This pain reminds me of what memory I have not yet faced and unearths the memories I have displaced, rejecting linear timelines and welcoming another tremor. Fearless vulnerability is integral to making because of the inherent physical, emotional, and psychic discomfort and pain of the process. These emotions are found in spray foam squeezing through a window or by pressing my thumb on a clay slab until my fingerprint wears away. I articulate the unavoidable and unspeakable by stacking associations of memories until consciousness unfolds into fully formed emotions conveyed by a memory. My work manifests through series of experimental and performative material investigations indexing fingers and tongues – movements and language. Seismic waves are waves that travel through the Earth or other elastic body2 to 8 kilometersThe primary factor is the composition of the rock that the wave travels through. Catching something that is abruptly no longer in motion often finds objects in precarious or acrobatic positions that push the bounds of fragility – on the verge of falling and breaking but captured in the moment before. Focusing on these traces offers space for one to inspect and contemplate this primary event at a distance, freezing memories caught in the tremor. My work inspects these objects, like stains on a mattress, as remnants or traces of what has happened. It can be compared to the seismic wave of an earthquake in its pulsations, which are a reminder of its magnitude as are the objects left in its wake. It is felt physically, emotionally, and mentally throughout a lifetime alone, in a family, and in a community. A tremor is a reverberation of an initial event. The primary or P wave (Figure 2a) is the fastest (5. Body waves can be characterized as either primary or sec-ondary. Featured work Husk, 2018-2020 Reverberate, 2021 Seismic Waves There are two basic types of seismic waves: body waves which travel through the body of the earth and sur-face waveswhich travel around the surface of the earth. The rate of change of seismic waves with depth in Earth (as shown in Figure 9.6) has been determined over the past several decades by analyzing seismic signals from large earthquakes at seismic stations around the world. Visit Emily Irvin’s website and Instagram page. Their writing of poetry and feminist theories has also been published in Italy, Iran, and the US. basic principles of unsteady flows long wave theory Saint-Venant. Emily Irvin’s work has been exhibited internationally in Italy, Mexico, and USA. Design of a small building for wind and seismic loading including torsional effects. In 2021, they received an MFA from the University of Colorado, Boulder. They received a BS in 2015 and a BFA in 2016 from the Ohio State University. This study develops an approach for estimating seismic performance of complex critical urban infrastructures. Seismic migration is a process of estimating earth’s reflectivity from a recorded seismic wavefield using a velocity-depth model. Emily Irvin asks ceramic questions, observing their body in relation to the tangible world.
0 Comments
Leave a Reply. |