Images

The lava fragments ejected ranged in size from dust-sized particles up to spatter bombs about 70 cm (~30 inches) across. The larger clasts - the bombs - dotted the ground around the tourist overlook and webcam, giving the area a look reminiscent of a cow pasture.

Spatter landed on wooden fencing laying on the ground at the closed tourist overlook, igniting it in a few places.

Spatter landed on wooden fencing laying on the ground at the closed tourist overlook, igniting it in a few places.

The part of the Overlook crater wall that collapsed is evident in the center of this photo by its white color.

Tim Sargent, a hydrology tech at the New England Water Science Center, is checking to make sure that the bracket he installed is level.

Marinna Martini prepares to deploy a NIMBBLE from the R/V Connecticut south of Martha's Vineyard

Map showing the "June 27 breakout" flow at Pu‘u ‘Ō‘ō in Kīlauea's East Rift Zone. The area of the new flow as mapped on June 30 is shown in pink, while widening of the flow as July 18 is shown in red.

Here is steeper view of the inactive lava pond, just left of center. After it was abandoned, its surface crusted over and sagged to form a gentle bowl. Skylights and points of fume just right of center mark the trace of the new tube. Pu‘u ‘Ō‘ō is at upper right. The view is toward the south-southeast.

The front of the "June 27 breakout" flow, seen here as the silvery lava at lower right, is about 2.0 km (~1.2 miles) northeast from its vent (as measured in a straight line), and surrounds what little remains of Pu‘u Kahauale‘a, a forested cone several hundred years old. View is toward the southwest, and Pu‘u ‘Ō‘ō is at upper right.

Since the onset of the "June 27 breakout" flow, the central part of Pu‘u ‘Ō‘ō's crater has been collapsing slowly. Thick fume and steam prevented good views, but this photo shows the edge of the ring fracture that bounds the collapse. The heavy fume comes from pits that formed where spatter cones used to be.

Since the onset of the "June 27 breakout" flow, the central part of Pu‘u ‘Ō‘ō's crater has been collapsing slowly. Thick fume and steam prevented good views, but this photo shows the edge of the ring fracture that bounds the collapse. The heavy fume comes from pits that formed where spatter cones used to be.

Perhaps the most interesting feature in the new crater at Pu‘u ‘Ō‘ō is the pit formed on the southern side of the crater floor. There, a small lava pond roughly 10 m (~30 ft) across has been sporadically overflowing and sending lava toward the deeper central part of the crater. View is to the south.

Perhaps the most interesting feature in the new crater at Pu‘u ‘Ō‘ō is the pit formed on the southern side of the crater floor. There, a small lava pond roughly 10 m (~30 ft) across has been sporadically overflowing and sending lava toward the deeper central part of the crater. View is to the south.

After the June 27 breakout started, a perched lava pond - looking something like a giant above-ground swimming pool - grew over the main vent. Notice the nearly flat upper surface of the now-inactive pond just above and to the left of center, and the relatively steep levee which contained the pond.

After the June 27 breakout started, a perched lava pond - looking something like a giant above-ground swimming pool - grew over the main vent. Notice the nearly flat upper surface of the now-inactive pond just above and to the left of center, and the relatively steep levee which contained the pond.

Here is steeper view of the inactive lava pond, just left of center. After it was abandoned, its surface crusted over and sagged to form a gentle bowl. Skylights and points of fume just right of center mark the trace of the new tube. Pu‘u ‘Ō‘ō is at upper right. The view is toward the south-southeast.

The front of the "June 27 breakout" flow, seen here as the silvery lava at lower right, is about 2.0 km (~1.2 miles) northeast from its vent (as measured in a straight line), and surrounds what little remains of Pu‘u Kahauale‘a, a forested cone several hundred years old. View is toward the southwest, and Pu‘u ‘Ō‘ō is at upper right.

Here is a closer view showing the beleaguered Pu‘u Kahauale‘a surrounded by active pāhoehoe flows. The view is to the northwest.

Jen Suttles collects water samples from a salt marsh tidal creek (East Falmouth, MA) for laboratory analysis of total organic carbon.  These samples will be compared to data recorded by instrumentation deployed in an adjacent tidal creek as part of research efforts to quantify carbon dynamics in coastal ecosystems

The Salt Marsh Observatory at Sage Lot Pond in the Waquoit Bay National Estuarine Research Reserve serves as an important platform for research in coastal salt marshes. Infrastrucutre in this marsh allows researchers to access sites while maintaining habitat and platform health.

A Sontek IQ ADCP measures depth and velocity of a salt marsh creek (Cape Cod, MA)