Virgin Islands National Park

TheVirgin Islands National Parkis anational park of the United Statespreserving about 60% of the land area ofSaint John, U.S. Virgin Islands, as well as more than 5,500 acres (2,226 ha; 9 sq mi) of adjacent ocean, and nearly all ofHassel Island, just off theCharlotte Amalie,Saint Thomasharbor.
The park is well known forscuba divingand snorkeling, and has miles of hiking trails through thetropical rainforest.
Cruz Bayis the gateway port to the park, as well as the visitor center location. Ferries operate hourly fromRed Hook, St. Thomas, thrice daily from Charlotte Amalie, St. Thomas and West End,Tortola, twice daily fromJost Van Dyke, and twice weekly fromVirgin Gorda.
Twocategory 5 hurricanesimpacted the Virgin Islands in September 2017,IrmaandMaria.The park received 112,287 visitors in 2018, after having received 304,408 visitors in 2017, and an average of more than 450,000 visitors per year in the preceding ten-year period from 2007 to 2016.The park was reopened in December 2017 with all roads, trails and beaches declared accessible to visitors.
As stated in the foundation document:
In 1956,Laurance Rockefeller'sJackson Hole Preservedonated its extensive lands on the island to the National Park Service, under the condition that the lands had to be protected from future development. The remaining portion, the Caneel Bay Resort, operates on a lease arrangement with the NPS, which owns the underlying land.
The boundaries of the Virgin Islands National Park include 75% of the island, but various in-holdings within the park boundary (e.g., Peter Bay, Maho Bay) reduce the park lands to 60% of the island acreage.
Much of the island's waters, coral reefs, and shoreline have been protected by being included in the national park. This protection was expanded in 2001, when theVirgin Islands Coral Reef National Monumentwas created.
In 2006,The Trust for Public Landpurchased the 415-acre (167.9 ha) Estate Maho Bay for preservation.The property includes beaches, undisturbed forest as well as historic Danish colonial andTaíno Indianartifacts.The trust intends to sell the property to theNational Park Serviceas federal funds become available.In 2011, the trust donated 18 acres at Mamey's Peak to the National Park Service.In 2012, the National Park Service purchased 58 acres from the trust for $2.25 million, using money from the federalLand and Water Conservation Fund.In 2013, an additional 72 acres of the Estate Maho Bay property was sold to the National Park Service for $2.5 million, the largest addition to the park.
HurricanesIrmaandMaria, bothcategory 5 hurricanes, impacted the Virgin Islands in September 2017.The park was reopened in December 2017 with all roads, trails and beaches declared accessible to visitors.The park received 112,287 visitors in 2018, after having received 304,408 visitors in 2017, and an average of more than 450,000 visitors per year in the preceding ten-year period from 2007 to 2016.
Beaches, coral reefs, hiking trails, and natural sites are the park's main attractions.
Visitors can stay in numerous resorts, hotels, and vacation villas near the park on St. John. Cinnamon Bay Campground is located inside the park, as isCaneel BayResort on the north shore which lies on Rockefeller's former personal estate. Overnight and day use mooring balls are available to boaters.
The beaches of Virgin Islands National Park are regularly named some of the best in the world.
Trunk Bay is a body of water and the adjacent beach onSaint John. Trunk Bay has an underwater trail for snorkeling along itscoral reef.The beach area is divided into two halves, the main Trunk Bay beach and swim area, and Burgesman Cove which is located on the west end of Trunk Bay near Jumbie Bay.
Cinnamon Baybeach is a long, wide stretch of sand on the north shore of St. John. The beach is popular for sunbathing, snorkeling, and water sports. The bay is also home to the Cinnamon Bay Campground and water sports rental.
HoneymoonBeach is on the north shore of St. John and can be accessed from Cruz Bay by hiking the 1 mile (1.6 km) long Lind Point Trail or from Caneel Bay Resort. The beach features soft white sand under tall palm trees. Kayaks and snorkel equipment are available for rent.
Maho Bay is known for its soft sand and calm, shallow waters. The sand and seagrass sea floor make it a good place to seesea turtlesandstingrays.
Located on St. John's south shore, Salt Pond Bay is a protected bay and beach. The beach can be reached by hiking a short trail from Route 107, about 4 miles (6.4 km) south of Coral Bay. The bay is a popular snorkeling spot and has fringing reefs on both sides of the bay, sea grass in the center, and a deep coral reef far out in the middle of the bay. Overnight and day use mooring balls are available for boaters. From Salt Pond Bay, hikers can access Drunk Bay and Ram Head Trail.
TheCinnamon BayNature Trail passes sugar plantation ruins, while theBordeaux MountainTrail leads to the highest point on the island at 1,277 feet (389 m) above sea level.
The Reef Bay Trail offers views of forests, remnants of sugar mills, historicalTaínopetroglyph rock carvings,a spring-fed waterfall and reflection pool, as well as snorkeling over the coral reef at Genti Bay. The hike is strenuous and the round trip from Centerline Road is more than 6 miles (9.7 km). A ranger-guided hike is offered, including a boat ride back to Cruz Bay from Reef Bay.
The Bordeaux Mountain Trail is a steep and rocky path leading from Little Lameshur Bay to the highest point of the island. The trail is unmaintained and although there are several overlooks along the way, there is no view from the top of this densely forested mountain. The trail gains almost 1,300 feet (396 m) in about 1 mile (1.6 km).
The 1 mile (1.6 km) long Lind Point Trail begins in Cruz Bay, behind the Virgin Islands National Park Visitor Center. The trail leads up to Lind Point, overlooking Cruz Bay harbor, before continuing on to Honeymoon Beach.
Starting in Cruz Bay, just north of Mongoose Junction, the Caneel Hill Trail leads up a steep incline to the top of Caneel Hill. A wooden observation platform is at the summit with views of St. John, St. Thomas, Jost Van Dyke, and many smaller islands. On a clear day, a hiker may see St. Croix and evenPuerto Rico.
Beginning at Salt Pond Bay, the Ram Head Trail travels about 1 mile (1.6 km) down a dry and rocky peninsula to the southernmost point on St. John.
Across from the entrance to Cinnamon Bay Campground, the Cinnamon Bay Nature Trail is a 0.5-mile (0.8 km) loop winding through the ruins of a sugar factory. Signs along the path explain the history of the area. The trail is a mixture of boardwalks and paved paths with no steep hills.
The park protects dozens of historic ruins from the colonial and plantation eras through the 1950s.
TheAnnaberg Historic Districtprotects a partially restored sugar factory and windmill located just east of Mary's Point. National park signage guides visitors through the ruins and explains the process of turning sugar cane into molasses. Volunteers and park rangers are frequently in the area to answer questions. The bake house hosts cooking demonstrations and offers samples ofdumb bread. The windmill is located on Annaberg Point, which offers views of Tortola, Great Thatch Island, and the Narrows.
The ruins of theReef Bay Sugar Factory Historic Districtcan be reached via Reef Bay Trail or L'Esperance trail.
TheReef Bay Trail petroglyphsareTaínorock carvings located on rock pools near a waterfall. They can be reached via a 0.25-mile (0.4 km) long spur trail from Reef Bay Trail. The petroglyph site was added to theNational Register of Historic Placesin 1982.
The well-preservedCatherineberg Sugar Mill Ruinsare among the most easily accessed in the park, and include a windmill tower and ahorse mill.
Virgin Islands National Park encompasses 14,737 acres (5,964 ha; 23 sq mi) of land and ocean. The park covers almost 60 percent of St. John Island, adjacent ocean, and almost all of Hassel Island.
The main features are coral reefs, which almost completely surround the park, and the ocean waters, tropical forests and beaches.
Wild donkeys, deer, mongoose, pigs, goats,birds, iguanas, skinks, tortoises, frogs,fish, and crabs inhabit the park. Bats are the only native land mammal in the park.
The park has been recognised as anImportant Bird Area(IBA) byBirdLife Internationalbecause it supports populations ofbridled quail-doves,green-throated caribs,Antillean crested hummingbirds,brown pelicans,Caribbean elaenias,Puerto Rican flycatchers,pearly-eyed thrashersandLesser Antillean bullfinches.
According to theKöppen climate classificationsystem, Virgin Islands National Park has a tropical savanna wet and dry climate (Aw). ClassAtropical climateshave an average temperature of 18 °C (64.4 °F) or higher in every month of the year, with significant annual precipitation. ClassAwclimates have a pronounced dry season, with the driest month having precipitation less than 60 mm (2.36 in) and less than 1/25 of the total annual precipitation.
The average rainfall per year is 55 inches (1,400 mm). In the winter, trade winds blow from 11 knots (13 mph; 20 km/h) to 21 knots (24 mph; 39 km/h). The average temperature for the park is 79 °F (26 °C).
The park experiences very little temperature variation between summer and winter, while the sea is warm year-round. The main tourist season is from December to April, which are the driest months. During the remaining months (i.e., theAtlantic hurricane season), prices for accommodations are reduced considerably. Camping and rustic lodging are available in the park from November through August at Cinnamon Bay Campground. Caneel Bay Resort provides luxury accommodations along with upscale dining in the park from November through July.
Located at the east end of theGreater Antilles, St. John resides on the northeastern end of theCaribbean Plate. The island formed during theCretaceouswith the eruption of the Water IslandFormation, consisting ofkeratophyresandpillow basalts. Igneous activity then changed to that of anisland arc, characterized by the Louisenhoj Formation, consisting ofandesiteand basalt. Volcanism abated during the deposition of the Outer BrassLimestone. Volcanism resumed as evidenced by the Late Cretaceous Tutu Formation, consisting ofvolcaniclasticturbidites, basalt, and andesite. Adiabasedike swarmfollowed and then compressivefoldingattributed to the Caribbean Plate colliding with theBahama Platform. The LateEocenesaw the intrusion of Narrowsplutonand Virgin Gordabatholith, associated with the Greater Antillesarcmagmatism, and more compressive folding associated with the spreading of theCayman Trough. This spreading is also tied tosinistralstrike-slipfaulting at 39Ma.