>anons are under attack
>anons are not divided
PLEASE FIX THE BREAD AND TIDY UP THE SHIP.
Q
Can we figure out some way to work together to verify each bread as it moves?
That's probably the best way to proceed, isnt it? A new super secret division of digital soldiers that have proven themselves against the darkness.
After 20 years of feeling mostly alone in this fight I must say that would be a very nice way to end it. KEK
https://www.nysga-online.net/wp-content/uploads/2019/06/NYSGA-1991-SP1-Subsurface-Geology-Of-The-Finger-Lakes-Region.pdf
That the Finger Lakes are deeply scoured and infilled by thick sediment
sequences was known from bathymetric surveys of the lakes completed in the
late 1800's (Bloomfield, 1978), a drill record of 1,080' (329m) of
unconsolidated sediment at Watkins Glen (Tarr, 1904), and the publication of a
line drawing of one seismic reflection profile from Seneca Lake (Woodrow et
al., 1969). This paucity of subsurface geologic data has been a major void in
our knowledge and understanding of the geologic history of the Finger Lakes.
Many questions remained unresolved including the most fundamental – "When and
by what processes were the great Finger Lakes troughs eroded?" (Bloom, 1984,
p. 61). Based on the one seismic reflection profile from Seneca Lake, Bloom
(1984) noted that bedrock beneath the lake floor was more V-shaped like that
of a river valley rather than the expected U-shaped glacial trough, and that
there had been multiple erosional and depositional events. He concluded that
more comprehensive seismic reflection surveys of the Finger Lakes "might
reveal a barely suspected missing chapter in the history of the Finger Lakes
region" (Bloom, 1984, p. 61).
During the summer of 1984 we initiated a seismic reflection investigation
of the Finger Lakes with a pilot study of the northern half of Seneca Lake
(Stephens, 1986) supported by a "starter" grant from Syracuse University .
Preliminary results were very encouraging and revealed a detailed stratigraphy
of a thick sediment fill. These preliminary data formed the basis of a
National Science Foundation grant for a comprehensive seismic reflection study
of all eleven Finger Lakes which was carried out during the summers of 1986
and 1987 (Mullins and Hinchey, 1989). The scientific objectives of this study
were three-fold: (1) the provincial question of the origin and evolution of
the Finger Lakes; (2) evaluation of the processes of deglaciation along the
southern margin of the Laurentide ice sheet; and (3) to use the thick sediment
sequence beneath the lakes as a record of continental environmental (paleolimnology/paleoclimatology) change.
Im giving you a hug.
Witches used to trip balls by rubbing a paste made from psychedelics on their inner thighs by rubbing a coated broom handle up there.
They "flew" on full moons.
Mebbe.