T&C Surf Designs’ Kalo Collection to benefit Boys & Girls Club of Hawaiʻi

On Kauaʻi, the Boys & Girls Club of Hawaiʻi operates four program locations, with a new teen center planned at the former Garden Island newspaper building in Līhuʻe.

The free meals are helping many of the 80% of community college students on Kauaʻi who are dealing with damaged homes, lost income and/or prolonged power outages due to Hurricane Lowell.

Direct2UH removes traditional application barriers by providing eligible seniors direct admission to one or more UH campuses based on their grade point average, with no application fee.

“In my opinion, diversity of representation in the legal profession is required for access to and actual achievement of justice.” — Hawaiʻi Supreme Court Justice Sabrina S. McKenna

Native Hawaiian nonprofits are working to update state’s historic preservation program administrative rules to involve lineal and cultural descendants in decisions regarding iwi kūpuna.

Nāmaka has overcome challenges including internal theft to provide diners with a tropical ambiance and locally inspired gourmet cuisine.

Direct2UH removes traditional application barriers by providing eligible seniors direct admission to one or more UH campuses based on their grade point average, with no application fee.

“In my opinion, diversity of representation in the legal profession is required for access to and actual achievement of justice.” — Hawaiʻi Supreme Court Justice Sabrina S. McKenna

Native Hawaiian nonprofits are working to update state’s historic preservation program administrative rules to involve lineal and cultural descendants in decisions regarding iwi kūpuna.

The Coffee and Cacao Innovation Lab will work with small farmers in Hawaiʻi and the continental United States, as well as in Latin America, Africa and Asia.

Here is up-to-date information about recovery efforts and resources from Hurricane Lowell.

The combination of deformation and geochemical datasets show the new fissure vents were the same magma source we have seen in previous fountaining episodes at the summit of the Big Island volcano and likely formed because the magma system was highly pressurized and simply forced its way along the easiest path to the surface.