I caught a virus and have not been able to get out hiking this week. I started feeling a bit better yesterday and feel even better today, so I do plan on going out hiking this afternoon. So for today's blog post I decided to check in with the NASA website http://earthobservatory.nasa.gov/.
Using a high-magnification lens, an astronaut photographed almost the
entire 10.5-kilometer long (6.5 mile) Manihiki Island, which lies in
the middle of the Pacific Ocean. Manihiki is one of the larger islands
in the remote Cook Island chain.
From space, Manihiki has the hallmarks of a classic atoll, with its
fringing coral reef and a central lagoon. The coral lives in the warm,
shallow waters which appear as the light blue zones around the main
coastline and the numerous small islets within the lagoon. Most of the
main atoll is made of sandy beaches without vegetation; it appears white
or cream due to dead coral broken up by waves. Soils develop on the
highest parts of these beaches, supporting dense stands of dark green
trees. A few clouds cast shadows on the water.
Two small towns—Tauhunu and Tukao—appear as clusters of small bright
patches etched into the forest. Aircraft land at the runway in Tukao
after flying from New Zealand, which is 3,650 kilometers (2270 miles) to
the southwest. Tourism is the main economic activity on the atoll, with
diving in the lagoon and fishing in the waters outside it as the major
attractions. Manihiki also produces rare black pearls, which are
harvested from the local species of oyster.
The Cook Islands are an independent nation, in “free association”
with New Zealand. The population is small (15,000 people in 2011) and
situated mostly on Manihiki and the 14 other large islands.
An Earth-observing satellite has observed one of the largest
landslides not caused by an earthquake that scientists have observed in a
decade. The landslide occurred in Chin, a remote state in western
Myanmar (Burma), after slow-moving Tropical Storm Komen drenched the
area in July 2015.
The Global Precipitation Measurement (GPM) core observatory observed rain rates of 150 millimeters (5.9 inches)
per hour as Komen moved ashore from the Bay of Bengal on July 30. The
intense rainfall triggered destructive flooding and numerous landslides.
According to some estimates, more than 17,000 homes were destroyed in
Myanmar, 46 people were killed, and hundreds of thousands of people were
affected by the storm.
For months after the storm, monsoon clouds prevented satellites from
collecting visible light imagery of Chin, however
scientists found evidence of three large slides, including an
exceptionally large event that moved 395 million tons of material.
On October 23, 2015, clouds cleared enough for a
satellite to capture a view of several landslides in Chin, including a
massive slide northeast of Tonzang. In the second image above, soil and debris
from the landslide appears tan/brown in contrast to the green forests.
Streams appear as narrow strips of brown because of mud and sediment
washed away by the floods. The first image shows the same area on
November 8, 2014.
Hawaii’s Mauna Loa is the largest active volcano on Earth. The shield volcano
rises gradually from sea level to 4,169 meters (13,678 feet). The
flanks of the mountain extend another 5 kilometers (3 miles) below the
surface, and the massive volcano pushes Earth’s crust down another 8
kilometers. Overall, Mauna Loa’s summit stands about 17,000 meters
(56,000 feet) above its base. For comparison, Mount Everest stands 8,848 meters (29,029 feet) above sea level.
Though it has been quiet during recent decades, Mauna Loa has a long history of volcanic activity. Geologists estimate that the hotspot
that feeds Mauna Loa first started to erupt about one million to
700,000 years ago. After underwater eruptions built up a seamount for
hundreds of thousands of years, lava emerged above the Pacific surface
about 400,000 years ago.
On average, Mauna Loa has erupted roughly every six years for the
past 3,000 years. The most detailed eruption records are available for
the past few centuries. Eruptions usually begin in the summit caldera
with lava flowing down one of the volcano’s two rift zones: the
Northeast Rift Zone and the Southwest Rift Zone. The rift zones are
chains of craters and fissures that extend from the summit to the sea.
The Operational Land Imager (OLI) on Landsat 8
acquired this image of Mauna Loa on December 20, 2014. The elongated
crater in the center is the summit caldera. Lava flows appear black; as
they age, they fade and become gray. Very little vegetation appears on
the summit of Mauna Loa because of the frequent lava flows and the high
elevation. One of the largest flows in modern times occurred in 1950,
when some 376 million cubic meters flowed out from the volcano and
spread across 112 square kilometers (43 square miles) of the island.
Mauna Loa last erupted in 1984. In September 2015, volcanologists raised an alert
after detecting an increase in the number of shallow earthquakes near
the summit and the upper Southwest Rift Zone. However, Mauna Loa is not
yet erupting. Rather, magma reservoirs beneath the summit and upper
Southwest Rift Zone are filling.
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