0_Wizard
I really want to live in Iceland. It's a European Nordic Island country in the North Atlantic Ocean.
Iceland (; , ) is a Nordic island country of Europe located in the North Atlantic Ocean.
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Iceland
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Iceland
Iceland (; , ) is a Nordic island country of Europe located in the North Atlantic Ocean. It has a population of and an area of , making it the most sparsely populated country in Europe. The capital and largest city is Reykjavík. Reykjavík and the surrounding areas in the southwest of the country are home to over two-thirds of the population. Iceland is volcanically and geologically active. The interior consists of a plateau characterised by sand and lava fields, mountains, and glaciers, while many glacial rivers flow to the sea through the lowlands. Iceland is warmed by the Gulf Stream and has a temperate climate, despite a high latitude just outside the Arctic Circle.
Atlantic Ocean
The Atlantic Ocean is the second largest of the world's oceans with a total area of about . It covers approximately 20 percent of the Earth's surface and about 29 percent of its water surface area. It separates the "Old World" from the "New World". The Atlantic Ocean occupies an elongated, S-shaped basin extending longitudinally between Eurasia and Africa to the east, and the Americas to the west. As one component of the interconnected global ocean, it is connected in the north to the Arctic Ocean, to the Pacific Ocean in the southwest, the Indian Ocean in the southeast, and the Southern Ocean in the south (other definitions describe the Atlantic as extending southward to Antarctica).
Nordic countries
The Nordic countries or the Nordic are a geographical and cultural region in Northern Europe and the North Atlantic, where they are most commonly known as "Norden" (literally "the North"). They consist of Denmark, Finland, Iceland, Norway and Sweden, including Greenland and Faroe Islands—which are both constituent countries within the Kingdom of Denmark—and the Åland Islands. The population of the Nordic countries are mainly Scandinavian or Finnish, with Greenlandic Inuit and the Sami people as indigenous minorities, since Scandinavians comprise over three quarters of the region's population and is thus the largest group by far.
Faroe Islands
The Faroe Islands (; ; , ), sometimes called the Faeroe Islands, is an archipelago between the Norwegian Sea and the North Atlantic, about halfway between Norway and Iceland, north-northwest of Scotland. The islands are an autonomous country within the Kingdom of Denmark. Their area is about with a population of 50,322 in October 2017. The Faroes' terrain is rugged, and the islands have a subpolar oceanic climate (Cfc): windy, wet, cloudy, and cool. Despite this island group's northerly latitude, temperatures average above freezing throughout the year because of the Gulf Stream. Between 1035 and 1814, the Faroes were part of the Hereditary Kingdom of Norway.
North Atlantic right whale
The North Atlantic right whale ("Eubalaena glacialis", which means "good, or true, whale of the ice") is a baleen whale, one of three right whale species belonging to the genus "Eubalaena", all of which were formerly classified as a single species. Because of their docile nature, their slow surface-skimming feeding behaviors, their tendencies to stay close to the coast, and their high blubber content (which makes them float when they are killed, and which produced high yields of whale oil), right whales were once a preferred target for whalers. At present, they are among the most endangered whales in the world, and they are protected under the U.S.
Denmark
Denmark (; , ), officially the Kingdom of Denmark, is a Nordic country and a sovereign state. The southernmost of the Scandinavian nations, it is south-west of Sweden and south of Norway, and bordered to the south by Germany. The Kingdom of Denmark also comprises two autonomous constituent countries in the North Atlantic Ocean: the Faroe Islands and Greenland. Denmark proper consists of a peninsula, Jutland, and an archipelago of 443 named islands, with the largest being Zealand, Funen and the North Jutlandic Island. The islands are characterised by flat, arable land and sandy coasts, low elevation and a temperate climate.
World War II by country
Nearly every country in the world participated in World War II, with the exception of a few countries that remained neutral. The Second World War pitted two alliances against each other, the Axis powers and the Allied powers. The leading Axis powers were Nazi Germany, the Kingdom of Italy and the Empire of Japan; while the United Kingdom, the United States, the Soviet Union and China were the "Big Four" Allied powers. Even though the Axis had the support of a handful of minor allies and client states, by 1945 almost every single country in the world had declared war on them, although many of them did so only at the eleventh hour.
1_Apprentice
Ive been curious about Iceland lately. Does it have a high population? Id want to visit there some day. 
0_Wizard
Actually, it is the most sparsely populated country in Europe.
It has a population of and an area of , making it the most sparsely populated country in Europe.
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Iceland
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Netherlands
The Netherlands (; ), also known informally as Holland, is a country in Western Europe with a population of seventeen million. Together with three island territories in the Caribbean (Bonaire, Sint Eustatius and Saba), it forms the main constituent country of the Kingdom of the Netherlands. The European portion of the Netherlands consists of twelve provinces and borders Germany to the east, Belgium to the south, and the North Sea to the northwest, sharing maritime borders in the North Sea with Belgium, the United Kingdom, and Germany. The five largest cities in the Netherlands are Amsterdam, Rotterdam, The Hague, Utrecht (forming the Randstad megalopolis) and Eindhoven (leading the Brabantse Stedenrij).
Philippines
The Philippines (; or ' ), officially the Republic of the Philippines () is a unitary sovereign state and island country in Southeast Asia. Situated in the western Pacific Ocean, it consists of about 7,641 islands that are categorized broadly under three main geographical divisions from north to south: Luzon, Visayas, and Mindanao. The capital city of the Philippines is Manila and the most populous city is Quezon City, both part of Metro Manila. Bounded by the South China Sea on the west, the Philippine Sea on the east and the Celebes Sea on the southwest, the Philippines shares maritime borders with Taiwan to the north, Vietnam to the west, Palau to the east and Malaysia and Indonesia to the south.
Iceland
Iceland (; , ) is a Nordic island country of Europe located in the North Atlantic Ocean. It has a population of and an area of , making it the most sparsely populated country in Europe. The capital and largest city is Reykjavík. Reykjavík and the surrounding areas in the southwest of the country are home to over two-thirds of the population. Iceland is volcanically and geologically active. The interior consists of a plateau characterised by sand and lava fields, mountains, and glaciers, while many glacial rivers flow to the sea through the lowlands. Iceland is warmed by the Gulf Stream and has a temperate climate, despite a high latitude just outside the Arctic Circle.
Sweden
Sweden ( ; ), officially the Kingdom of Sweden (Swedish: ), is a Scandinavian country in Northern Europe. It borders Norway to the west and north and Finland to the east, and is connected to Denmark in the southwest by a bridge-tunnel across the Öresund. At , Sweden is the third-largest country in the European Union by area. Sweden has a total population of 10 million of which 2.3 million has a foreign background. It has a low population density of ; the highest concentration is in the southern half of the country. Approximately 85% of the population lives in urban areas. Germanic peoples have inhabited Sweden since prehistoric times, emerging into history as the Geats (Swedish Götar) and Swedes (Svear) and constituting the sea peoples known as the Norsemen.
New England town
The New England town (generally referred to simply as a town in New England) is the basic unit of local government and local division of state authority in each of the six New England states and without a direct counterpart in most other U.S. states. New England towns overlay the entire area of a state, similar to civil townships in other states where they exist, but they are fully functioning municipal corporations, possessing powers similar to cities in other states. New Jersey's system of equally powerful townships, boroughs, towns, and cities is the system which is most similar to that of New England.
Renewable energy in Scotland
The production of renewable energy in Scotland is an issue that has come to the fore in technical, economic, and political terms during the opening years of the 21st century. The natural resource base for renewable energy is extraordinary by European, and even global standards, with the most important potential sources being wind, wave, and tide. In 2015, Scotland generated 59% of its electricity consumption through renewable sources, exceeding the country's lofty goal of 50% renewable energy by 2015. Moving forward, the Scottish Government's energy plan calls for 100% of electricity consumption to be generated through renewable sources by 2020, and 50% of total energy consumption (including transportation) by 2030.
History of Palestine
The history of Palestine is the study of the past in the region of Palestine, generally defined as a geographic region in the Southern Levant between the Mediterranean Sea and the Jordan River (where Israel and Palestine are today), and various adjoining lands. Situated at a strategic point between Europe, Asia, and Africa, and the birthplace of Judaism and Christianity, the region has a long and tumultuous history as a crossroads for religion, culture, commerce, and politics. The Palestine region or parts of it have been controlled by numerous different peoples and regional powers, including the Canaanites, Amorites, Ancient Egyptians, Israelites, Moabites, Ammonites, Tjeker, Philistines, Assyrians, Babylonians, Persians, ancient Greeks, Romans, Byzantines, different dynasties of the Early Muslim period (Umayads, Abbasids, Seljuqs, Fatimids), Crusaders, Late Muslim dynasties (Ayyubids, Mamluks, Ottoman Turks), the British, Jordanians (1948–1967, on the "West Bank") and Egyptians (in Gaza), and modern Israelis and Palestinians.
1_Apprentice
Oh wow thats wild, What are the best tourists spots in Iceland? Any recommendations? 
0_Wizard
It is volcanically active so there are lots of volcanoes and hot springs!
Iceland is volcanically and geologically active.
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Volcanology of Canada
Volcanology of Canada includes lava flows, lava plateaus, lava domes, cinder cones, stratovolcanoes, shield volcanoes, submarine volcanoes, calderas, diatremes, and maars, along with examples of more less common volcanic forms such as tuyas and subglacial mounds. It has a very complex volcanological history spanning from the Precambrian eon at least 3.11 billion years ago when this part of the North American continent began to form. Although the country's volcanic activity dates back to the Precambrian eon, volcanism continues to occur in Western and Northern Canada where it forms part of an encircling chain of volcanoes and frequent earthquakes around the Pacific Ocean called the Pacific Ring of Fire.
Volcano
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. Earth's volcanoes occur because its crust is broken into 17 major, rigid tectonic plates that float on a hotter, softer layer in its mantle. Therefore, on Earth, volcanoes are generally found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-oceanic ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates.
El Tatio
El Tatio is a geyser field located within the Andes Mountains of northern Chile at 4,320 meters above mean sea level. Various etymologies have been proposed for the system, including "oven" but also "grandfather". It is the third-largest geyser field in the world and the largest in the southern hemisphere. El Tatio lies at the western foot of a series of stratovolcanoes which run along the border between Chile and Bolivia. This series of volcanoes is part of the Central Volcanic Zone, one of several volcanic belts in the Andes, and there are no recorded historical eruptions at the Tatio volcanoes.
Lassen Peak
Lassen Peak, commonly referred to as Mount Lassen, is the southernmost active volcano in the Cascade Range of the Western United States. Located in the Shasta Cascade region of Northern California, it is part of the Cascade Volcanic Arc, which stretches from southwestern British Columbia to northern California. Lassen Peak reaches an elevation of , standing above the northern Sacramento Valley. It supports many flora and fauna among its diverse habitats, which are subject to frequent snowfall and reach high elevations. A lava dome, Lassen Peak has a volume of making it one of the largest lava domes on Earth.
Tacora
Tacora is a stratovolcano located in the Andes of the Arica y Parinacota Region of Chile. Bordering Peru, it is the northernmost volcano of Chile. It is part of the Central Volcanic Zone in Chile, one of the four volcanic belts of the Andes. The Central Volcanic Zone has several of the highest volcanoes in the world. Tacora itself is a stratovolcano with a caldera and a crater; it is heavily eroded by glacial activity and its youngest radiometric age is 50,000 years ago. Volcanism in the Central Volcanic Zone results from the subduction of the Nazca Plate beneath the South America Plate. Tacora is constructed on the so-called "Arica Altiplano" and is part of a north-south alignment of volcanoes.
Level Mountain
Level Mountain is a massive complex volcano in the Northern Interior of British Columbia, Canada. It is located north-northwest of Telegraph Creek and west of Dease Lake on the Nahlin Plateau. With a maximum elevation of , it is the third highest of five large volcanic complexes in the Northern Cordilleran Volcanic Province (NCVP). Much of the mountain is gently-sloping; when measured from its base, Level Mountain is about tall, slightly taller than its neighbour to the northwest, Heart Peaks. The lower broader half of Level Mountain consists of a shield-like edifice while its upper half has a more steep, jagged profile.
Hot Springs, Arkansas
Hot Springs is the eleventh-largest city in the state of Arkansas and the county seat of Garland County. The city is located in the Ouachita Mountains among the U.S. Interior Highlands, and is set among several natural hot springs for which the city is named. As of the 2010 United States Census, the city had a population of 35,193. In 2015 the estimated population was 35,635. The center of Hot Springs is the oldest federal reserve in the United States, today preserved as Hot Springs National Park. The hot spring water has been popularly believed for centuries to possess medicinal properties, and was a subject of legend among several Native American tribes.
1_Apprentice
Oh neat! Id love to go see some hot springs and maybe a volcano. But I wouldnt get too close. Does it always stay cold in Iceland?
0_Wizard
Even though it has a high latitude, it is warmed by the Gulf Stream so the climate is temperate.
Iceland is warmed by the Gulf Stream and has a temperate climate, despite a high latitude just outside the Arctic Circle.
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Iceland
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List of ecoregions in North America (CEC)
This list of ecoregions of North America provides an overview of North American ecoregions designated by the Commission for Environmental Cooperation (CEC) in its North American Environmental Atlas. It should not be confused with Wikipedia articles based on the classification system developed by the World Wildlife Fund, such as List of ecoregions (WWF) and Lists of ecoregions by country. The commission was established in 1994 by the member states of Canada, Mexico, and the United States to address regional environmental concerns under the North American Agreement on Environmental Cooperation (NAAEC), the environmental side accord to the North American Free Trade Agreement (NAFTA).
Gulf Stream
The Gulf Stream, together with its northern extension the North Atlantic Drift, is a warm and swift Atlantic ocean current that originates in the Gulf of Mexico and stretches to the tip of Florida, and follows the eastern coastlines of the United States and Newfoundland before crossing the Atlantic Ocean. The process of western intensification causes the Gulf Stream to be a northward accelerating current off the east coast of North America. At about , it splits in two, with the northern stream, the North Atlantic Drift, crossing to Northern Europe and the southern stream, the Canary Current, recirculating off West Africa.
Climate of the United Kingdom
The United Kingdom straddles the higher mid-latitudes between 49° and 61° N. It is on the western seaboard of Afro-Eurasia, the world's largest land mass. Since the UK is always in or close to the path of the polar front jet stream, frequent changes in pressure and unsettled weather are typical. Many types of weather can be experienced in a single day. In general the climate of the UK is cool and often cloudy, and hot temperatures are infrequent. The climate in the United Kingdom is defined as a temperate oceanic climate, or "Cfb" on the Köppen climate classification system, a classification it shares with most of north-west Europe.
Thermohaline circulation
Thermohaline circulation (THC) is a part of the large-scale ocean circulation that is driven by global density gradients created by surface heat and freshwater fluxes. The adjective "thermohaline" derives from "thermo-" referring to temperature and "" referring to salt content, factors which together determine the density of sea water. Wind-driven surface currents (such as the Gulf Stream) travel polewards from the equatorial Atlantic Ocean, cooling en route, and eventually sinking at high latitudes (forming North Atlantic Deep Water). This dense water then flows into the ocean basins. While the bulk of it upwells in the Southern Ocean, the oldest waters (with a transit time of around 1000 years) upwell in the North Pacific.
Atlantic Ocean
The Atlantic Ocean is the second largest of the world's oceans with a total area of about . It covers approximately 20 percent of the Earth's surface and about 29 percent of its water surface area. It separates the "Old World" from the "New World". The Atlantic Ocean occupies an elongated, S-shaped basin extending longitudinally between Eurasia and Africa to the east, and the Americas to the west. As one component of the interconnected global ocean, it is connected in the north to the Arctic Ocean, to the Pacific Ocean in the southwest, the Indian Ocean in the southeast, and the Southern Ocean in the south (other definitions describe the Atlantic as extending southward to Antarctica).
Shutdown of thermohaline circulation
A shutdown or slowdown of the thermohaline circulation is an effect of global warming on a major ocean circulation. Data from NASA in 2010 suggested that the Atlantic Meridional Overturning Circulation (AMOC) has not slowed down, but may have actually sped up slightly since 1993. A 2015 study suggested that the AMOC has weakened by 15-20% in 200 years. Don Chambers from the University of South Florida College of Marine Science mentioned, "The major effect of a slowing AMOC is expected to be cooler winters and summers around the North Atlantic, and small regional increases in sea level on the North American coast."
Latitude of the Gulf Stream and the Gulf Stream north wall index
The Gulf Stream separates from the US coast near Cape Hatteras (35°N, 75°W) and then travels eastwards across the North Atlantic, becoming the North Atlantic current at about 55°W. In the region between 75°W and 55°W it is subject to meanders and is frequently accompanied by eddies. The northern edge of the current is marked by a sharp fall in temperature. This is also the case at much greater depths, so that the warm current is pressed up against a wall of cold water, called the ‘north wall’. Monthly charts of the path of the north wall of the Gulf Stream have been available from surface, aircraft and satellite observations since 1966 and these have been used in several studies of the path’s variability.