Short URL:
Photo Sharing & Video Hosting by SmugMug
  Photo Hosting  Login  Help  
 
 
Michael Garrison  > Beaches & Coastline > Maui's Beaches & Coast
Scenery of Maui's Beaches & Coastlline.
gallery pages:  <<  <  21  22  23  24  25  26  >  >>
< 208 of 319 >
Molokini Crater, looking southeastward into the "horseshoe" of the crater. 

Molokini Island (area above sea level = 22.4 acres) is the uppermost portion of a cinder cone that erupted within Haleakala‘s Southwest Rift Zone. That part of the cone that emerges above the waterline (49 meters maximum elevation) represents about 30 percent of the rim of a small tuffaceous cinder cone that is approximately 400 m (1300+ feet) in diameter. The crater area of the cinder cone forms a lagoon about 30 m (90 feet) deep; outside the lagoon the bottom drops off sharply to a depth of about 150 m (450 feet). [Photograph of the leeward side of the island taken within the Alalakeiki Channel, to the south of Maui.]

To view geographic and other scientific information about Molokini, go to the Coral Reef Assessment and Monitoring Program (CRAMP) home page. To view the results of the 1998 CRAMP Survey of Molokini Island, click here. To view the lists of Molokini's flora and fauna, click here.
A solitary beachfront home sits on a small peninsula south of Wailea on Ahihi Bay, south Maui. Although moderately protected by fringing reef, much of the shoreline in this region is eroded to beach rock, shingle, and cobble by southwestern Kona storm waves.
A typical stretch of beach in the Kawili'lipoa neighborhood of Kihei, south Maui. The substrate consists of coarse white sand and a considerable amount of coral rubble of various grain sizes.   Despite the stout berm anchored by a large thicket of Kiawe trees, Ironwood trees, and coconut palms, and a tough mat of vines and ground-hugging shrubs, this beach has been eroded more than 25 percent since 1947.

East of the Maui Isthmus the shallow sloped coast of Haleakalä faces due west and is heavily developed with tourist facilities at Kïhei and Wailea. Here seawalls and hotel property back long stretches of calcareous sandy beach of varying widths. This coast receives less than 40 cm of rain each year and although moderately protected by fringing reef, much of the shoreline is eroded to beachrock, shingle, and cobble by southwestern Kona storm waves.
South of luxury developments at Wailea, the west-facing coast of Haleakalä includes the most recent lava flows on Maui. Vents at 465 and 170 m above current sea level erupted in 1790 AD, covering 5.7 km ² of the southwest side of the mountain with lava. Pu'u Olai, a parasitic cone formed during this episode, lies on the coast and separates two wide calcareous beaches, Big Beach (pictured here) and Little Beach, collectively known as Mäkena Beach. Big Beach is more than one kilometer long and about 20 m wide; it is backed by a sand-floored forest of Kiawe trees. 

Big Beach, Ahihi Bay, south Maui. Molokini Crater is visible on the horizon.
A partially collapsed lava tube (indicated by red arrow) that emptied seaward during the last volcanic eruptions on Maui in 1790. The large boulders in the foreground are the remnants of the lava tube's roof that collapsed.

Ahihi-Kinau Natural Area Reserve, south Maui.
A panoramic composite image of the 1790 lava flow, Nukuele Point at Cape Kinau, Ahihi-Kinau Natural Area Reserve, Ahihi Bay, south Maui.
Another view of the a'a lava flow at Nukuele Point on Cape Kinau, Ahihi-Kiinau Natural Area Reserve, south Maui. The neighbor island of Ko'olawe is visible on the horizon.

The recent lava flow that forms Cape Kinau (center-right of photo) may be shot-through with a network of lava tubes. The intense black color and lack of vegetation on the flow attests to its recent (1790 AD) eruption.
Clinkery a'a lava flow at Nukuele Point on Cape Kinau, Ahihi-Kiinau Natural Area Reserve, south Maui. The neighbor island of Ko'olawe is visible on the horizon.

In 1790, this extensive lava flow erupted from a split cinder cone on the lower flank of Haleakala volcano, covering many square miles of coastal flats. This was the last volcanic activity on Maui.
Typical view of the arid southern flanks of Haleakala volcano. This coastal desert extends from Ulupalakulu eastward to just west of the village of Kaupo (where the east Maui rain forest begins). The neighbor island of Kaho'olawe is visible on the horizon.
Molokini Crater, looking southeastward into the "horseshoe" of the crater.

Molokini Island (area above sea level = 22.4 acres) is the uppermost portion of a cinder cone that erupted within Haleakala‘s Southwest Rift Zone. That part of the cone that emerges above the waterline (49 meters maximum elevation) represents about 30 percent of the rim of a small tuffaceous cinder cone that is approximately 400 m (1300+ feet) in diameter. The crater area of the cinder cone forms a lagoon about 30 m (90 feet) deep; outside the lagoon the bottom drops off sharply to a depth of about 150 m (450 feet). [Photograph of the leeward side of the island taken within the Alalakeiki Channel, to the south of Maui.]

To view geographic and other scientific information about Molokini, go to the Coral Reef Assessment and Monitoring Program (CRAMP) home page. To view the results of the 1998 CRAMP Survey of Molokini Island, click here. To view the lists of Molokini's flora and fauna, click here.
Coral Reef Assessment and Monitoring Program (CRAMP) home page. To view the results of the 1998 CRAMP Survey of Molokini Island, click here. To view the lists of Molokini's flora and fauna, click here." href="javascript:openLB(166369279,'',XLarge,'',1024,621);">Molokini Crater, looking southeastward into the "horseshoe" of the crater. 

Molokini Island (area above sea level = 22.4 acres) is the uppermost portion of a cinder cone that erupted within Haleakala‘s Southwest Rift Zone. That part of the cone that emerges above the waterline (49 meters maximum elevation) represents about 30 percent of the rim of a small tuffaceous cinder cone that is approximately 400 m (1300+ feet) in diameter. The crater area of the cinder cone forms a lagoon about 30 m (90 feet) deep; outside the lagoon the bottom drops off sharply to a depth of about 150 m (450 feet). [Photograph of the leeward side of the island taken within the Alalakeiki Channel, to the south of Maui.]

To view geographic and other scientific information about Molokini, go to the Coral Reef Assessment and Monitoring Program (CRAMP) home page. To view the results of the 1998 CRAMP Survey of Molokini Island, click here. To view the lists of Molokini's flora and fauna, click here.
Molokini Crater, looking southeastward into the "horseshoe" of the crater.

Molokini Island (area above sea level = 22.4 acres) is the uppermost portion of a cinder cone that erupted within Haleakala‘s Southwest Rift Zone. That part of the cone that emerges above the waterline (49 meters maximum elevation) represents about 30 percent of the rim of a small tuffaceous cinder cone that is approximately 400 m (1300+ feet) in diameter. The crater area of the cinder cone forms a lagoon about 30 m (90 feet) deep; outside the lagoon the bottom drops off sharply to a depth of about 150 m (450 feet). [Photograph of the leeward side of the island taken within the Alalakeiki Channel, to the south of Maui.]

To view geographic and other scientific information about Molokini, go to the Coral Reef Assessment and Monitoring Program (CRAMP) home page. To view the results of the 1998 CRAMP Survey of Molokini Island, click here. To view the lists of Molokini's flora and fauna, click here.
Original size: 1170x710 |
Current: 800x485 |
Keywords: molokini
gallery pages:  <<  <  21  22  23  24  25  26  >  >>
< 208 of 319 >

Comments

| hide gallery comments |


Photo Sharing · About SmugMug · API · Browse Photos · Prints & Gifts · Terms · Privacy · Contact · Login
© 2013 SmugMug, Inc.
Show FeedsAvailable Feeds
Gallery Photos:
Atom FeedAtom | RSS FeedRSS