Observations on large cosmic-ray bursts have been performed at the altitude of 3500 meters with a model C meter surrounded by thick lead shields. G-M counters, connected to appropriate electronic circuits, were placed over these lead shields in order to record extensive air showers simultaneously with bursts. It is found that about 2 percent of the 100 particle bursts and about 14 percent of the 1000 particle bursts under 10.7 cm Pb are produced by extensive air showers. This fraction continues to increase with increasing burst size and becomes almost 100 percent for bursts of more than 4000 particles. The experimental observations are consistent with the assumption that the part of the burst-producing radiation which does not consist of air showers or of ju-mesons is attenuated in lead with the absorption meanfree-path of 346db36 g/cm 2 . The correction for the number of bursts produced by /x-mesons is based on a revision of the calculations of Christy and Kusaka; the revised calculation indicates that /i-mesons (spin 1/2) produce 68db5 percent of the bursts in a model C meter under 10.7 cm Pb at sea level.It is pointed out that the high energy i\f-component of the cosmic radiation (i.e., those particles having strong nuclear interactions with matter) can produce enough electronic radiation to account for the observed burst frequency, if jQ l z 2 p(z)dz=0.12, where p(e/E)d(e/E) is the probability per nuclear collision that an iV-ray of high energy E produces electronic radiation of energy (e, de). The neutral meson mechanism satisfies this condition, provided one assumes that practically all of the energy of a high energy iV-ray is carried away by mesons when a nuclear collision in lead takes place, and that one-third of this energy goes into neutral mesons. The calculations are made on the assumption that the absorption mean-free-path of high energy N-rays is 124 g/cm 2 in air, and that the directional intensity of the primary cosmic radiation with energies greater than E Bev is 0.12(4.5/£) 2 sterad -1 cm -2 sec -1 at the top of the atmosphere.