33 file audio bebas royalti untuk "Sea Bubbles"

Waves and bubbles recorded on the shore. Recorded with zoom h1.

Waves and bubbles recorded on the shore. Recorded with zoom h1.

Calm waves crashing on a beach with the sound of fizzing bubbles as they break to an end. Recorded in walton-on-the-naze, essex, uk. Recorded with a zoom h6 msh-6 stereo mic on a calm spring morning.

Calm waves crashing on a beach with the sound of fizzing bubbles as they break to an end. Recorded in walton-on-the-naze, essex, uk. Recorded with a zoom h5 msh-6 stereo mic on a calm winter evening.

Busy calm waves crashing on a beach with a hint of fizzy bubbles. Recorded in walton-on-the-naze, essex, uk. Recorded with a zoom h5 msh-6 stereo mic on a calm winter evening.

Calm waves crashing on a beach with the sound of fizzing bubbles as they break to an end. Recorded in walton-on-the-naze, essex, uk. Recorded with a zoom h6 msh-6 stereo mic on a calm spring morning.

Bubbles in the sea. How it was created: is a sound extracted from a filming of a fishbowl of an aquarium, recorded by me. Recorder used: the camera of a cell phone samsung j5software used: any video converter to convert it to mp3, audacity to cut itdate: june 20, 2017location: buenos aires.

Field recording - recorded with a zoom h6 in stereo. Bubbling and filter tanks running in a small petting tank at an aquarium. (there's a shark in the petting tank. ).

This is an under water recording of some bubbles. I filled up a laundry bin with water, stuck a sennheisser md21 (dynamic omnimic) wrapped in a plastic bag in there (under the water level). I pumped bubbles from the bottom of the bin through a bicycle pump. Gear used: md21 -> m-audio dmp3 -> terratec ewx2496. Completely unprocessed, 2:43 of 24 bit 44khz wave. Submission for the earthfirewindwater contest.

Recorded with a 2 x micrtech gefell m296 omnis in ab on a dat. This is a 10 jear old recording;-)very gentle waves on the sand of the beach. You ca hear the bubbles of the salty foam bursting.

Water pouring out of fountain.

Ocean-like sub frequency information. Can be used as a layer for many purposes.

Sound effect recorded by kids using a straw and zoom h4 in nantes, transfert - le remorqueur.

Whilst being very uncreative and recording myself burp, i found some interesting sounds when changing the speed of the tracks.

Field recording of bergen harbour in norway. Can hear some distant boats with fog sirens and seagulls. Recorded using zoom h4n xy stereo setup. August 2012.

Bubbling sounds on exhale and regulator hiss during inhale. There is briefly a whizz sound from a rigid inflatable boat propeller passing nearby. Recorded with a contour+2 camera.

Go-pro recording of waves on the beach on a windy day, the microphone is very close to the water and after 45 seconds it gets under the waves for a cool submerged sound.

[cartoon, drowning 01. Wav]. Cartoon, drowning. If you enjoyed the sound, please star, comment, spread the word!🗣 it really helps! 🎯. Note: make sure to check out the other sounds! the sound quality is always better when you download the sound(s)! ⭐. More content otw!/matrixxx aka lil mati.

[cartoon, drowning 02. Wav]. Cartoon, drowning. If you enjoyed the sound, please star, comment, spread the word!🗣 it really helps! 🎯. Note: make sure to check out the other sounds! the sound quality is always better when you download the sound(s)! ⭐. More content otw!/matrixxx aka lil mati.

Stereo hydrophone recording of a small croatian harbor basin. Hydrophones submerged by approx. 1m, next to the bounding wall of the basin, facing the open sea. Lots of waves can be heard, in the onset, a small motorboat passes in the far range. Recorded with a pair of jrf series d hydrophones, spaced 18 cm apart with 0° dispersion.

Mud volcano field, davis-schrimpf seep field, salton sea, california. Lat: 33. 20070326716746lon: 244. 42179501054162. The davis-schrimpf onshore seep field site in the salton sea geothermal system is the result of shallow magmatic intrusions in a sedimentary basin. The ssgs is situated in the salton trough in southern california, an area with abundant surface manifestations of hydrothermal activity. The hydrothermal system in the salton trough occurs in a pull-apart setting where rifting and associated magmatic intrusions are responsible for the strong heat flow. One of the most concentrated and well-expressed onshore seep fields is the davis-schrimpf field, where more than 50 individual seeps are located in this area. Gas venting from gryphons and pools is vigorous with a continuous bubbling activity. Water and mud mixtures are continuously expelled down the flanks of the gryphons. Carbon dioxide produced from de-volatilization reactions involving sedimentary carbonate is the main driver for the seep activity. The morphological features of the davis- schrimpf seep field are strikingly similar to seep fields on dormant mud volcanoes however, the davis-schrimpf seeps are not related to mud volcanism, as mud volcanism normally implies large-scale mud breccia eruptions and a low temperature seep stage. From the; journal of geophysical research, vol. 114, b09201, doi:10. 1029/2008jb006247, 2009.

Individual gryphons, davis-schrimpf seep field, salton sea, california. Lat: 33. 20070326716746lon: 244. 42179501054162. The davis-schrimpf onshore seep field site in the salton sea geothermal system is the result of shallow magmatic intrusions in a sedimentary basin. The ssgs is situated in the salton trough in southern california, an area with abundant surface manifestations of hydrothermal activity. The hydrothermal system in the salton trough occurs in a pull-apart setting where rifting and associated magmatic intrusions are responsible for the strong heat flow. One of the most concentrated and well-expressed onshore seep fields is the davis-schrimpf field, where more than 50 individual seeps are located in this area. Gas venting from gryphons and pools is vigorous with a continuous bubbling activity. Water and mud mixtures are continuously expelled down the flanks of the gryphons. Carbon dioxide produced from de-volatilization reactions involving sedimentary carbonate is the main driver for the seep activity. The morphological features of the davis- schrimpf seep field are strikingly similar to seep fields on dormant mud volcanoes however, the davis-schrimpf seeps are not related to mud volcanism, as mud volcanism normally implies large-scale mud breccia eruptions and a low temperature seep stage. From the; journal of geophysical research, vol. 114, b09201, doi:10. 1029/2008jb006247, 2009.