SAVDAV FALL

There is an alluring water Fall at a village named Savadav in Kankavli Taluka. Being safe for swimming, it is crowded with tourists, especially during rainy season. You can directly let the water pour over your body. The road leading to the spot of the fall is full of curvings and ups and downs, with pleasant greenery all around. You can enjoy bathing and swimming at both sides of the fall. There is a small cave-type space at the stream-side, often used for keeping tiffin – material etc. you can reach this picanick spot by a tar-road Bombay-Goa-Highway (NH-17) either from Otav Fork or from Belane Fork. Distance from Otav – 9km, Distance from Belane- 6km. Nearest Railway Station-Nindgaon
Location: Savdav, Maharashtra 416602, India

Comments

Post a Comment

Popular posts from this blog

Image
Why Clouds Form On Mountain Tops? Air moves upward and downward in the atmosphere when blown over mountains and in response to thermals. It is easiest to explain what happens is if we examine things from the perspective of a small, imaginary, parcel of air. Think of holding the air in your hands and then letting go. Pressure decreases with elevation in the atmosphere. When a parcel of air rises it expands as the pressure lowers. If no external energy is added or removed (adiabatic expansion) the expansion causes the air parcel to cool. The rate of cooling for dry air is about 0.98°C per 100 meters of rise (5.4°F/1000 ft). The cooling rate is called the dry adiabatic lapse rate. If the air parcel is moved downward it warms at the same rate. The vapor pressure of water is temperature dependent. As the air cools it tends to become water saturated. Note that there are two effects here a) the air is expanding and thus diluting the water vapor and b) the air is cooling meanin...
Read more