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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

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