Today we live in what geologists have named the Anthropocene. The Earth has entered a new geological epoch, and the climate crisis is a reality. The crisis is so substantial and complex that our existing knowledge of environmental disasters is insufficient. Without the realization that we, as human beings, are intimately connected to all other kinds of life, we are guilty of a collective sin of omission by ignoring the fundamental connectedness of humanity and nature. We are not just part of the same cycle, we are nature. And since everything affects and is affected by everything else, it seems sufficient to consider the Anthropocene from many perspectives and fields. 'Connectedness' includes a diverse selection of contributions, including Björk, Greta Thunberg, Donna Haraway and Tomas Saraceno, that brings many perspectives and disciplines into the discussion to the crucial period in which we are currently living.
Deep-water Oil Sand Reservoirs: Ancient Case Histories and Modern Concepts
Amongst other things , before the arrival of the official Ordnance Survey 1:50 000 sheets , she made me topographic ... Mike Rhodes , Mike Henderson , Jeff Cooper , Roy Cohen , Keith O'Nions , Tony Fallick , Peter Hill , John Craven ...
The veins cut Cambro - Ordovician metasedimentary rocks , approximately 150 m from Trout Brook Pluton Appendix II ( cont ... TB - 7 46 32 35 66 42 00 TODD MOUNTAIN Sn , Cu , Pb , Zn , Ag , Au , As quartz , graphite chlorite , muscovite ...
The major feature in the north polar region is open ocean , with continental blocks all south of 35 ° N . Figure 1A shows the effects of monsoons produced by the concentration of continental blocks in the southern hemisphere .
Quaternary Pollen Biostratigraphy in the British Sector of the Central North Sea
Sedimentology of the Upper Proterozoic Glacial Record, Vestertana Group, Finnmark, North Norway
Ostracod Biostratigraphy of the Kimmeridgian in Northern and Western Europe
At time T, the process reverses and deposition is progressively re-established to the left of point P. Deposition spreads over the surface NP which is also the erosional surface LP, the surface of the unconformity (after Eicher, 1976, ...
... to early Palaeozoic ( Iapetus ) ocean basin ( Harland and Gayer 1972 , Gee 1975a , Roberts and Gale 1978 ) . ... 3–5 m ) . Uppermost zones of the Upper Cambrian and lowermost Ordovician ( Tremadoc ) are absent in the Autochthon .
This is despite information suggesting that the Ti-Tree Basin is (in places) infilled to depths of at least 320 metres with sediments, including hydraulically conductive sand-richlayers.