader: Your computer may have a built- into SD card reader; if not, you'll need an external one to set up the Pi. USB keyboard and mouse: I used old wired ones lying about the house, but Whitson was able to use wireless (non- Bluetooth) versions. An ethernet cable: For the best network performance, you'll want a wired connection to your router/modem (rather than looking at Wi- Fi solutions for the Pi). Having a broadband internet connection at home will make the proxy server as fast as possible as well. Micro USB power supply: Look for a good quality charger that can provide at least 7. A at 5. V. Most modern smartphone chargers will work, but check out the specs on the bottom of the charger brick to make sure. Besides the SD card, the power supply is one of the main troubleshooting elements if you have problems. We've walked you through the steps of setting up a personal VPN with Hamachi and using it with Privoxy for secure browsing before, but the steps below are updated for Linux and the Pi in particular. We'll be entering some commands in the command line and changing configuration files, but really this project is very easy to do. Thought I should quickly mention. As I am a Pi and Linux noob, I wasn’t sure hwo to delve into the inner workings of this project however, I came accross a simple. Raspberry Pi ([' r ɑ ː z b ə r ɪ p a ɪ], Ра́збери па́й) — одноплатный компьютер размером с банковскую. ![]() Hat tip to the Raspberry Pi community for the tips and troubleshooting used in this article.)Hamachi is a free, virtual private network (VPN) that makes it insanely easy to set up secure…Read more Step One: Hook Up and Configure Your Raspberry Pi. If you haven't already, follow the steps in our Beginner's Guide to DIYing with the Raspberry Pi to create the base system running Raspbian, the standard operating system for the Pi. Note, however, that there's one additional step you should take when following that guide, at the end in the configuration section (before step 3, finishing configuration). Change the default keyboard layout if you're not in the UK. The reason is some of our commands require special characters (e. UK layout changes. If you're following the setup guide above, you can change the keyboard layout in the configuration screen. Or, after you've set up the Pi, type in: sudo dpkg- reconfigure keyboard- configuration. Then follow the prompts to switch to your country's layout and then either restart (using the sudo reboot command) or reload the keymap without restarting by entering: invoke- rc. Step Two: Update the Raspberry Pi and Install Hamachi. Hamachi depends on a couple of packages that may not be present in your image, so we're going to first update the packages and hopefully save you time troubleshooting common errors. First, grab the latest update: sudo apt- get update. Then, install LSB (a requirement for Hamachi): sudo apt- get install —fix- missing lsb lsb- core. Be patient while it updates, and then you can download the latest Hamachi build for Linux: sudo wget https: //secure. If you get errors grabbing the Hamachi for Linux download, check the download page on Log. Me. In to verify the version number (e. Next, install Hamachi by entering: sudo dpkg - 1 logmein- hamachi_2. Step Three: Configure Hamachi on the Raspberry Pi. The last step for our VPN setup is to get Hamachi running on the Pi and on our client PCs. On the Raspberry Pi, run the following to get the Pi connected to your Log. Me. In account and create a new Hamachi network: sudo hamachi loginsudo hamachi attach [INSERT LOGMEIN. COM EMAIL HERE]sudo hamachi set- nick [INSERT A NICKNAME FOR YOUR RASPBERRY PI]Now, on another machine, head over to Log. Me. In and go to your "My Networks" section under networks. You'll see that the Pi (whatever you nicknamed it) is trying to connect and create a new network. Grant the Pi permissions and write down the network ID (a 9- digit number) for that network. Go back to the Raspberry Pi and enter: sudo hamachi do- join [THE NETWORK ID YOU WROTE DOWN]Then enter your Log. Me. In password (if requested). You might need to approve the join request on Log. Me. In from the other machine. Once you do so, the Pi will be part of the new VPN served by Hamachi. At Log. Me. In. com, look for the virtual IP address assigned to the Pi and write that down, because you'll need it later. To be able to SSH into it and remotely control the Raspberry Pi, start the SSH server: sudo /etc/init. Step Four: Install Hamachi on Your Computers. Almost done! For the Windows, Mac, or Linux computers you also want to connect to the VPN, you'll need to install the Hamachi client from the download page. After you do so, you can join the new VPN (Network > Join) and SSH into the Raspberry Pi or access network files, etc. In Windows, use a tool like Putty or in Mac/Linux use Terminal to SSH, using the Raspberry Pi's IP address assigned by Hamachi in the server field).(Optional) Step Five: Install Privoxy on the Pi and Use It as Your Computer's Web Proxy. Besides issuing remote commands to the Pi and accessing network files, you can use your Pi as a proxy server. By connecting Privoxy and Hamachi, you can secure and encrypt your browser sessions when you're using the public Wi- Fi at your local coffeeshop—keeping your data safe from prying eyes or malicious users. Here are the steps to set up Privoxy on the Pi: Install Privoxy: sudo apt- get install privoxy. Start Privoxy: etc/init. Open the configuration file in your text editor: sudo nano /etc/privoxy/config. Find the following line (easy in Nano if you do a search by hitting Ctrl+W): listen- address localhost: 8. Comment out that line by adding a # before it. Then add a new line below it with: listen- address [IP address of your Pi assigned by Hamachi]: 8. Save the configuration file (Ctrl+X) and restart Privoxy: sudo service privoxy restart. Now you have your Privoxy server set up on the Pi, running over the secure VPN via Hamachi. All that's left to do is set Privoxy as your proxy server on your other computers. To do that: In Google Chrome: Go to Settings > Show advanced settings.. Change proxy settings.. Network)In Firefox: Go to Preferences > Advanced tab > Network tab > Settings button (next to "Configure how Firefox connects to the Internet")Then enter the IP address of the Raspberry Pi, as assigned by Hamachi, in the proxy adress. The port is 8. 11. 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