War in the Pacific National Historical Park invited the Junior Rangers to return to Asan Bay Overlook for a special volunteer project on November 22, 2014. In preparation for the unveiling ceremony of the brand new panels at Asan Bay Overlook, the Junior Rangers will serve as special stewards by beautifying the site. As Junior Rangers, they are representatives of the park and are important youth leaders in preserving the island’s significant historical monuments.
Found throughout the Indo-Pacific, the crown of thorns starfish, Acanthaster planci, is one of the largest sea stars in the world (up to 45 cm across). Unlike the typical starfish with five arms, the crown of thorns starfish is disc-shaped with multiple arms (up to 21) covered in poisonous spines. These unique features gave rise to this starfish’s commonly referred to name of the crown of thorns.
Acanthaster planci is a corallivore, which means that it feeds on live coral tissue. After climbing on a coral colony, the crown of thorns starfish extrudes its stomach out through its mouth and spreads it over the surface of the corals. The stomach secretes digestive enzymes that liquefy the coral tissue which is then absorbed.
For the rest of the story visit: Crown of Thorns Starfish Wreak Havoc in American Samoa — The NPS Responds
This Tuesday, our friends from National Parks Conservation Association explored the National Park of American Samoa.
Park Ranger Pua met up with them here at our visitor center to learn about the natural resources we protect and preserves through the interpretive exhibits displayed. They also experienced Samoan dancing and singing by some of the park staff and crews.
Park Ranger Pua gave them a taste of our national park as he welcomed them with a warm gesture of hospitality by serving them an all-natural, refreshing and healthy snacks woven in coconut fronds called “mailo”.
For more photo adventures of the group, check us on Facebook!
The National Parks Conservation Association (NPCA) is the only independent, membership organization devoted exclusively to advocacy on behalf of the National Parks System. Its mission is “to protect and enhance America’s National Park System for present and future generations.”
The following is this week’s edition of “Volcano Watch” from the USGS Hawaiian Volcano Observatory:
With the June 27th lava flow entering Pāhoa this past week, the USGS Hawaiian Volcano Observatory (HVO) and Hawaiʻi County Civil Defense have been providing updates to the media and the public each day. This short-term information is useful to gauge the immediate hazards that the flow might pose to nearby residences and infrastructure. But recently, a frequent inquiry has been, “When will this end?” To answer this question, we should first consider the June 27th flow as a whole and examine it over a longer time frame.
Whenever HVO geologists are asked about when the flow will stop, we remind people that the Puʻu ʻŌʻō eruption—Kīlauea Volcano’s ongoing East Rift Zone eruption and the source of the June 27th lava flow—has been going on for over 31 years. This sustained time period suggests that Puʻu ʻŌʻō could continue to erupt for years to come.
But how long the Puʻu ʻŌʻō eruption persists is only part of the story. For most of its 31 years, the eruption has sent lava flows south, towards the ocean. In recent years, these flows created only minor risks, because much of the area south of Puʻu ʻŌʻō was already covered by a broad lava flow field. The June 27th flow is unusual (but not unprecedented) in that the flow direction is towards the northeast.
What caused this shift in flow direction and change in hazard? The short answer is vent location.
The Puʻu ʻŌʻō eruption began in 1983 and has continued essentially nonstop ever since, but the vent location (the spot where lava comes out of the ground) has shifted many times. A vent can create its own lava flow field that covers areas downslope, and a given vent can remain active for days to several years before it shuts down.
Recent flows (those erupted 2013 to present), such as the Kahaualeʻa flows and the June 27th flow, have been directed towards the northeast, because their vents opened on the northeast part of the Puʻu ʻŌʻō cone. Because these vent locations are slightly north of the pre-2013 vents, lava has not been able to flow south of the East Rift Zone ridgeline. Instead, the East Rift Zone, with its older lava shields, lava ponds, and ground cracks, helped contain these more recent flows north of the ridgeline—sending them to the northeast.
There is no way of knowing how long the June 27th vent will persist, but for guidance, we can look at the duration of other recent vents on Kīlauea. The Kahaualeʻa and Kahaualeʻa 2 vents (2013–2014) lasted for 2.5 months and 13 months, respectively. The Peace Day vent (2011–2013) erupted for about two years. The Fissure D vent (2007–2011) lasted for nearly four years. This indicates that individual vents on Puʻu ʻŌʻō have the potential to remain active for several years.
If the June 27th vent remains active for several years, its lava flow activity will likely follow the same pattern exhibited by other recent vents and their flow fields. Routine fluctuations in lava supply to the pāhoehoe flow field will trigger new breakouts from the lava tube, which will slowly widen the flow. What begins as a narrow pioneer flow can gradually, over the course of months, widen with the addition of breakouts into a more expansive lava flow field. This lateral enlargement of the flow field can be the most destructive aspect of the activity.
So, how long will the June 27th lava flow last? All we can say with certainty is that, based on other recent activity, it has the potential to persist for months to years. But we cannot precisely forecast the flow’s duration. Should an abrupt change occur at Puʻu ʻŌʻō, the June 27th vent and its flow could end any day. Currently, there are signs that the eruption rate is varying but no signs that the vent is shutting down. We should be prepared for the flow to remain active for some time.
Puna residents are encouraged to stay informed about the June 27th lava flow’s status and progress through daily updates posted on HVO and Hawaiʻi County Civil Defense websites (http://hvo.wr.usgs.gov and http://www.hawaiicounty.gov/active-alerts/). You can also sign up to receive Volcano Activity Notices, distributed via the USGS Volcano Notification Service, at http://volcanoes.usgs.gov/vns/.
While working in the freshwater streams at Kalaupapa National Historical Park to collect data on the fish, shrimp, and snails, we ran into a virtual ‘o’opu city. There are two species of native ‘o’opu (gobies) in this video clip. They are ‘o’opu ‘alamo’o and ‘o’opu nōpili. Can you tell the difference? Can you tell the males from the females? The poster below can help you in your efforts.
Watch out for the invasive Tahitian prawns. The ‘o’opu definitely do.
Today, the National Park of American Samoa celebrates 26 years of preserving and protecting our islands majestic coral reefs, lush tropical rain forests, fruit bats as vital pollinators, and the rich Samoan culture.
Come celebrate with us as we continue to bring valued service to our community. Drop us a birthday greeting on our Facebook page. :)