U.S. Department of Interior, U.S. Geological Survey
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Incandescent hole formed on November 30, 2004 in MLK vent, part of the cluster of vents in the MLK-June 25-Puka Nui complex at south base of Pu`u `O`o.

 
     
  Small new hornito, informally known as a carlito, near Kiln hornito near upper end of PKK lava tube. Such features form above a fulltube and make a roaring noise as gas escapes through small openings in the roof of the tube. The hot gas keeps the rock inside thecarlito incandescent. This guy is about 1 meter high at most.  
     
  Early dawning sky forms backdrop for breakout in west branch of PKK flow at brink of old sea cliff above West Highcastle lava delta. Width of breakout, about 4 meters.  
     
  Eye-level view of pahoehoe toe in west finger of west branch. Filaments of crust stretch around bubbles as lava oozes ahead. Toe is about 10 centimeters high.  
     
  Incandescent hole formed on November 30, 2004 in MLK vent, part of theAerial view looking east across Pu`u `O`o. Kona windblows thick gas plume north from main crater. West Gap pit also is choked with gas just west of main crater. Red is active rock slide at headwall of Puka Nui, a large, complex collapse area in central part of image. The individual pits have not been named, except for Lua Hou, the tiny pit giving off narrow gas plume near right edge of photo. Note the concentric cracks around the larger collapse features. Lava flows in this area cover older spatter and cinder from Pu`u `O`o, which is unstable and slowly spreading, developing pits in the overlying flows. Yellowish slope in middle of photo is part of Pu`u `O`o's cone that is falling apart. cluster of vents in the MLK-June 25-Puka Nui complex at south base of Pu`u `O`o.  
     
  Geophysicists make measurements across the roof of a lava tube leading from the episode 51 vents. The measurements reveal the size of the tube and the cross-sectional area of the lava stream. Together with measurements of the speed of the lava stream, these data allow us to estimate lava discharge from the volcano.  
     
  Lava bubbles explode from two openings in the roof of the lava tube system on the Kamokuna lava bench. The openings are located 10-25 m inland from the edge of the bench. The largest bubbles tossed fragments as high as 40 m and flung ribbons of spatter several meters long that landed intact on the bench. The bursts were accompanied by loud, chugging noises as the lava exploded from the tube. During the activity, a steam jet (lower right) produced a vigorous white steam plume. These explosions occur when seawater flashes to steam within the confined space of an active lava tube.  
     
  General view of new Kohola ocean entry, looking east from Ka Lae`apuki, of cascades and new flow coating beach. Sea cliff is about 10 m high. Wispy glow near center right edge is from steam at water's edge.  
     
 

Steam generated by entry of lava into water reflects incandescence and appears reddish.

 

 
     
  Detail of largest breakout feeding lava into water (near right of image). Flow is about 7 meters long.  
     
  Lobe of lava moving along west edge of flow reached top of sea cliff and began plunging to beach below. This image was taken several minutes after the falls began. Liquid lava is 2-4 meters wide.  
     
  Near view of flat toe moving across quite flat surface. Note that lava at moving front of toe is emerging from base and cooling as it rises. Flaming grass at front of another toe.  
     
  Lava pours down flank of 4-m-high tumulus in old (>600 year) flow. Lava comes from interior of Kohola flow, which banked against north side of tumulus, inflated over the top, and now spills down steep south side.  
     
  Pretty Petunia skylight in roof of PKK lava tube, upper part of PKK flow. View looks downstream. Some of the  lava visible through the skylight will eventually end up at East Lae`apuki 1-2 hr later.  
     
  View from farther right, looking at the ever more sluggish lava falls and its growing surface crust.  
     
  Tube-fed pahoehoe flow from Kupaianaha crosses the highway and enters Kalapana in 1986.  
     
  Pahoehoe toe, about 1 meter long, approaches a loose rock (lower center) on a ledge near top of gaping crack.  
     
  The actual breakout point, where lava wells from a lava tube and sees the light of day for the first time in its history.  
     
 

Looking west at Banana ocean entry. Lava enters the water at several places along the front of the 1.5-yr-old Wilipe`a lava delta. Note the numerous breakouts in the Banana flow on the surface of the delta.

 
     
  Lava falls. Lava hits a newly(?) forming delta, pours down it, and finally freefalls into water. Height of falls, about 7 meters.  
     
 

Slender lava falls off side of Wilipe`a delta. Wider cascade in background. Falls are 2-3 meters high.

 
     
 

Gush of lava comes down old sea cliff, suddenly breaking out of flow between cascades.

 
     
     
 

Source: http://www.kohalagallery.com/volcano1.htm

 
     
     
 

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