Lava cascade in Thunderbolt Distributary of Labyrinth Cave system
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central section spreads <strong>in</strong>to still-uncollapsed<br />
tubes. The upper part <strong>of</strong> the Silver<br />
Connector level decreases <strong>in</strong> height and<br />
cont<strong>in</strong>ues eastward, where it is nearly<br />
filled with lava. It eventually becomes a<br />
crawlway that cont<strong>in</strong>ues for 30 ft to<br />
where it is plugged with congealed lava.<br />
It is open another 10 ft farther downstream<br />
as the western end <strong>of</strong> the downstream<br />
entrance level.<br />
Part <strong>of</strong> the middle section <strong>of</strong> the<br />
Silver Connector level is equivalent to<br />
the Upper Cataract Tube, but collapse <strong>of</strong><br />
both floor and ro<strong>of</strong> prevents trac<strong>in</strong>g this<br />
connection.<br />
The upstream (western) end <strong>of</strong> the<br />
Silver Connector level is even more<br />
complex: west <strong>of</strong> the Silver Connector<br />
breakdown this level extends <strong>in</strong>to parts<br />
<strong>of</strong> at least five tubes. The highest three<br />
levels are reached from Silver <strong>Cave</strong> (map<br />
14, pl. 5), whose ro<strong>of</strong> lies only 10-12 ft<br />
below the ground surface. The lowest<br />
passage extend<strong>in</strong>g north from the base <strong>of</strong><br />
the Silver Connector is 85 ft below the<br />
surface but still 25 ft above the underly<strong>in</strong>g<br />
Cocoa Pipel<strong>in</strong>e.<br />
Two breakdowns <strong>in</strong> the floor <strong>of</strong> the<br />
Silver Connector level give access to the<br />
Cocoa Pipel<strong>in</strong>e: the eastern (downstream),<br />
Central Connector is an easy<br />
and safe passage <strong>in</strong>to the pipel<strong>in</strong>e; the<br />
other, 540 ft upstream, is the deep,<br />
steep-sided, and very unstable Cocoa<br />
Connector.<br />
The Silver Connector level seems<br />
geologically un<strong>in</strong>terest<strong>in</strong>g at first; its<br />
floor is noth<strong>in</strong>g but a hummocky jumble<br />
<strong>of</strong> large fallen blocks that are difficult to<br />
walk over. The walls are more <strong>in</strong>structive,<br />
for patches <strong>of</strong> dripstone show the<br />
perched rema<strong>in</strong>s <strong>of</strong> a collapsed tube here<br />
and there, and irregular shelf-like extensions<br />
from the walls can be identified as<br />
edges <strong>of</strong> the floor <strong>of</strong> a broken-<strong>of</strong>f tube.<br />
Only rarely can one see any primary<br />
features <strong>in</strong> the high and <strong>in</strong>accessible<br />
ro<strong>of</strong>. In fact, play<strong>in</strong>g a strong light over<br />
this ro<strong>of</strong>, 15-60 ft overhead, is a disconcert<strong>in</strong>g<br />
experience when one notices<br />
the many precariously perched blocks<br />
that appear ready to fall. However, no<br />
other cave <strong>in</strong> <strong>Lava</strong> Beds National Monument<br />
provides such <strong>in</strong>sights <strong>in</strong>to the<br />
structure and mechanics <strong>of</strong> operation <strong>of</strong><br />
lava tubes as does Post Office. Just as the<br />
shambles after an earthquake reveal the<br />
structural details <strong>of</strong> broken build<strong>in</strong>gs, an<br />
<strong>in</strong>spection <strong>of</strong> the collapsed walls <strong>of</strong> the<br />
Silver Connector level provides details<br />
<strong>of</strong> tube construction and <strong>of</strong> the mechanics<br />
<strong>of</strong> plastic flow <strong>in</strong> lava tubes that could<br />
never be <strong>in</strong>ferred from well-preserved<br />
lava tubes coated with lava plaster. A<br />
few select features <strong>of</strong> this remarkable<br />
lava-tube ru<strong>in</strong> that contribute to the<br />
understand<strong>in</strong>g <strong>of</strong> lava tubes are described<br />
here<strong>in</strong>. Areas <strong>of</strong> special <strong>in</strong>terest or beauty<br />
are also described. Not all features<br />
shown on the map are described here<strong>in</strong>.<br />
The floor <strong>of</strong> the Silver Connector<br />
level, 200 ft upstream from the breakdown<br />
that connects it with the Upper<br />
Cataract Tube, is surmounted by an<br />
unusually high and steep conical pile <strong>of</strong><br />
collapse debris. The pile rises 45ft above<br />
the thick blanket <strong>of</strong> tumbled blocks that<br />
forms the floor <strong>of</strong> the cave. Nearby are<br />
irregular benches jutt<strong>in</strong>g from the wall at<br />
various po<strong>in</strong>ts, remnants <strong>of</strong> at least three<br />
tubes that coalesced to create a cave<br />
30-45 ft high. Farther upstream (northwest)<br />
65 ft from the base <strong>of</strong> this huge<br />
collapse pile, the floor <strong>of</strong> the Silver<br />
Connector level drops away <strong>in</strong>to the<br />
Central Connector, a breakdown 60 ft<br />
long and 6-15 ft wide. This connector<br />
gives easy access to the eastern part <strong>of</strong><br />
the Cocoa Pipel<strong>in</strong>e lava tube, 25 ft<br />
below. Before visit<strong>in</strong>g this very different<br />
level, however, cont<strong>in</strong>ue upstream <strong>in</strong> the<br />
Silver Connector level by carefully skirt<strong>in</strong>g<br />
the Central Connector along the top<br />
<strong>of</strong> its southeast wall. For some distance<br />
upstream from the Central Connector,<br />
the ceil<strong>in</strong>g <strong>of</strong> the Silver Connector level<br />
is nearly 35 ft high and coated with<br />
<strong>of</strong>f-white caliche (calcium carbonate<br />
crusts). If illum<strong>in</strong>ated while wet, caliche<br />
has a highly reflective, silvery glow.<br />
Water dripp<strong>in</strong>g from this ro<strong>of</strong> has deposited<br />
upon collapse blocks on the floor<br />
f<strong>in</strong>e examples <strong>of</strong> the fragile arborescent<br />
growths <strong>of</strong> caliche popularly called<br />
"cave coral." Most growths are white,<br />
but where sta<strong>in</strong>ed by hydrous iron and<br />
manganese oxides, organic soil compounds,<br />
or fungi, they can be deep red,<br />
lustrous black, yellow, p<strong>in</strong>k, silky gray,<br />
and light blue.<br />
The next major <strong>in</strong>terruption, 540 ft<br />
farther upstream from the Central Connector,<br />
is the Cocoa Connector, a deep,<br />
unstable 22- by 15-ft hole. The descent<br />
through the Cocoa Connector to the floor<br />
<strong>of</strong> the Cocoa Pipel<strong>in</strong>e, 40 ft below, is<br />
over loose and easily rolled debris. A<br />
descent here is neither recommended nor<br />
necessary because there are two safer<br />
entrances <strong>in</strong>to the Cocoa Pipel<strong>in</strong>e. Upstream<br />
toward the Cocoa Connector, the<br />
blanket <strong>of</strong> collapse blocks on the floor<br />
thickens, and many huge blocks as much<br />
as 40ft long are embedded <strong>in</strong> the debris.<br />
Some <strong>of</strong> these large blocks show surface<br />
features, which testify that they are large<br />
pieces <strong>of</strong> the separations between two<br />
superposed levels. Collapse over considerable<br />
areas must have occurred <strong>in</strong> places,<br />
as such large blocks surely are not due<br />
to the slow unravel<strong>in</strong>g upward <strong>of</strong> ro<strong>of</strong><br />
slabs loosened along m<strong>in</strong>or jo<strong>in</strong>ts and<br />
cracks. The truncated edges <strong>of</strong> some<br />
floor benches still hang<strong>in</strong>g from the walls<br />
also imply large-scale rockfalls. The<br />
piles <strong>of</strong> collapse blocks are a jigsaw<br />
puzzle <strong>of</strong> surface features and the broken<br />
walls <strong>of</strong> lava tubes. It is common to f<strong>in</strong>d<br />
large fallen blocks with several coat<strong>in</strong>gs<br />
<strong>of</strong> lava plaster sliced <strong>in</strong> cross-section on<br />
one or more broken edges.<br />
Downstream 65 ft from the Cocoa<br />
Connector, the Silver Connector level<br />
makes a 45° turn to the left (as viewed<br />
look<strong>in</strong>g upstream) and heads almost due<br />
south. The Cocoa Pipel<strong>in</strong>e below turns<br />
the same corner with an even sharper<br />
bend. The effect <strong>of</strong> a sharp bend <strong>in</strong> the<br />
orig<strong>in</strong>al, pre-lava topographic valley <strong>in</strong><br />
controll<strong>in</strong>g the superposition <strong>of</strong> the two<br />
lava tubes seems clear, because the curve<br />
became gentler as the pre-flow depression<br />
was filled <strong>in</strong>.<br />
The dangerous Cocoa Connector can<br />
be skirted safely on its northwest side.<br />
Once around it one climbs a steep 15- to<br />
20-ft pile <strong>of</strong> collapse rubble. In another<br />
190 ft is the large vertical hole through<br />
several levels called the Silver Connector.<br />
Silver Connector<br />
The breakdown 190 ft upstream from<br />
the Cocoa Connector (map 15, pl. 5) has<br />
for several years been called the Silver<br />
Connector (fig. 51) because its top is <strong>in</strong><br />
Silver <strong>Cave</strong>. It extends vertically for 60<br />
Post Office <strong>Cave</strong> 77