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I discovered shatter cones approximately 1. Historic Santa Fe Plaza on NM Highway 4. Location map of the Santa Fe Impact Structure in north central New. Mexico,USA. Further investigation revealed a road cut with a beautiful nest of shatter cones rivaling those of Vredefort, Sudbury, and other well known shatter cone exposures. The road cut contains shatter cones ranging in size from a few centimeters up to 2 meters in a large tabular lensof resistant crystalline rock striking north south and dipping 6. The lens is composed of several rock types which are cut by a dominant fracture system striking plusor minus 1. The rocks in the lensare schist exhibiting varying degrees of schistosity and grain size. JohnLewis/236458517alt10?$prod_main$' alt='Carry Map 3 4 Crackle' title='Carry Map 3 4 Crackle' />Sony Corporation, Son Kabushiki Kaisha, s o n i often referred to simply as Sony is a Japanese multinational conglomerate. Subscribe to Vandenberg launch alerts via RSS December 13, 2017 Time still TBD A Delta 4 is scheduled to loft a reconnaissance payload into orbit for the National. Hear that roar A big airplane is taking off Cargo planes carry many goods that we use. Jumbo jets carry many people. Through delightfully simple text and. There is a black, isotropic except for some elongation of the grains, fine grained quartz, hornblende, biotite schist exhibiting very little schistosity that produces the best nestled, convex, horsetail striations shatter cones with the sharpest detail. There is a soft, grey schist exhibiting a high degree of schistosity which contains numerous, convex, horsetail striations shatter cones, but without the fine grained detail found in the hard black schist. Carry Map 3 4 Crackle' title='Carry Map 3 4 Crackle' />The schist is intruded by a granitic rock of at least three different grain sizes very fine grained granite, and fine to medium grained granite, and a pegmatite. There are shatter cones developed in all these granites of varying grain sizes, but as with the schist the finer the grain and more isotropic the rock the sharper and more precise the horsetail striations are. Nest of shatter cones in fine grained granitic rock some of the cones are over 1. Photo of a beautiful shatter cone in a black, hard, isotropic except for some elongation of the grains, fine grained quartz, hornblende, biotite schist exhibiting very little schistosity. Photo of a small shatter cone in a fine grained granitic rock found approximately 1 kilometer west of the above mentioned road cut verifying that the shatter cones were not caused by blasting during road construction. The discovery of Shatter Cones precipitated an investigation into their origin. Siobhan P.  Frackelman et. Shatter cone and microscopic shock alteration evidence for a post Paleoproterozoic terrestrial impact structure near Santa Fe, New Mexico, USASiobhan P. Fackelman, Jared R. Morrow, Christian Koeberl, Thornton H. Mc. Elvain, 2. 00. Elsevier B. V. All rights reserved. This paper verified that the horsetail striations are indeed shatter cones and they also found Planar Deformation Features within the shatter cones confirming that they were caused by a bolide impact. Kasturi Serial Ringtone Download. The authors speculate the age of the impact to be between early Mississippian and Mesoproterozoic. My research which has continued through 2. Mid Tertiary. The balance of this page is my interpretation of continuing research on the Santa Fe Impact. Structure. The morphological Santa Fe Impact Structure has yet to be defined and may be completely destroyed however, the following oblique view downloaded from Google Earth is an elongated circular structure that could represent the remnants of the Santa Fe Impact Structure or a smaller slightly younger impact structure that helped destroy an earlier larger impact structure that actually was responsible for generating the nest of shatter cones. Marker 0. 50. 21 is the location of the nest of shatter cones in the road cut, I have found shatter cones all along the valley from the road up to markers 0. I have taken samples looking for planar microstructures. Markers 0. 50. 56, 0fo. Pennsylvanian and Mississippian sandstone where I have samples of quartz grains with planar microstructures whose angles to the C Axis I have measured and indexed fitting the requirements for Planar Deformation Features see below. I have found breccia, mega breccia, melts, and probable allocthonus slideblocks all containing quartz with planar microstructures PMs that fit the scale of planar deformation features PDFs and histograms of the angle of the pole of the planar microstructure to the c axis resemble those of known impact structures. Waypoint Numbers on the following two maps 0. I have found grains of quartz with planar microstructures. Waypoint 0. The above map plots the location of the sandstone samples on a geologic map of the Santa Fe Impact Structure. The Geologic Map was cut and pasted from the Preliminary Geologic Map of the Santa Fe Quadrangle Bauer, May, 2. Last Revised 8 October 2. The formation symbols on the map are hard to read at this scale however, the buff yellow represents the Nambe Member of the Tertiary Tesuque Formation, the blue represents the Paleozoic Formations and the grey represents the Precambrian formations, all of which are described below. The descriptions have been cut and pasted from the Preliminary Geologic Map. Ttn Namb Member upper Oligocene to lower Miocene Poorly sorted sandy pebble to cobble conglomerate, sandstone, and minor mudstone composed of detritus eroded from pre Tertiary rocks. Color is typically red to pink but is locally white to very pale pink or buff. Base is unconformable on Proterozoic or Pennsylvanian rocks atvarious locations in the map area. Basal contact is highly irregular in part because of erosional relief along the basal unconformity and also because of interpreted deposition of lower parts of the member in small half grabens. In the Big Tesuque watershed there are at least 4. Namb Member locally present below the Bishops Lodge Member. These lowest Namb strata are distinctive for their abundance of Paleozoic clasts 2. Namb strata between Bishops Lodge volcaniclastic intervals in the Bishops Lodge Arroyo de la Piedra area contain 2. Paleozoic clasts and Namb beds above the Bishops Lodge Member contains lt 1. Paleozoic clasts. These variations in clast composition have been demonstrated through 1. Namb Member. The abundance of Paleozoic clasts in the lower Namb Member is curious since these strata rest on Proterozoic rocks. Although one cannot discount the possibility of Paleozoic rocks cropping out in the vicinity of the current Santa Fe Range during Tesuque deposition, it is also possible that the Paleozoic clasts originated from localities east of the Picuris Pecos fault. The latter interpretation would require Neogene west side up motion of that fault zone, which has been suggested previously but has not been supported by structural studies along the fault. A zone of unusually coarse blocks of Paleozoic limestone and sandstone at the base of the Namb Member near Big Tesuque Creek is indicated on the map by closed box symbols. These clasts are 2 4 m across. Spiegel and Baldwin portrayed a dip slope containing such clasts above Proterozoic rocks on the north side of Big Tesuque Creek as Pennsylvanian bedrock. Despite the large size of the Paleozoic clasts found on that slope, there is no outcrop of such rocks and exposures along the USFS Winsor Trail, at the southern end of that slope, clearly show the large blocks to be in the basal Tesuque Formation. The origin of these large clasts is unknown and is especially puzzling in the absence of nearby Paleozoic outcrops. They may be a residual lag of Pennsylvanian clasts resting on exhumed Precambrian outcrops and then buried beneath Tesuque Formation. Otherwise, clast sizes in the Namb Member are generally 2 2. About Vandenberg Air Force Base. As expected, I was only able to observe the Titan 4 while the solid. A relatively faint exhaust trail appeared. I focused the binoculars on it, I could. As the vehicle climbed, the flame became. As soon as the SRBs separated and they got surprisingly. The SRBs flashed a few times while tumbling, and then faded. Pacific Ocean impact. Goodbye Titan Russ Schnapp. San Diego, CA. Wow This was one day I was actually glad to be a taxpayer My love. I parked at the North end of Union Sugar Road on the bank of the. Santa Ynez river next to an immense field of artichokes, just under. We could see the top 3. The weather was perfect with only a few alto nimbus clouds. Liftoff occurs, the last of the Titans slowly lifts up past the trees. Through binoculars we could see the. The flame was so very very bright, it burned. The length. of the flame was 3 or 4 times the length of the rocket itself. It. only took a few seconds before the sound hit us. It started off as a. The rocket turned to. South and pointed its engines almost directly at our location. You could actually feel the sound pressing against your skin and. When booster separation occurred, we. Everything faded into the. We could still hear the rumble and crackle of the. Inside tip for readers While we were driving back into Lompoc to. I have. ever seen. There was tons of equipment including a generator to run. I stopped and asked where we could view the footage. The. gentleman told me its to be included in an upcoming pilot working. Space on the Fox Network to be aired sometime between Spring. Fall Todd Walker and Jer Jarvis. Pismo Beach, CA. The launch was visible and quite audible from here at Morro Bay in. Because of the southerly. I was watching with a 2. It was a peculiar sight when the main liquid. My wife, watching without a telescope, remarked. The solids did seem to keep burning long after separation. Their crazy. tumbling still smoking as well was amusing to watch. The main engines. When the noise showed up, it was appropriately. Vandenberg. J. R.