There is no flat answer(no pun intended) as there are different typ[es of seismographs. Obvisoulsy the big ones are non-portable and are mounted on fixed axes so they are virtually a part of the earth"s crust of bedrock. These instruments counting auxiliary ballast and such like would weigh several tons. as they are stationary, the weights are not generally quoted. Thee are portable seismometers used for mining and prospecting and these can be as light as perhaps ten or fifteen pounds. all things being equal the big boys are more accurate. in some Seismological stations they have three Seismographs, normally on all the time on different axes- for example: North-south, East_west, and vertical (Up and down) the last application would require a Gallitzin type of Seismogaph invented in Czarist Russia in about l906.This type is made in portable forms but has to be oriented to the precise vertical or horizontal axis before use-rather like a modern 35MM Camera. Sperry made seismographs. They are better known for Gyroscopes , but they did make Sesimographs,.ratrher seismometers, these were Three-axis types and could be used on Survey Ships -for oceanographic work. The three axes (R.P.I.) were selected by small rotary switches like those on some household lamps-twist on and off.
The average weight of a modern seismograph is typically around 100-200 pounds, depending on the size and model. The weight can vary based on the specific features and components included in the seismograph.
The plural form of "modern teacher" is "modern teachers."
Advantages of moving average method include simplicity, easy implementation, and ability to smooth out short-term fluctuations in data. Disadvantages include potential lag in forecasting, inability to capture sudden changes in data patterns, and reliance on historical data which may not always reflect future trends accurately.
Weight is a measure of the gravitational force acting on an object due to its mass. It is typically measured in units such as pounds or kilograms.
Film is a modern technology that involves capturing, storing, and projecting moving images. The alphabet, on the other hand, is pre-modern and dates back to early civilizations, enabling written communication and literacy. Both film and the alphabet have had significant impacts on society and communication.
20 pound copy paper refers to the weight of the paper, with 20 pounds indicating the weight of a ream (500 sheets). It is a standard weight for general everyday printing and copying tasks. The higher the weight, the thicker and more durable the paper will be.
John Miline invented the first modern seismograph in 1880
John Milne created the first modern seismograph.
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John Milne invented the seismograph in Tokyo, Japan in the late 19th century. He installed the first modern seismograph at the Imperial University of Tokyo in 1880.
Cro-Magnon were early modern humans. The weight would be the same as a modern female.
The average weight of an modern tank is about 60-65 tonnes.
The first seismograph was invented by Zhang Heng in 132. The modern seismograph was invented by John Milne, Thomas Gray, and James Alfred Ewing in 1880.
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The part of the seismograph that moves during an earthquake is called the pen.
In simple terms a seismograph works with a pen attached to a heavy weight hanging near the ground. As the ground shakes the line being drawn by the pen wiggles to reveal how strong the earthquake is.
A seismometer, sometimes known as a seismograph, in modern day is usually inertial an it has: 1) A weight of some kind, called the inertial mass, that moves inside but stays attached. 2) A recording device for the mass. Basically, the motion in the ground, even very slight, will move this weight and it is the movement of the weight which causes a reading on changes underground. Some modern systems now use electronics. Instead of a writing device for recording, it uses magnetic strips to record information. A seismograph records data from an earthquake with a needle and ink. When an earthquake occurs ts records this data and uses the needle with ink on it to show the highs and lows of the P waves, S waves, and surface waves the earthquake produces. The ink lines are recorded on graph paper showing the number of how high or low the earthquake's strength is and measures the waves.