The Must-see Attraction for Foreign Visitors- the Yehliu Geopark
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Pedestal rock area/ wave-cut platform- 2 main characteristics of the Geopark
In the first area, you will see lots of pedestal rocks, ginger shaped rocks and candle shaped rocks. When looking around, pedestal rocks are everywhere. With time passing by, the hard concretion inside the sandstone is exposed, and with the effect of wind, sun, rain, wave as well as the erosion of the northeast monsoon, the pedestal rocks of different shapes, such as the pedestal rocks with no necks, bulk necks, narrow necks and broken necks, are thus formed. The landscape with lots of pedestal rocks is very uneven, so pay attention while you are walking on it. Do not be too focused on taking photos or enjoying the view and fall.
The second area on the other side of the Geopark has the wave-cut landscape. You will find sea caves, coastal notches, wave-cut platform and cuesta. On one side of the wave-cut platform is the cliff and on the other side is the rapid wave. You will find lots of interesting rocks eroded by the seawater here, including the Twenty-four Filial Exemplars Rocks.
Landscape Wonder- The Pedestal Rocks
When first walking into the Geopark, you will see a huge area of the pedestal rocks. When seeing afar, it's like the cute mushrooms park. And the pedestal rocks are the landscape that attracts most people in the Yehliu Geopark. The process for the formulation of the pedestal rock is first the rock formation exposed from the sea surface, and the seawater will erode the rock continuously. After some time, the hard concretion inside the sandstone is exposed, and with the effect of wind, sun, rain, wave as well as the erosion of the northeast monsoon, the pedestal rocks of different shapes, such as the pedestal rocks with no necks, bulk necks, narrow necks and broken necks, are thus formed. The different shapes of the rocks represent the different formation processes. The landscape with lots of pedestal rocks is very uneven, so pay attention while you are walking on it. Do not be too focused on taking photos or enjoying the view and fall.
The Star of the Geopark - "Queen's Head"
The next coming up is the star of the Yehliu Geopark, "Queen's Head". The Queen's Head is a kind of pedestal rock. When the crustal structure was rising, the differential erosion of the seawater made the Queen's Head what it is like today. If we divide its height by the average crust rising speed in northern Taiwan, we will learn the Queen's Head is about 4,000 years old. The Queen's Head is a kind of pedestal rock. However, the joint on its upper concretion broke during 1962-1963. When viewing from a certain angle, it looks similar to the head portrait of Elizabeth II and thus acquires the name. With the natural weathering effect over the decades, the neck of the Queen's Head is getting even narrower. To prevent erosion by human activities for that tourists might touch it, the Queen's Head is now under protection. If you would like to take a photo with the Queen's Head, you can walk on the wooden plank trail to line up. Besides, you can view the Queen's Head from afar and take photos with it on the trail.
The "Cute Princess Rock" and "Candle Shaped Rock" are the popular landscape at the Geopark. The formation process of the "Cute Princess Rock" is similar to that of the Queen's Head. The eroded rock looks like a princess with a ponytail and is said to be the potential replacement of the Queen's Head. Doesn't the rock look like a little girl with her hair in a bun? Though the Cute Princess Rock is probably not as element and sophisticated as the Queen's Head, it gives people a feeling of passion and sweetness.
How was the "Candle Shaped Rock" named? I guess you already know! The landscape looks just like candles. There are 3 main processes for the formation of the Candle Shaped Rock. First the candle fire is exposed, and the area around it is eroded to form a groove. Finally, the candlestick is cut and the Candle Shaped Rock is thus formed. The candle fire is actually a round concretion in the rock formation. When seawater erodes sandstone, the round concretion which is harder is exposed on the ground. And when waves dash against the concretion, seawater flow around the concretion to erode the sandstone around it. A groove is formed as a result. Since the formation outside the concretion is harder, seawater will flow according to the shape of the formation and cut the rock into a cone shape that looks like a candlestick. And a rock that looks like the shape of candle is formed by mother nature.
Amazing Rocks- Cuesta
Now let's look at the beautiful scene of the Cuesta in the second area. Walking along on the road to the Cuesta, you will see the most beautiful sea and mountain scene in the Geopark. You can view the Cuesta on one side and the sea cliff as well as wave-cut platform on the other side.
The Cuesta features a sharp cliff on one side and a smooth slope on the other side. It is formed because the main stratum is pushed by uneven force and speed, which results in uneven rise of the stratum. When the stratum is pushed, the lump on the ground will cause the stratum to break. And after the seawater erosion, a landscape that looks like a "natural slide" is gradually formed.
Guess how famous is the Yehliu Geopark? CNN once reported that the scene at the "Yehliu Geopark" is like the landscape in the outer space and that it has the environment that looks just like the one Mars has. You will definitely find lots of gorgeous and special rocks, including the "Queen's Head", "Ice Cream Rocks", "Beehive Rocks", "Ginger Shaped Rocks" and other wave-cut landscape. You will definitely be amazed by the diverse geologic structure and landscapes here. What's more, you can see how great and powerful nature is. Whether it's from the perspective of geographic environment or location and transportation, the Geopark is definitely worth visiting!
Transportation Information of the Yehliu Geopark
*Tamsui Bus No.862 (Take the bus heading to Keelung in front of MRT Tamsui Station and get off at Yehliu.) The bus sets out every 30 minutes.
*KUO-KUANG eBus No. 1815 (Take the bus heading to Chinshan Youth Activity Center at the KUO-KUANG eBus Station at Taipei Main Station. The Bus drives along Zhongxiao E. Road and makes a brief stop at the Taipei City Hall Bus Station. Please get off at Yehliu.) The bus sets out every 20 minutes.
*Keelung Bus No.790 (Take the bus heading to Jinshan next to Keelung Train Station and get off at Yehliu.) The bus sets out every 15 minutes.
*Keelung Bus No.1068 (Take the bus heading to Jinshan at National Taiwan University and get off at Yehliu Geopark.)
*Keelung Bus No.953 (Take the bus heading to Jinshan at the bus station next to Banqiao Train Station and get off at Yehliu Geopark.)
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