Autonomous Meridian Sensory Response: from Internet subculture to audiovisual therapy

ASMR (Autonomous Sensory Meridian Response) is the name given to a pleasant sensation that can be felt most commonly on the scalp and can be triggered by various gentle sounds (like whispers, crinkles or tapping), smooth and repetitive visual stimuli, personal attention (like the touch of a hairdresser or a masseur) or other events. ASMR is often associated with a general feeling of relaxation and peace. Whilst academic research on the sociological, artistic, sensory and cognitive dimensions is still in its infancy ASMR has grown into a worldwide, cross-disciplinary, inter-cultural, multi-lingual social media sensation. This paper outlines the rise of ASMR as Internet subculture from its inception as ‘whispering community’ on Internet platforms and blogs, to become a truly popular (i.e. made by the people) platform for creative expression, self-made holistic therapy and in some instances true artistic audiovisual endeavours. This paper comments on the reasons behind the rise of the ASMR community as a fertile ground for creative expression. Audiences’ expectations are dictated by the attention-induced nature of the sensory experience, a factor that spawned an exceptionally perceptive viewership if one considers the inherently fragmented essence of ubiquitous streaming media and the impatient scanning and skipping modes of reception it encourages. ‘ASMRtists’ thus enjoy a privileged relationship with audiences who are not impressed with the relentless pour of energy and information from social media platforms and treasure, instead, the slow, the quiet and the subtle. Examples from various ASMR content creators will be analysed from the compositional standpoint, highlighting technical and idiomatic similarities with forms of improvisatory practices and experimental artistic languages such as Musique Concrète. The paper will also illustrate recent audiovisual projects related to ASMR carried out at Keele University and will introduce the audience to planned developments towards ASMR related content delivered through mobile platforms

Accretion, structure and hydrology of intermediate spreading-rate oceanic crust from drillhole experiments and seafloor observations

Downhole measurements recorded in the context of the Ocean Drilling Program in Hole 504B, the deepest hole drilled yet into the oceanic crust, are analyzed in terms of accretion processes of the upper oceanic crust at intermediate spreading-rate. The upper part of the crust is found to support the non steady-state models of crustal accretion developed from seafloor observations (Kappel and Ryan, 1986; Gente, 1987). The continuous and vertical nature of borehole measurements provides stratigraphic and structural data that cannot be obtained solely from seafloor studies and, in turn, these models define a framework to analyze the structural, hydrological, and mineralogical observations made in the hole over the past decade.Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/43190/1/11001_2005_Article_BF01204282.pd

Drilling deep into young oceanic crust, Hole 504B, Costa Rica Rift

Hole 504B is by far the deepest hole yet drilled into the oceanic crust in situ, and it therefore provides the most complete “ground truth” now available to test our models of the structure and evolution of the upper oceanic crust. Cored in the eastern equatorial Pacific Ocean in 5.9-m.y.-old crust that formed at the Costa Rica Rift, hole 504B now extends to a total depth of 1562.3 m below seafloor, penetrating 274.5 m of sediments and 1287.8 m of basalts. The site was located where the rapidly accumulating sediments impede active hydrothermal circulation in the crust. As a result, the conductive heat flow approaches the value of about 200 mW/m² predicted by plate tectonic theory, and the in situ temperature at the total depth of the hole is about 165°C. The igneous section was continuously cored, but recovery was poor, averaging about 20%. The recovered core indicates that this section includes about 575 m of extrusive lavas, underlain by about 200 m of transition into over 500 m of intrusive sheeted dikes; the latter have been sampled in situ only in hole 504B. The igneous section is composed predominantly of magnesium-rich olivine tholeiites with marked depletions in incompatible trace elements. Nearly all of the basalts have been altered to some degree, but the geochemistry of the freshest basalts is remarkably uniform throughout the hole. Successive stages of on-axis and off-axis alteration have produced three depth zones characterized by different assemblages of secondary minerals: (1) the upper 310 m of extrusives, characterized by oxidative “seafloor weathering“; (2) the lower extrusive section, characterized by smectite and pyrite; and (3) the combined transition zone and sheeted dikes, characterized by greenschist-facies minerals. A comprehensive suite of logs and downhole measurements generally indicate that the basalt section can be divided on the basis of lithology, alteration, and porosity into three zones that are analogous to layers 2A, 2B, and 2C described by marine seismologists on the basis of characteristic seismic velocities. Many of the logs and experiments suggest the presence of a 100- to 200-m-thick layer 2A comprising the uppermost, rubbly pillow lavas, which is the only significantly permeable interval in the entire cored section. Layer 2B apparently corresponds to the lower section of extrusive lavas, in which original porosity is partially sealed as a result of alteration. Nearly all of the logs and experiments showed significant changes in in situ physical properties at about 900–1000 m below seafloor, within the transition between extrusives and sheeted dikes, indicating that this lithostratigraphic transition corresponds closely to that between seismic layers 2B and 2C and confirming that layer 2C consists of intrusive sheeted dikes. A vertical seismic profile conducted during leg 111 indicates that the next major transition deeper than the hole now extends—that between the sheeted dikes of seismic layer 2C and the gabbros of seismic layer 3, which has never been sampled in situ—may be within reach of the next drilling expedition to hole 504B. Therefore despite recent drilling problems deep in the hole, current plans now include revisiting hole 504B for further drilling and experiments when the Ocean Drilling Program returns to the eastern Pacific in 1991