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re: Here's another song my brother and I made using AI called, "Frannie of the Bay"
Posted on 8/26/26 at 2:55 pm to Dawglovertoo
Posted on 8/26/26 at 2:55 pm to Dawglovertoo
quote:
When the page open just scroll down to where it says, "Bill and Bob Clark" and tap our names. The interview will begin. We go into great detail about our February 5, 1985
Yep, you are autistic.
Posted on 8/26/26 at 3:30 pm to DeltaTigerDelta
Is this the same guy that claimed he was with Jerry Garcia at Monterey or Altamont or somewhere?
Posted on 8/26/26 at 4:05 pm to hogcard1964
quote:
Is this the same guy that claimed he was with Jerry Garcia at Monterey or Altamont or somewhere?
Yes
Among other claims
Posted on 8/27/26 at 10:24 am to hogcard1964
quote:
Is this the same guy that claimed he was with Jerry Garcia at Monterey or Altamont or somewhere?
It was in Toronto in 1970 at the first concert of The Festival Express tour.
Posted on 8/27/26 at 10:29 am to DeltaTigerDelta
quote:
Yep, you are autistic
Yep, you are afraid to accept the truth that sea serpents exist in reality.
Posted on 8/27/26 at 10:32 am to Cdawg
Thanks. I appreciate you saying that.
Posted on 8/27/26 at 10:38 am to jchamil
Your ignorant opinion of me doesn't trump what I saw with my own eyes on February 5, 1985.
Here's the final version of the slowed down and enlarged segment of my January 26, 2004 video of sea serpents in San Francisco Bay with the song I made called, "Serpent of the Bay" included in the video.
Here's the final version of the slowed down and enlarged segment of my January 26, 2004 video of sea serpents in San Francisco Bay with the song I made called, "Serpent of the Bay" included in the video.
This post was edited on 8/27/26 at 10:40 am
Posted on 8/27/26 at 10:59 am to TheTideMustRoll
Bruce Champagne who has a B.S. in Marine Biology analyzed the entire video and disagrees with you.
Here's what he wrote in his written report analysing my January 26, 2004 video explaining why it isn't sea lions, seals, dolphins or whales in the video.
"Sea lions may swim at the surface, intermittently leaping clear of the water (Riedman, 1990). The author has observed this often predictable, group swimming behavior displayed by sea lions, presumably minimizing the vulnerability to predators (Carcarodon carcharias, etc.) as they swim out to deeper water through a high-risk area to feed. A review of The Clark video, with magnification to selected and successive still frames shows that the hump-like images maintain a nearly single-file position and continuous positional orientation as the images track and change direction. The author was unable to locate a frame or a sequence displaying the head and/or flippers of a pinniped, as would be an expected characteristic observation of such swimming behaviors. At no time did the line of humps break formation from the single file track, as would be expected by a group of swimming pinnipeds (Personal Observation).
True seals, or phocids are known to swim at the surface in a different manner than that of the sea lions, or otariids. In the wild, phocids swim in near vertical movements from the seafloor to the surface, presumably as a means of minimizing their more vulnerable surface position to predators (LeBlouf, et al, 1986). Typically, it may be difficult to observe phocids during the minimal exposure at the surface, which may only be a breach of the surface by the head or nostrils. The calculated dimensions of the recorded images in the video extended above the surface (Paiva and Slusher, 2005) are also in excess of known pinniped species. The author further suggests that the behavior (swimming and breaching) and morphology displayed by the images in the video are not consistent with known, pinniped behaviors and size ranges.
Cetaceans are also known to enter the San Francisco Bay. Most frequently observed are Gray Whales (Eschrichtius robutus) and Harbor Porpoises (Phocoena Phocoena). Less frequently observed are Pacific White-sided Dolphins and the Dall's Porpoise. (Phocoenoides dalli). Occasionally, Humpback Whales (Megaptera novaeangliae) have entered the bay and associated waterways.
The largest measured images in the Clark video are within the known ranges of both Gray and Humpback Whales. Whales are also known to breach the surface at a height comparable to that measured by the animals in the video. However, the animals in the Clark video maintain an extended position above the surface for approximately 2.5 sec., and continue to maintain a lower position above the surface without submerging below the air/water interface. The periscope behavior exhibited by the images on the video is likely a deliberate and control behavior which appears to be in excess of the known capabilities of larger cetaceans as they are unable to control their mass from falling below the air/water interface after breaching. Additionally, if the track line segments in the video are considered only visible parts of one unit for inclusion within the known size ranges of the larger cetaceans the flexibility exhibited by the images in the Clark video do not appear to be within the range of flexure of either species of whale. If the image segments are considered independent animals, the grouping would be inconsistent with known mysticete group behavior relevant to this sequence (Walker, 1962). The "spyhopping" behavior displayed by some whale species may produce a similar appearance as that of the images in the video. However, the "spyhopping" behavior is a stationary surface display and is not consistent with the movement displayed by the images in the video. Exhalations, or "blows," could be identified at the distances involved in the video (Personal Observation), but these predictable and lingering exhalations are not observed in the video, as would be expected.
The smallest segments of the recorded images are within the known size ranges of the Pacific White-sided Dolphin and Dall's Porpoise. However, the swimming motions and behaviors, both individually and grouped, are not consistent with the known behavior of either species. Because the behaviors and capabilities of the Clark video images are not consistent with the known abilities and/or behaviors of the cetacean species frequenting the area, it is proposed that the video images are not those of a known cetacean."
Here's what he wrote in his written report analysing my January 26, 2004 video explaining why it isn't sea lions, seals, dolphins or whales in the video.
"Sea lions may swim at the surface, intermittently leaping clear of the water (Riedman, 1990). The author has observed this often predictable, group swimming behavior displayed by sea lions, presumably minimizing the vulnerability to predators (Carcarodon carcharias, etc.) as they swim out to deeper water through a high-risk area to feed. A review of The Clark video, with magnification to selected and successive still frames shows that the hump-like images maintain a nearly single-file position and continuous positional orientation as the images track and change direction. The author was unable to locate a frame or a sequence displaying the head and/or flippers of a pinniped, as would be an expected characteristic observation of such swimming behaviors. At no time did the line of humps break formation from the single file track, as would be expected by a group of swimming pinnipeds (Personal Observation).
True seals, or phocids are known to swim at the surface in a different manner than that of the sea lions, or otariids. In the wild, phocids swim in near vertical movements from the seafloor to the surface, presumably as a means of minimizing their more vulnerable surface position to predators (LeBlouf, et al, 1986). Typically, it may be difficult to observe phocids during the minimal exposure at the surface, which may only be a breach of the surface by the head or nostrils. The calculated dimensions of the recorded images in the video extended above the surface (Paiva and Slusher, 2005) are also in excess of known pinniped species. The author further suggests that the behavior (swimming and breaching) and morphology displayed by the images in the video are not consistent with known, pinniped behaviors and size ranges.
Cetaceans are also known to enter the San Francisco Bay. Most frequently observed are Gray Whales (Eschrichtius robutus) and Harbor Porpoises (Phocoena Phocoena). Less frequently observed are Pacific White-sided Dolphins and the Dall's Porpoise. (Phocoenoides dalli). Occasionally, Humpback Whales (Megaptera novaeangliae) have entered the bay and associated waterways.
The largest measured images in the Clark video are within the known ranges of both Gray and Humpback Whales. Whales are also known to breach the surface at a height comparable to that measured by the animals in the video. However, the animals in the Clark video maintain an extended position above the surface for approximately 2.5 sec., and continue to maintain a lower position above the surface without submerging below the air/water interface. The periscope behavior exhibited by the images on the video is likely a deliberate and control behavior which appears to be in excess of the known capabilities of larger cetaceans as they are unable to control their mass from falling below the air/water interface after breaching. Additionally, if the track line segments in the video are considered only visible parts of one unit for inclusion within the known size ranges of the larger cetaceans the flexibility exhibited by the images in the Clark video do not appear to be within the range of flexure of either species of whale. If the image segments are considered independent animals, the grouping would be inconsistent with known mysticete group behavior relevant to this sequence (Walker, 1962). The "spyhopping" behavior displayed by some whale species may produce a similar appearance as that of the images in the video. However, the "spyhopping" behavior is a stationary surface display and is not consistent with the movement displayed by the images in the video. Exhalations, or "blows," could be identified at the distances involved in the video (Personal Observation), but these predictable and lingering exhalations are not observed in the video, as would be expected.
The smallest segments of the recorded images are within the known size ranges of the Pacific White-sided Dolphin and Dall's Porpoise. However, the swimming motions and behaviors, both individually and grouped, are not consistent with the known behavior of either species. Because the behaviors and capabilities of the Clark video images are not consistent with the known abilities and/or behaviors of the cetacean species frequenting the area, it is proposed that the video images are not those of a known cetacean."
Posted on 8/27/26 at 11:01 am to hogcard1964
quote:
Coffee steaming bright"?
The coffee I'm drinking right now is steaming bright.
Posted on 8/27/26 at 11:03 am to Prosecuted Collins
quote:
How is this dude not banned yet?
Why should I be banned?
Posted on 8/27/26 at 12:49 pm to Dawglovertoo
quote:
Why should I be banned?
For trolling with your shitty serpent video and shitty AI songs would be my guess
I love that that blurry video is your definitive proof of sea serpents
Posted on 8/28/26 at 10:29 am to jchamil
Posting music on a music board isn't trolling.
My definitive proof sea serpents exist in reality is that on February 5, 1985 I saw a 60+ foot long sea serpent directly in front of me only 20 yards away in San Francisco Bay.
However, the slowed down and enlarged segment of my January 26, 2004 video shows the extremely long, black, uniform in width serpentine portions of the upper body of two sea serpents swimming against an incoming tide using vertical undulations in San Francisco Bay.
quote:
I love that that blurry video is your definitive proof of sea serpents
My definitive proof sea serpents exist in reality is that on February 5, 1985 I saw a 60+ foot long sea serpent directly in front of me only 20 yards away in San Francisco Bay.
However, the slowed down and enlarged segment of my January 26, 2004 video shows the extremely long, black, uniform in width serpentine portions of the upper body of two sea serpents swimming against an incoming tide using vertical undulations in San Francisco Bay.
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