The lower levels of the repuslierilft canyons of Boka City, Atimonia drop off and seal off about at the undergroundscape and the sub undergroundscape, and the subterrainainscape and the presubterrainainscape as well as the subpreundergroundscape and the pre-subundergroundscapelift.

The levels of the repuslierlift canyons of Boka City; Atimonia start at the highest and most uppermost level the macrostrata or the frame grid work nautliftscape and otherwise known throogh out the entire city  as the strata except for openings into underground and the sub underground and the subterrainain scape and the microsubterrrainainscape known as the rift chute channel strait conduit sub chasm and microchasm and microsubchasm connections into the underground, underground-scape and sub underground and subundergroundscape known as the upwelling and uprisings.

The next stop on our virtual journey is to the lowest levels or foundation or basement or root levels in the repulsierlift canyons is the middle levels.  In fact the middle levels are split and reemerged and re congruently intersublayered into many different middle upper; middle upper middle; middle upper lower and middle lower and even lower middle lower; lower middle upper lower; lower middle upper middle lower lower middle lower middle lower middle middle lower lower middle lower levels .

There are certain areas of the repuslierlift known as subsurface and substructure; submegastructure and submacrostructure, sub-mega-macro-structure.

In fact the middle upper levels start off where the primindal, dientrical, contrugent, strastrical, honeycomb and interlayered and interleveled buildings start to become deep subpreunderchasm deep root basement strato-scraper root buildings when the upper overstrata and the middle sub-under-pre-underchasm and the deep lower level under-over-pre-substratric underoverpresubmicroprotoroot buildings start to emerge and remerge and converge into the underchasm, underoverchasm, underoversubchasm, underoverpresubchasm and the relating underground chasm, the subpreunderoversubchasmic underground rift channel, con-emerges  and converges into the underoversubpresubchasm-underoversubpresubstrata; as well as the sub-upwelling and uprisings.  The middle lower level buildings start to wind, up down, center and towards towering sections of the repulser lift canyons. The canyons start to shift, rotate and blend and twist and up-ended and up-unending streams of repulser lift traffic, upoverunending under-over-sub-prestreams of repuslierlift traffic