alias “+jumpthrow” “+jump;-attack”; alias “-jumpthrow” “-jump”; bind “p” “+jumpthrow”

bind "f" "use weapon_flashbang";bind "c" "use weapon_hegrenade";bind "x" "use weapon_molotov";bind "g" "use weapon_smokegrenade";bind "q" "use weapon_decoy";bind "x" "use weapon_incgrenade";bind mwheelup +jump;bind mwheeldown +jump;bind space +jump;bind "t" "+lookatweapon"

-high-nod3d9ex1 -freq 144 -novid -nojoy -tickrate 128 +cl_forcepreload 1 +mat_queue_mode 2 -console -d3d9ex -HIGH -THREADS 4 +FPS_MAX 0 +CL_SHOWFPS 1 +CL_INTERP 0 +CL_INTERP_RATIO 1 +RATE 128000 +CL_UPDATERATE 128 +C

FAKU YOU SAK

+rep The method was developed by Willard Libby in the late 1940s and soon became a standard tool for archaeologists. Libby received the Nobel Prize for his work in 1960. The radiocarbon dating method is based on the fact that radiocarbon is constantly being created in the atmosphere by the interaction of cosmic rays with atmospheric nitrogen. The resulting radiocarbon combines with atmospheric oxygen to form radioactive carbon dioxide, which is incorporated into plants by photosynthesis; animals then acquire 14
C by eating the plants. When the animal or plant dies, it stops exchanging carbon with its environment, and from that point onwards the amount of 14
C it contains begins to decrease as the 14
C undergoes radioactive decay. Measuring the amount of 14
C in a sample from a dead plant or animal such as piece of wood or a fragment of bone provides information that can be used to calculate when the animal or plant died. The older a sample is,

The method was developed by Willard Libby in the late 1940s and soon became a standard tool for archaeologists. Libby received the Nobel Prize for his work in 1960. The radiocarbon dating method is based on the fact that radiocarbon is constantly being created in the atmosphere by the interaction of cosmic rays with atmospheric nitrogen. The resulting radiocarbon combines with atmospheric oxygen to form radioactive carbon dioxide, which is incorporated into plants by photosynthesis; animals then acquire 14
C by eating the plants. When the animal or plant dies, it stops exchanging carbon with its environment, and from that point onwards the amount of 14
C it contains begins to decrease as the 14
C undergoes radioactive decay. Measuring the amount of 14
C in a sample from a dead plant or animal such as piece of wood or a fragment of bone provides information that can be used to calculate when the animal or plant died. The older a sample is,