>>20682205 new potus new jersey
https://earthquake.usgs.gov/earthquakes/eventpage/us7000ma74/region-info
@ exactly 10:23 am est
1023
Apr 04, 2018 7:21:22 PM EDT
Q !xowAT4Z3VQ ID: 169658 No. 897229
Apr 04, 2018 7:19:05 PM EDT
Anonymous ID: b3f149 No. 897173
Apr 04, 2018 7:16:46 PM EDT
Q !xowAT4Z3VQ ID: 169658 No. 897116
We don’t say his name.
Adios.
The protected flow into AZ is no more.
Under the cover of his health, he will not be seeking another term.
Q
>>897116
Good shit.
Quick question: The Wall can't just be for stopping drugs, assassins, and child traffickers - which other nations were/are planning to use Mexico as an attack vector in the event of war?
Is there another Zimmerman Telegram we don't know about?
>>897173
Would you invade a country whereby a good portion of its citizens are armed?
The ‘ultimate deterrent’.
Q
https://earthquake.usgs.gov/earthquakes/eventpage/us7000ma74/map
Administrative Region
ISO
USA
Region
New Jersey
Country
United States
Nearby Places
Whitehouse Station, New Jersey, United States
7.7 km (4.8 mi) S
Population: 2089
Bridgewater, New Jersey, United States
12.7 km (7.9 mi) SE
Population: 44464
Bradley Gardens, New Jersey, United States
15.7 km (9.8 mi) SSE
Population: 14206
Somerville, New Jersey, United States
17.1 km (10.6 mi) SE
Population: 12202
Trenton, New Jersey, United States
51.8 km (32.2 mi) S
Population: 84225
Distance and direction from epicenter to nearby place.
Nearby place information was automatically generated from GeoNames. The list includes populated places, not necessarily cities. If this information is inaccurate, please consider updating the GeoNames database.
Tectonic Summary
Earthquakes in the New York - Philadelphia - Wilmington Urban Corridor
Since colonial times people in the New York - Philadelphia - Wilmington urban corridor have felt small earthquakes and suffered damage from infrequent larger ones. New York City was damaged in 1737 and 1884. Moderately damaging earthquakes strike somewhere in the urban corridor roughly twice a century, and smaller earthquakes are felt roughly every 2-3 years.
Earthquakes in the central and eastern U.S., although less frequent than in the western U.S., are typically felt over a much broader region. East of the Rockies, an earthquake can be felt over an area as much as ten times larger than a similar magnitude earthquake on the west coast. A magnitude 4.0 eastern U.S. earthquake typically can be felt at many places as far as 100 km (60 mi) from where it occurred, and it infrequently causes damage near its source. A magnitude 5.5 eastern U.S. earthquake usually can be felt as far as 500 km (300 mi) from where it occurred, and sometimes causes damage as far away as 40 km (25 mi).
Faults
Earthquakes everywhere occur on faults within bedrock, usually miles deep. Most bedrock beneath the urban corridor was assembled as continents collided to form a supercontinent about 500-300 million years ago, raising the Appalachian Mountains. Most of the rest of the bedrock formed when the supercontinent rifted apart about 200 million years ago to form what are now the northeastern U.S., the Atlantic Ocean, and Europe.
At well-studied plate boundaries like the San Andreas fault system in California, often scientists can determine the name of the specific fault that is responsible for an earthquake. In contrast, east of the Rocky Mountains this is rarely the case. New York City, Philadelphia, and Wilmington are far from the nearest plate boundaries, which are in the center of the Atlantic Ocean and in the Caribbean Sea. The urban corridor is laced with known faults but numerous smaller or deeply buried faults remain undetected. Even the known faults are poorly located at earthquake depths. Accordingly, few, if any, earthquakes in the urban corridor can be linked to named faults. It is difficult to determine if a known fault is still active and could slip and cause an earthquake. As in most other areas east of the Rockies, the best guide to earthquake hazards in the New York - Philadelphia - Wilmington urban corridor is the earthquakes themselves.