shove your little poll up your ass
how original.
Virgin Galactic gets FAA’s OK to launch customers to space
(((They))) can hurl human beings into space but I can't fly my drone over a national fucking park. makes sense.
https://www.nbcnews.com/science/space/virgin-galactic-gets-faas-ok-launch-customers-space-rcna1275
Could there have been a DUMB under it?
>it's fucking Miami, you betta believe there's one near it
what coast?
>>14000065
>You don't have time to fuck around
> you need to know the general consensus has been brought to turn your better senses against yourself.
>Those who would prefer the world be silent in this escalating war are relentless in censoring any discussion of what was found
I have not found this to be true.
The Miami oolite of South Florida is representative of a grainstone‐rich carbonate unit that has been surficially karsted, and therefore may be considered as an analog for subsurface reservoirs/aquifers with “high” permeability extremes. The deposit can potentially serve to improve a conceptual understanding of heterogeneity as imparted by shallow‐marine facies changes and early meteoric diagenetic modification.
Reviewed here are recent studies of the Miami oolite with the intent to emphasize those key aspects of the facies and early diagenesis that most impact permeability and fluid flow. The Miami oolite displays the preserved morphology of a fossilized ooid sand body, even though it has been subaerially exposed in a tropical climate since its deposition approximately 120 kyr bp during the last interglacial highstand. The depositional motif is one of a dip‐oriented, tidal bar belt of shoals and shallow channels fronted by a strike‐oriented barrier bar.
The barrier bar comprises cross‐stratified grainstones and locally burrowed grain/packstones, while the tidal shoals and channels are more commonly burrowed pack/grainstones. Surficial karst features (dolines and stratiform caves) have been added during the ca 120 kyr of subaerial exposure, but of more significance is the associated solution‐enhancement of the widespread burrowed facies.
Since the Miami oolite is the uppermost portion of the Biscayne Aquifer, there is also an understanding of fluid flow through the deposit that sheds valuable insight on the larger‐scale, shallow subsurface plumbing.
The pore system comprises matrix pores (interparticle and separate vugs) and touching‐vug macropores that are commonly associated with burrowed [Ophiomorpha] intervals. Ground Penetrating Radar, well, and flow‐test data indicate that matrix porosity provides most of the groundwater storage, whereas the touching vug macropores account for the majority of flow.
The dolines and shallow caves seem to be sufficiently spaced as to generally not be in direct connection, with the result that they are less important in terms of regional flow than the prevailing pore system.
https://www.researchgate.net/publication/338795208_Impact_of_Facies_and_Diagenetic_Variability_on_Permeability_and_Fluid_Flow_in_an_Oolitic_Grainstone_-_Pleistocene_Miami_Oolite
Limestone.
https://www.researchgate.net/figure/Figure-13-Location-map-showing-Florida-Bahamas-region-Digital-elevation-data-coverage_fig1_306493130
ATLANTIC COASTAL RIDGE.
Miami Limestone
The Miami Limestone (formerly the Miami Oolite), named by Sanford (1909), occurs at or near the surface in southeastern peninsular Florida from Palm Beach County to Dade and Monroe Counties. It forms the Atlantic Coastal Ridge and extends beneath the Everglades where it is commonly covered by thin organic and freshwater sediments. The Miami Limestone occurs on the mainland and in the southern Florida Keys from Big Pine Key to the Marquesas Keys. From Big Pine Key to the mainland, the Miami Limestone is replaced by the Key Largo Limestone. To the north, in Palm Beach County, the Miami Limestone grades laterally northward into the Anastasia Formation. The Miami Limestone consists of two facies, an oolitic facies and a bryozoan facies (Hoffmeister et al. [1967]). The oolitic facies consists of white to orangish gray, poorly to moderately indurated, sandy, oolitic limestone (grainstone) with scattered concentrations of fossils. The bryozoan facies consists of white to orangish gray, poorly to well indurated, sandy, fossiliferous limestone (grainstone and packstone). Beds of quartz sand are also present as unindurated sediments and indurated limey sandstones. Fossils present include mollusks, bryozoans, and corals. Molds and casts of fossils are common. The highly porous and permeable Miami Limestone forms much of the Biscayne Aquifer of the surficial aquifer system.
https://mrdata.usgs.gov/geology/state/sgmc2-unit.php?unit=FLPSm;0
q!!!
QQQQQQQQQQQQQQQQQQQQQQQQ
nope. not this time.
surprised they didn't steal the van
>>14000589
fucking WHORES that spread their little piggy legs
be gone whores
nobody wants your rican ass
keep it up, cunt
it's always the dirty little perverts with tiny dicks who love the porn and nasty whores
I filtered your ass, Jew perv