Based on VLF observations in Northern Finland at Kannuslehto (KAN, L ~ 5.5), recently we revealed a new and previously unknown daytime type of VLF emissions at frequencies well above 4÷5 kHz. These emissions have neither been seen before because they were hidden by strong impulsive sferics originating in lightning. The peculiar VLF signals, discovered after filtering out the sferics, were studied. It is shown here that these emissions, which have a complicated spectral structure, occur during the winter around local noon under the quiet solar and geomagnetic conditions (Vsw < 400÷500 km/s, BIMF < 5÷7 nT, Np < 5÷8 cm -3 , AE < 150÷200 nT). These emissions are usually right-hand polarized and can last for several hours as a series of separate short discrete wideband (from 4 to 10 kHz and higher) signals, each with a duration between one and several minutes. We suppose that these waves are generated via the electron-cyclotron resonance mechanism deep inside the magnetosphere at much lower L-values than KAN. However, the details of the generation and propagation mechanisms of these newly discovered VLF emissions remain unclear.