As part of the USGS Coral Reef Project, the USGS is working on the Kona (west) coast of Hawaiʻi to evaluate geologic resources at two historical parks.
Overview
The island of Hawaiʻi, known as the Big Island, is the largest in the Hawaiian Islands chain. Greater than twice the area of the remaining main eight Hawaiian Islands combined, Hawaiʻi encompasses 10,432 sq km (4,028 sq mi). The island was formed from five major volcanoes. The volcano of Mauna Kea is the tallest mountain on Earth, reaching nearly 9 km (5.5 mi) from the seafloor to the summit. Although shorter, Mauna Loa's massive size makes it the largest volcano in the world. Kīlauea, long thought to be part of Mauna Loa, is the only currently active subaerial volcano in the Hawaiian Island chain and is home to Pele, the Hawaiian volcano goddess.
Motivation
Live coral growth on the Big Island is typically limited to scattered aggregate corals on volcanic boulders and pavement. The USGS is working with the National Park Service on the Kona (west) coast of Hawaiʻi to evaluate the geologic resources at Puʻukoholā Heiau National Historic Site, Kaloko-Honokōhau National Historical Park, and at Puʻuhonua O Hōnaunau (City of Refuge) National Historical Park, including benthic habitat mapping of the nearshore coral ecosystem and nutrient flux from groundwater sources. Other partners involved in this work include the University of Hawaiʻi, Stanford University, and the University of California, Santa Cruz.
The island of Hawaiʻi is just one of the USGS Coral Reef Project's study locations.
Reef Hydrodynamics and Sediment Processes
Role of Reefs in Coastal Protection
Reef Resource Assessments - Planning for the Future
Hydrogeology and Reef Health
Climate Change and Land-use Histories
Hawai'i data sets produced by the Coral Reef Project
Dynamically downscaled future wave projections from SWAN model results for the main Hawaiian Islands
Projected flooding extents and depths based on 10-, 50-, 100-, and 500-year wave-energy return periods, with and without coral reefs, for the States of Hawaii and Florida, the Territories of Guam, American Samoa, Puerto Rico, and the U.S. Virgin Islands,
Below are publications associated with this project.
The value of US coral reefs for flood risk reduction
Nearshore water quality and coral health indicators along the west coast of the Island of Hawaiʻi, 2010–2014
Rigorously valuing the role of U.S. coral reefs in coastal hazard risk reduction
Geochemical sourcing of runoff from a young volcanic watershed to an impacted coral reef in Pelekane Bay, Hawaii
Rare earth element behavior during groundwater – seawater mixing along the Kona Coast of Hawaii
Groundwater-derived nutrient and trace element transport to a nearshore Kona coral ecosystem: Experimental mixing model results
Ground-truthing electrical resistivity methods in support of submarine groundwater discharge studies: Examples from Hawaii, Washington, and California
The effectiveness of coral reefs for coastal hazard risk reduction and adaptation
Coastal circulation and sediment dynamics in Pelekane and Kawaihae Bays, Hawaii--measurements of waves, currents, temperature, salinity, turbidity, and geochronology: November 2010--March 2011
From ridge to reef—linking erosion and changing watersheds to impacts on the coral reef ecosystems of Hawai‘i and the Pacific Ocean
Seafloor morphology and coral habitat variability in a volcanic environment: Kaloko-Honokohau National Park, Hawaii, USA
The use (and misuse) of sediment traps in coral reef environments: Theory, observations, and suggested protocols
As part of the USGS Coral Reef Project, the USGS is working on the Kona (west) coast of Hawaiʻi to evaluate geologic resources at two historical parks.
Overview
The island of Hawaiʻi, known as the Big Island, is the largest in the Hawaiian Islands chain. Greater than twice the area of the remaining main eight Hawaiian Islands combined, Hawaiʻi encompasses 10,432 sq km (4,028 sq mi). The island was formed from five major volcanoes. The volcano of Mauna Kea is the tallest mountain on Earth, reaching nearly 9 km (5.5 mi) from the seafloor to the summit. Although shorter, Mauna Loa's massive size makes it the largest volcano in the world. Kīlauea, long thought to be part of Mauna Loa, is the only currently active subaerial volcano in the Hawaiian Island chain and is home to Pele, the Hawaiian volcano goddess.
Motivation
Live coral growth on the Big Island is typically limited to scattered aggregate corals on volcanic boulders and pavement. The USGS is working with the National Park Service on the Kona (west) coast of Hawaiʻi to evaluate the geologic resources at Puʻukoholā Heiau National Historic Site, Kaloko-Honokōhau National Historical Park, and at Puʻuhonua O Hōnaunau (City of Refuge) National Historical Park, including benthic habitat mapping of the nearshore coral ecosystem and nutrient flux from groundwater sources. Other partners involved in this work include the University of Hawaiʻi, Stanford University, and the University of California, Santa Cruz.
The island of Hawaiʻi is just one of the USGS Coral Reef Project's study locations.
Reef Hydrodynamics and Sediment Processes
Role of Reefs in Coastal Protection
Reef Resource Assessments - Planning for the Future
Hydrogeology and Reef Health
Climate Change and Land-use Histories
Hawai'i data sets produced by the Coral Reef Project
Dynamically downscaled future wave projections from SWAN model results for the main Hawaiian Islands
Projected flooding extents and depths based on 10-, 50-, 100-, and 500-year wave-energy return periods, with and without coral reefs, for the States of Hawaii and Florida, the Territories of Guam, American Samoa, Puerto Rico, and the U.S. Virgin Islands,
Below are publications associated with this project.