The archipelago is located in the northern hemisphere within the Atlantic Ocean and extends along a west-northwest to east-southeast orientation (between 36.5°–40° North
latitudes and 24.5°–31.5° West
longitudes) in an area approximately wide. The islands of the Azores emerged from the
Azores Plateau, a 5.8 million km2 region that is morphologically accented by a depth of . (green) and the
Canary Islands (yellow) in the northern Atlantic The nine islands that compose the archipelago occupy a surface area of , that includes both the main islands and many islets located in their vicinities. They range in surface area from the largest, São Miguel, at to the smallest, Corvo, at approximately . São Jorge, Pico and Faial are collectively called ('Islands of the Triangle'). Each of the islands has its own distinct geomorphological characteristics that make them unique: • Corvo is a crater of a major
Plinian eruption • Flores (its neighbor on the
North American plate) is a rugged island carved by many valleys and escarpments • Faial is characterized for its
shield volcano and
caldera (
Caldeira Volcano) •
Pico has the highest point, at , in the Azores and Portugal • Graciosa is known for its active Furnas do Enxofre and mixture of
volcanic cones and plains • São Jorge is a long slender island, formed from
fissural eruptions over thousands of years • Terceira, almost circular, contains one of the largest craters in the region • São Miguel is pitted with many large craters and fields of spatter cones • Santa Maria – the oldest island – is heavily eroded, being one of the few places to encounter brown sandy beaches in the archipelago. , located within the
Sete Cidades Massif, in
Sete Cidades,
São Miguel Island. The islands can be divided into three recognizable groups located on the Azores Plateau: • The
Eastern Group () of São Miguel, Santa Maria and Formigas Islets • The
Central Group () of Terceira, Graciosa, São Jorge, Pico and Faial • The
Western Group () of Flores and Corvo. Several sub-surface reefs (particularly the
Dollabarat on the fringe of the Formigas), banks (specifically the
Princess Alice Bank and
D. João de Castro Bank), as well as many
hydrothermal vents and sea-mounts are monitored by the regional authorities, owing to the complex geotectonic and socioeconomic significance within the economic exclusion zone of the archipelago.
Geology , the highest mountain in Portugal, displays the remnants of its last major eruption on its northern flank From a geostructural perspective, the Azores are located above
an active triple junction between three of the world's major tectonic plates (the
North American plate, the
Eurasian plate and the
African plate), The Western Group is located on the North American plate, while the remaining islands are located within the boundary that divides the Eurasian and African plates. The principal tectonic structures that exist in the region include the
Mid-Atlantic Ridge, the
Terceira Rift, the Azores Fracture Zone and the Glória Fault.
Mountains Volcanoes The islands' volcanism is associated with the
rifting along the Azores triple junction; the spread of the crust along the existing faults and fractures has produced many of the active volcanic and seismic events, while supported by buoyant upwelling in the deeper mantle, some associate with an
Azores hotspot. Most of the volcanic activity has centered primarily along the Terceira Rift. volcanic cave on Terceira Island The islands have many examples of volcano-built geomorphology including caves and
lava tubes (such as the
Gruta das Torres,
Algar do Carvão,
Gruta do Natal, Gruta das Cinco Ribeiras), the coastal lava fields (like the coast of
Feteiras, Faial, the Mistério of
Prainha or São João on Pico Island) in addition to the inactive cones in central São Miguel, the aforementioned Capelinhos on Faial, the volcanic complexes of Terceira or
Plinian caldeira of Corvo Island. The islands of the archipelago were formed through volcanic and seismic activity during the
Neogene Period; the first embryonic surfaces started to appear in the waters of Santa Maria during the
Miocene epoch (from circa 8 million years ago). The sequence of the island formation has been generally characterized as: Santa Maria (8.12 Ma), São Miguel (4.1 Ma), Terceira (3.52 Ma), Graciosa (2.5 Ma), Flores (2.16 Ma), Faial (0.7 Ma), São Jorge (0.55 Ma), Corvo (0.7 Ma) and Pico (0.27 Ma). All islands have experienced volcanism during their geological history, with Late
Holocene volcanism being recorded from Flores and Faial. Within recorded "human settlement" history Santa Maria, Graciosa, Flores, and Corvo have not experienced any volcanic eruptions; in addition to active fumaroles and hot-springs, the remaining islands have had sporadic eruptions since the 14th century. Apart from the Capelinhos volcano in 1957–1958, the last recorded instance of "island formation" occurred off the coast of São Miguel, when the island of
Sabrina was briefly formed.
Earthquakes Owing to its geodynamic environment, the region has been a center of intense seismic activity, particularly along its tectonic boundaries on the Mid-Atlantic Ridge and Terceira Rift. Seismic events although frequent, are usually tectonic or vulco-tectonic in nature but in general are of low to medium intensities, occasionally punctuated by events of
magnitude 5 or greater. The most severe earthquake was registered in 1757, near
Calheta, which exceeded magnitude 7. In comparison, the 1522 earthquake that was mentioned by historian
Gaspar Frutuoso measured 6.8, but its effects were judged to be X (
Extreme) on the
Mercalli intensity scale, and was responsible for the destruction of Vila Franca do Campo and landslides that may have killed more than 5,000 of the inhabitants.
Biodiversity The archipelago lies in the
Palearctic realm and has a unique biotic community that includes the
Macaronesian
subtropical laurissilva, with many
endemic species of plants and animals. There are at least 6,112 terrestrial species, of which about 411 are
endemic. The majority (75%) of these endemics are animals, mostly
arthropods and
mollusks. New species are found regularly in the Azores (e.g., 30 different new species of land snails were discovered circa 2013). of São Jorge can be seen by the
hydrangeas (blue markings) and
Pittosporum undulatum (centre-right) Even though the Azores look very green and sometimes wild, the vegetation has been extremely altered. A great part of it has been wiped out in the past 600 years for its valuable wood (for tools, buildings, boats, fire wood, and so on) and to clear land for agriculture. As a result, it is estimated that more than half of insects on Graciosa have disappeared or will become extinct. Many cultivated places (which are traditionally dedicated to pasture or to growing
taro, potatoes, maize and other crops) have been abandoned, especially as a result of emigration. Consequently, some invasive plants have filled these deserted and disturbed lands.
Hydrangeas are another potential pest, but their threat is less serious. Hydrangeas were introduced from America or Asia, but some locals consider them a symbol of the archipelago and propagate them along roadsides.
Cryptomeria, the Japanese cedar, is a
conifer extensively grown for its timber. The two most common of these alien species are
Pittosporum undulatum and
Hedychium gardnerianum. Reforestation efforts with native laurissilva vegetation have been accomplished successfully in many parts of the Azores. There are at least three endemic living bird species. The
Azores bullfinch, or
Priolo, is restricted to remnant laurisilva forest in the mountains at the eastern end of São Miguel and is classified by BirdLife International as
endangered.
Monteiro's storm petrel, described to science as recently as 2008, is known to breed in just two locations in the islands but may occur more widely. The
Azores chaffinch, formerly considered a subspecies of the
common chaffinch, is an abundant and conspicuous resident on all the islands. An extinct species of owl, the
São Miguel scops owl, has recently been described, which probably became extinct after human settlement because of habitat destruction and the introduction of alien species. Five species of flightless
rail (
Rallus spp.) once existed on the islands, as did a flightless quail (
Coturnix sp.), a species of
gadfly petrel Pterodroma zinorum, and another species of bullfinch, the
greater Azores bullfinch, but these also went extinct after human colonization. Eleven subspecies of bird are endemic. The Azores has an endemic bat, the
Azores noctule, which has an unusually high frequency of diurnal flight. on São Miguel Island The islets of the Formigas (the Portuguese word for "ants"), including the area known as the
Dollabarat Reef, have a rich environment of maritime species, such as
black coral and
manta rays, different species of sharks, whales, and sea turtles. Seventeen marine reserves (with special conservation status) were added to the Azorean Marine Park (which covers around ). On São Miguel there are notable micro-habitats formed by hot springs that host
extremophile microorganisms.
Climate conditions over the eastern and central groups; in this photo taken on June 17, 2013. The archipelago is spread out at roughly the same latitude as the southern half of mainland Portugal, but its location in the mid-Atlantic Ocean gives it a generally tepid,
oceanic, mild to warm
subtropical climate, with mild annual oscillations.
'Azores High' anticyclone The Azores archipelago is located in a transition and confrontation zone between air masses of tropical origin and masses of cooler air of polar origin. The climate is largely determined by variations in the atmospheric pressure field over the North Atlantic. These variations, conditioned by the mass of the American continent and the Atlantic water mass, are overlapped by a semi-permanent subtropical Atlantic
anticyclone, commonly known as the
Azores High. This anticyclone experiences seasonal variations which can affect the archipelago in many ways. In winter, the Azores High is positioned further south and allows for a descent of the
Polar front, approaching it to the archipelago. In summer, the anticyclone's movement further north leads to the departure towards higher latitudes of the polar front and its associated disturbances. Far enough away from the mainland coasts, the continental air masses that reach the archipelago are weakened by the maritime influence. The same cannot be said for the higher altitudes (e.g. Mount Pico), where upper air masses of continental origin and with a more direct pathway can reach the surface and present those areas with drier air and more extreme temperatures. At the same time, this free atmosphere circulating air transports
aerosols to the archipelago, namely volcanic ash or fine sands from the
Sahara desert, which sporadically affect the radiation and air quality.
Köppen classification Under the
Köppen climate classification, the Eastern Group is usually classified as
Mediterranean while the Central and Western Groups (especially
Flores and
Corvo) are more
humid subtropical and overall rainier because of the effects of the
Gulf Stream. This stream has a large effect over the sea temperature which varies between in February and March, and in August and September, and increases earlier in the Western Group.
Salvador Rivas-Martínez's data presents several different bioclimatic zones for the Azores.
Seasonal lag is extreme in the low-sun half of the year, with December being milder than April in terms of mean temperatures. During summer the lag is somewhat lower, with August being the warmest month, though September is usually as warm or warmer than July.
Temperatures, humidity, and sunshine Although temperatures as warm as have been recorded on Pico, neither Ponta Delgada nor Angra do Heroísmo have ever been warmer than . No snowfall or temperatures below have been recorded at sea level on any of the islands. The coldest weather in winter usually comes from northwesterly
air masses originating from eastern Canada. However, since those air masses are warmed up as they pass across the warmer Atlantic Ocean, temperatures by day even then exceed . The average relative humidity can range from 80% at the coast to over 90% above . However, higher elevations above the
planetary boundary layer can experience extremely low values close to 10%.
Insolation is relatively low, with 35–40% of the total possible value for sunshine, and higher in topographically lower islands such as Graciosa or Santa Maria, inversely proportional to precipitation. This is directly caused by the
orographic lift of humid air masses and is especially pronounced in islands marked by high
orography.
Hurricanes Despite the northern position that the archipelago occupies, the Azores can be affected by the passage of
tropical cyclones, or tropical storms derived from them. Some can result from anomalies of low latitude systems, while others result from the return to the Atlantic after a route close to or even over the American continent. Though often small and in the process of dissipation, these cyclones result in many of the worst storms the archipelago is subject to. A total of 14
tropical or
subtropical cyclones have affected the region in history. Most of them were either
extratropical or
tropical storms when they affected the region, although several
Category 1 hurricanes have reached the Azores. The following storms have impacted the region while at Category 1 strength: •
Hurricane Fran in 1973 •
Hurricane Emmy in 1976 •
Hurricane Gordon in 2006 •
Hurricane Gordon in 2012 •
Hurricane Alex in 2016 Several tropical or subtropical storms have hit the region, including: •
Tropical Storm Irma in 1978 •
Hurricane Bonnie in 1992 •
Hurricane Charley in 1992 •
Hurricane Erika in 1997 •
Unnamed subtropical cyclone in 2005 •
Hurricane Gaston in 2016 •
Tropical Storm Gaston in 2022 •
Subtropical Storm Patty in 2024 •
Hurricane Gabrielle in 2025 Storms that were extratropical when they impacted the region include: •
Hurricane Tanya in 1995 •
Tropical Storm Ana in 2003 •
Tropical Storm Grace in 2009 == Economy ==