What is it Like to Live in Puerto Vallarta?

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The weather, cost of living and culture are just some of the questions that many people ask when considering moving to a new city. To answer this question, we’ve compiled information about living in Puerto Vallarta from real people who have lived here for a few months. Read on to learn more. You can also ask locals for tips and advice on how to make the most of your time in Puerto Vallarta.

Cost of living

The cost of living in Puerto Vallarta can be expensive, but it is not impossible to find affordable apartments. In fact, many residents enjoy life to the fullest here, and the average rent for a two-bedroom house is $650 USD. That price can be doubled, depending on the area, if you live in a popular part of town. And if you have a terrace or ocean view, you can further increase your rent!

While Puerto Vallarta doesn’t have the same high-end restaurants as nearby San Diego and San Francisco, it does have a great number of good, affordable restaurants at a range of price points. However, eating at restaurants within the city center or at touristy spots will cost you a bit more. Luckily, many Mexican supermarkets and international chains are nearby, and if you do have to shop, local mercados are a great way to stock up on fresh fruit and vegetables.

In addition to groceries, rent in Puerto Vallarta is relatively expensive. Expect to pay at least $300 USD per month for a one-bedroom apartment. If you plan on eating at restaurants and frequent the beach clubs, double the budget. Similarly, utilities and internet services are affordable. An eighty-five-square-foot condominium building will rent you a one-bedroom apartment for about $400 USD per month, while a one-bedroom apartment in a gated community may cost $1,500.

When calculating the cost of living in Puerto Vallarta, keep in mind that the exchange rate between the U.S. dollar and the Peso will influence the cost of living. However, the cost of living is still significantly lower than that in metropolitan areas in the U.S., especially if you’re coming from the Midwest or central parts of the U.S. However, prices for everyday expenses are the real standout.

The cost of living in Puerto Vallarta depends on what you’re doing and where you’re staying. In the winter months, the beach is the hub of activity. There are umbrellas and loungers for rent, waiters for drinks, and even parasailing. There are many things to do on the beach, from brunches to dancing. The expat community is active, hosting fundraisers and volunteering. The cost of living in Puerto Vallarta is relatively low for two people.

The weather in Puerto Vallarta is tropical. Highs rarely exceed 90 degrees Fahrenheit and lows rarely drop below 70. There are frequent dramatic rains, which help to regulate the humidity, but if you don’t have air conditioning, you’ll sweat more than you’d normally. But the weather in Puerto Vallarta is protected by the mountains and bay, so the city’s streets are rarely affected by rain, which helps keep the humidity at a manageable level.


If you are planning a vacation to Puerto Vallarta, Mexico, you should know that its weather is quite different from that of the country’s other beach towns. In fact, Puerto Vallarta has much better winter weather than other beach towns in Mexico, and you won’t have to worry about extreme temperatures and humidity. The best time to visit is December to May, when average high temperatures are around 30 degrees Celsius, and evening temperatures are in the low teens. The temperature of the sea is also cooler during winter, with the average temperature in the mid-20s. As Vallarta sits on the edge of a rainforest, rainfall is not a problem during winter months. The rainiest months are July to September, when temperatures can reach the mid-sixties.

The cool season lasts for about 3.8 months. The average temperature is 78 degrees Fahrenheit in June and July, with the lowest temperature in December falling to just below 20 degrees. Despite the high temperatures, December is not too wet and is often sunny. High temperatures in December are in the low 30s and can climb to 40 degrees. Nights are also warm, but rain in Puerto Vallarta can be refreshing. The city receives about 13 inches of rain per month in July and fifteen inches in September.

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The temperature in the winter is usually milder than summer, with the lowest averages occurring in February and July. Temperatures are moderately warm in May, but there are some days when the mercury reaches as high as 106 degrees. If you want to go surfing or swim, you should consider visiting in November. These are the best months to visit Puerto Vallarta because you can catch some good waves there. Just make sure you pack the right clothing in these months.

The rainy season in Puerto Vallarta is from late June to mid-October. Rainstorms will cause cloudy skies during the day but will last only an hour. Cloudy days are possible throughout the rainy season, but the rainfall is rare and only occurs on partly cloudy days. If you want to see the current weather in Puerto Vallarta, you can watch the weather online via a webcam. The webcams will let you know what the weather is like in real time.

The temperatures in Puerto Vallarta fluctuate a lot. The average temperature is around sixty-three degrees Fahrenheit. It rarely drops below forty-three degrees in winter, and it rarely dips below fifty-six degrees during summer. During the winter, the temperature may drop to as low as thirteen degrees during the day. In August, it’s hottest, while February is the coolest month. While summer months are ideal for swimming, winter months are also suitable for beach vacations and outdoor activities.


While in Puerto Vallarta, you should spend time exploring the culture and arts scene. There are many things to do and see. For example, you can take a tour of the ChocoMuseo. The museum features the works of 50 local artists. Visitors can buy art pieces or join a chocolate workshop. A tour is free and you can choose from an array of different art forms. If you’re a foodie, you can check out the local restaurants to sample local delicacies.

The tourism industry has risen steadily throughout the years. Today, it accounts for 50% of the local economy. International tourism to Puerto Vallarta is particularly high in the winter months, from late November to March, though this season can extend into April, depending on the timing of college spring break periods in the U.S. Despite its popularity, Puerto Vallarta remains a popular destination for tourists from the western U.S. and Canada.

As tourism in Puerto Vallarta has grown, so have the local arts scene and culture. The city was once home to a thriving fishing industry and is now known for its vibrant nightlife. In the early 1980s, the area’s poverty levels increased as the peso devalued. The devaluation boosted tourism, but at the same time, it stunted construction and investment. The result was a decline in infrastructure.

There are numerous opportunities for education and furthering one’s career. Puerto Vallarta has a campus of the University of Guadalajara, and a variety of lesser-known institutions. You can also attend high school and even college here. And if you’re looking for an animal sanctuary, you can also visit the Puerto Vallarta Zoo, where you can see some 350 species of wildlife. Or, try Huachinango zarandeado, a marinated red snapper in birria paste and garlic.

Whether you’re an art lover or simply love street art, Puerto Vallarta has something to offer you. There are galleries and art studios downtown that feature local and regional artists. If you’re looking for a piece of culture that’s unique to Puerto Vallarta, a street mural tour may be the perfect option. If you’re an amateur, you can also take a guided tour with a local artist to get a deeper appreciation of the artwork.

Another popular attraction is the Santo Domingo church. The church is the most photographed building in the city. Its spired structure is topped with bronze statues that represent the 4 cardinal points and the sun. The cathedral’s crown was re-sculpted by Carlos Terre, a native of Jalisco. Its name, Tecuntlanopeuh, means «originating at Las Penas.» The city was called Las Penas until 1918.

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What is the Continental Shelf? A continental shelf is a section of the sea floor that typically extends from the coast to a depth of 100-200 metres (330-660 feet). The shelf is gently inclined toward the sea, with an average slope of 0.1deg. At the end of the shelf, a steep drop called the shelf break separates the shelf from the continental slope, a steeper section of the sea floor that merges with a part of the ocean floor known as the continental rise.

Coastal countries have exclusive rights to claim a portion of the continental shelf

The LOSC is a UN treaty that establishes sovereign rights to parts of the ocean that are beyond the coastal state’s exclusive economic zone (EEZ). These rights are not always economically ascertainable, and some may be suspect of being there. These resources can be important sources of power or global strategic interests. Although the area has decreased from 70 percent of the sea floor to only 43 percent, the sea bed is still considered a common heritage of mankind.

Under the convention, coastal states may establish their continental shelves beyond the 200 nautical mile limit as long as the outer boundary follows precise topography or geological continuity. To claim an additional portion of the continental shelf, a coastal state may use an offshore island as a baseline. This baseline is crucial for countries seeking to extend their continental shelf, as it could lead to overlap between claims from different states. Coastal states may claim islands, but this would mean divergent territorial views.

The Paris Treaty has affirmed Norway’s sovereignty over Svalbard. It also confirms Norway’s sovereignty over its own territory and parts of its continental shelf. However, the Svalbard Treaty does not explicitly mention the continental shelf. However, it does confirm that Norway has sovereignty over its land and its territorial waters, but does not address whether it has exclusive rights to claim a portion of the shelf.

Fish species thrive in and around continental shelves

The vast expanses of ocean water surrounding the continental shelves support complex and productive marine ecosystems. They are economically and culturally important, exhibiting high nutrient availability due to freshwater inputs and upwelling. The water above the shelves is shallow, promoting primary production and allowing light to penetrate the substrate. In this way, many marine species thrive on these shelves. However, there are some risks to their survival.

Because shelf areas differ considerably, species may experience range shifts, resulting in greater abundance or reduced range size. Species may also shift their distributions into deeper waters or higher latitudes. Because shelf areas are not uniform across the oceans, changes in their availability will be highly regional. This is consistent with the pattern observed in studies of projected sea level rise. The distribution of shelf area is influenced by regional bathymetry, which is important for understanding the extent of shelf changes.

Coastal oceans are rich in diverse species of fish. Phytoplankton, a type of algae, feeds off sediment nutrients, making it the primary source of food for many fish species. In fact, phytoplankton is a primary source of nutrition for most animal species, including many fish species. Algae thrives in the rockier areas of continental shelves, providing food for marine life.


Scientists have discovered new cracks in the ocean floor just off the Eastern coast of the United States, which could trigger a massive tsunami, bringing 18-foot waves to the mid-Atlantic coast. Three researchers have found fissures off Virginia and North Carolina, putting lower Chesapeake Bay at risk of wave heights similar to category 4 hurricanes. According to the National Ice Center, the last time the Conger shelf fractured was in 1865.

The internal structure of both segments is similar, with a top Messinian M horizon defined as the type 1 sequence boundary. The shelf marginal wedge, on the other hand, has onlapping parasequences and a downlapping system tract. The shelf marginal wedge completes the cycle of sea level changes. The Damur canyons, for example, cut through the continental shelf. Large submarine slides, most likely triggered by large earthquakes, may also have contributed to the destabilization.

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The ice shelf in South Wales is being impacted by a fast-melting formation that has become a symbol of climate change. A flurry of icebergs calving from Thwaites Glacier could shatter part of the eastern ice shelf in just five years. It could also funnel land-based ice into the sea, contributing to sea-level rise. If this were to occur, scientists hope that the glaciers in the region will collapse.


Submarine canyons on the continental shelf begin at ocean depths of about a metre to more than three hundred metres and extend hundreds of kilometers across the shelf. These canyons may be very ancient, originating as rivers in the Neoproterozoic, and are characterized by the presence of turbidites at the ends of the canyon and at its mouth. Canyons on the continental shelf are primarily found in deep ocean, with some originating far offshore.

In the North Atlantic and Pacific Oceans, the vast majority of canyons are land-attached, whereas only about ten percent are detached. These canyons contain 45-55% more potential for hydrodynamic processes, including internal tides and currents. This is likely related to the seasonal variations of cross-shelf transport, as sediments are favored toward the canyon during the summer months. This is not to suggest that there are no canyons on the continental shelf, but it is likely that the existence of these structures is a good indicator for future research.

Submarine canyons are formed in the seabed near the coast of New England, and are an example of a deep-seated geological feature that forms underwater. They are created as a result of abrupt changes in sea level and contain traces of ancient shorelines. The shelf is formed by the inundation of continental margins by the world ocean during the last glacial period, as well as by recent tectonic subsidences of the earth’s surface.


Seawater 400 meters deep is three to four degrees Celsius warmer than nearby waters. Sea floor bathymetry determines the extent of this warm subsurface layer and whether it reaches fjords. This warm subsurface layer can also cause glaciers to melt. Researchers from the Ocean Measurement Group (OMG) have mapped these undersea canyons using an echo sounder aboard the research vessel M/V Cape Race. They have been using the echo sounder to navigate up narrow fjords on the continental shelf around Greenland. They were able to pinpoint locations where warmer Atlantic Ocean water meets bottoms of 0-degree glaciers.

Typical fjords are located on high latitude coastal areas, partly landlocked and surrounded by deep basins. A typical fjord has steep sides and considerable depth. The water in a fjord is often several times deeper than the surrounding continental shelf. As a result, fjords are among the deepest estuaries. And as the learning algorithm improves, new fjords may be found along the continental shelf.

Studies have mainly focused on the hydrographic conditions of fjords on the coastal shelf, although a few have focused on coastal fjords in conjunction with marine-terminating glaciers. Mortensen et al., for example, have focused on the hydrographic differences between inner and outer fjords, the hydrographic conditions between coastal and inner fjords, and the pan-shelf distribution of water masses. However, the authors focus on the interplay between these water masses and on links to proglacial fjords.

Seafloor slope

The sea slope of the continental shelf is the average slope of the sea floor, but it can vary considerably. It can range from one to twenty degrees, with the steepest slopes being found in the Pacific Ocean and the lowest in the Atlantic and Indian Oceans. Because of the steep sides of the continental slope, sedimentary materials that are carried to the seafloor do not remain on the slope, but flow downward into the next region.

The slope is steeper off stable coasts without major rivers and is lowest on the narrow continental shelves. Slopes are steeper in the Pacific and Atlantic Oceans, with Indian Ocean slopes being the flattest. Half of the continental slopes descend into deep sea trenches, while the other half end in shallow depressions or fan-like continent-wide rises. The transition from continental crust to oceanic crust typically occurs below the continental slope.

Submarine canyons are also common along the sea slope. These are submerged landslides that carry sediment and water deep into the ocean basin. Although many scientists have speculated about the formation of submarine canyons, most agree that the sediments formed by erosion, gravitational forces, or river valleys are responsible for their formation. These geological features are found all around the world, and may be an important source of information about the ocean’s geological history.

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