Environment
Like the rest of the Sierra Gorda region, Pinal de Amoles is marked by very rugged terrain, which includes canyons and steep mountains. The area is located in an area with extremely high peaks with small flat areas and mesas. The altitude varies between 839masl at the community of Huajales to 3350masl at the Cerro de la Calentura, which is also the highest point in the state. Eighty eight percent of the municipality’s territory belongs to the Sierra Gorda Biosphere Reserve of Querétaro, a region which is protected because of its extreme diversity of landscapes, climates, vegetation and wildlife. Pinal de Amoles represents the highest peaks of this region, which essentially separate the wetter lands to the north and east from the semi arid areas of the south and west as the mountains block moisture coming in from the Gulf of Mexico. Most of the rock is sedimentary, with about 45% limestone. About 15% is intrusive volcanic rock. This due to the fact that much of the Sierra Gorda was sea bed millions of years ago, with volcanic activity later in its geological history. The volcanic rock accounts for most of the municipality’s minable deposits.
Rivers are fast flowing due to the geography. The two most important rivers are the Extoraz in the south flowing east and El Rodezno or Río Escanela, which flows past Escanela, Escanelila and Ahuacatlán, emptying into the Jalpan Dam. There are also 169 bodies of surface water which include 143 fresh water springs, six small dams and 20 streams.
In the entire region, the coldest temperatures occur between December and January, with high temperatures in April and May. Temperatures vary widely depending on altitude with an annual average of 13C in the higher elevations such as Pinal de Amoles to 24C in lower areas such as Jalpan. In the highest elevations, frosts and freezes are not uncommon.
The north of the municipality is dominated by deciduous rainforest, which loses much of its leaves in the dry season. The center and northwest are dominated by pine and oak forests. Pine and holm oak forests are found mostly above 2,000 masl. The forests of the municipality are its most important natural resource. The types of wildlife is very varied and includes white-tailed deer, pumas, tigrillos (Leopardus tigrinus or Leopardus wiedii), bobcats, coyotes, raccoons, opossums, armadillos, foxes, skunks, hares and rabbits. Birds are especially varied and include woodpeckers, American goldfinches, sparrows, parrots, macaws and ravens. Reptiles include rattlesnakes and coral snakes as well as “river shrimp” or acamaya. A group of researchers from the Natural Sciences Faculty of the Universidad Autónoma de Querétaro have discovered a new species of crustacean similar to a very large shrimp or small lobster in the municipality. The crustacean is found in fresh water mostly in the Platanos Arroyo and can grow to a size of up to eight centimeters. Locally, the creature is called an “acocil” or freshwater lobster, like other creatures found in other parts of Mexico. However, studies have shown that this crustacean show enough peculiarities to warrant it as a separate species. The formal name for it is Procambarus Yacoy.
There three main types of climate. The first is temperate and humid, with rains in the summer and an average annual temperature of between 12 and 18C. There is little rain in the winter but the annual average is about 850mm. This climate prevails at altitudes over 2,000 masl. There is a semi hot and dry climate in areas with average annual temperatures between 18 and 22C with rains in the summer and little rain in winter. Average annual precipitation is about 500mm. Areas with a semi hot and humid climates have similar rainfall patters but with an average rainfall of just under 1000mm. Summers here are hot and humid. Like in the rest of the Sierra Gorda, the coldest temperatures occur between December and January, with high temperatures in April and May. In the highest elevations, many of which are in Pinal de Amoles, frosts, freezes and even snow are not uncommon. Recent significant freezes, frosts and snows have occurred in 2007 and 2010 with very high altitude communities such as San Gaspar most affected. The ice and snow make driving dangerous on Highway 120, as it has an abundance of curves. This can form “black ice” which is an invisible layer of ice over the earth, which can lower air temperatures further. The government works to help poorer communities deal with the cold conditions year with advisories. In 2010, the Sierra Gorda had it first significant snowfall in eighteen years in the municipality, with temperatures of -4C. In some places, the cover was 15 cm deep.
Most of the municipality is covered in forest of one type or another, and these forests are its main natural resource. These forests have been having problems in recent years between insect and parasitic plant infestations and logging. The infestations have been more severe than usual because of drought conditions weakening trees. While there are strict environmental laws for the area as part of the biosphere reserve, enforcement is spotty. The forests of this and neighboring municipalities have attracting illegal logging from those outside the area. Pinal de Amoles is one of the Sierra Gorda municipalities where this problem is the most serious.
In 2005, a road was built between El Llano de Huaxquilico to San Pedro Escanela, but it is controversial because of environmental concerns. Its building caused severe ecological damage in an area considered to be one of the most sensitive in the Sierra Gorda Biosphere Reserve, as it is where most of the local aquifers recharge. The area receives a large amount of rain, which has led to damage and mudslides affecting the road, making it almost impossible for more than one car to pass at a time.
In 2011, small earthquakes of about 3.5 on the Richter scale shook this municipality and neighboring Jalpan. The Centro de Geociencias de la Universidad Nacional Autónoma de México states that the quakes are due to microfractures under the Sierra Gorda and do not indicate the coming of a major earthquake.
The rugged terrain of the area gives rise to a number of waterfalls, forests, canyons, springs and other natural attractions. El Chuveje is one of the largest waterfalls in the state, measuring about thirty meters high and with a strong steady fall of water surrounded by mountains and vegetation. Activities include hiking, camping and bird watching with macaws and white tailed deer still to be seen although there are fewer than in the past. The waterfall is located a couple of kilometers from the park entrance and can only be reached by foot. The El Salto waterfall is located in San Pedro Escanela, with a height of 35 meters. The water falls into a clear pond at the foot of the elevation then forms a small river. It is not easy to reach and recommended only for experienced hikers. The Puente de Dios (Bridge of God) is a natural bridge located on the side of a small mountain near the Peña de la Gloria. The site of the bridge is a deep crevasse with thick vegetation and under the bridge a river with two small waterfalls flows. The La Angostura Canyon is about fifty meters long and contains part of the Escanela River, the same that passes through the Puente de Dios and then empties into the Ayutla River. The canyon contains several places where the water pools and are suitable for swimming in the summer. The Infiernillo Arroyo is found within a kilometer long canyon. In the lower part, there are various pools of blue water along with small waterfalls. Around these is thick vegetation.
The Barranca Arroyo is a small canyon structure about an hour and a half from the municipal seat. The water flows year round with several areas where it pools, but the water is cold. The area is surrounded by large mountains with abundant vegetation. There is camping, hiking and picnicking. The Peña de la Viuda is a natural monolith which falls directly into an arroyo. The area has abundant vegetation, and activities such as skiing, camping and hiking. La Escondida is an area in mountainous forest with a permanent fresh water spring. It permits camping and hiking. El Cidral is an area with cedar trees surrounding a clearing for camping and hiking. The Peña de la Glora waterfall is surrounded by thick vegetation. The lowest part has a natural spring and the upper part has a deep, unexplored cave. The Cueva de los Riscos (Cave of the Crags) is named after the crags which appear in various of its chambers. The entrance begins with a rocky descent then levels out to an area with sand. The center has a hillock with looks like a monolith rock. This can be climbed to observe the various crags with contain ice. One of these in the shape of a pulpit and another is called the “bell tower” because if it is struck it sounds like a bell.
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