{"id":62,"date":"2023-01-11T13:09:45","date_gmt":"2023-01-11T11:09:45","guid":{"rendered":"https:\/\/tic.visitpasvalys.lt\/?page_id=62"},"modified":"2023-01-24T15:30:09","modified_gmt":"2023-01-24T13:30:09","slug":"apie-pasvalio-krasta","status":"publish","type":"page","link":"https:\/\/tic.visitpasvalys.lt\/en\/apie-pasvalio-krasta\/","title":{"rendered":"Pasvalys &#8211; territory, residents"},"content":{"rendered":"\n<h4>Pasvalys<\/h4>\n\n\n\n<p>Pasvalis District is located in northern Lithuania. &nbsp;It is a typical district of the plains of the northern part of Lithuania (lowlands of \u017diemgala and M\u016b\u0161a-Nemun\u0117lis). The reason for the appearance of the plains characteristic of the region is a water basin that was formed as early as 350 million years ago &#8211; an ancient shallow lagoon, which, due to the accumulation of sediments, became more and more shallow. Layers of gypsum formed at the bottom, were covered by other sediments, and the water had to \u201cretreat\u201d.&nbsp;<\/p>\n\n\n\n<p>Karst phenomena characteristic to Pasvalys District are sinkholes, also known as \u201cliving eyes of nature\u201d. Snow and rainwater seep deep through the cracks and crevices and dissolve the gypsum layers that are laying there. A void appears in place of the dissolved gypsum. When it becomes so large that the remaining layer of earth on top can no longer support its weight, it begins to collapse, and a sinkhole is formed. Numerous karst collapses are scattered from Pasvalys towards Bir\u017eai.<\/p>\n\n\n\n<p>Later, the surface was levelled by advancing glaciers. Blocks of ice about 1 km thick would stop and \u201crest\u201d for 200-300 years, leaving hollows. Therefore, the lowest point of the District on the Latvian border near M\u016b\u0161a is just 16 meters above sea level.&nbsp;<\/p>\n\n\n\n<p>The highest point is in the west of the District in the Linkuva ridge separating the \u017diemgala and M\u016b\u0161a-Nemun\u0117lis lowlands: Velniakalnis rises to 75.2 meters near Kriau\u0161i\u0161kiai village. In addition to the ridge, the landscape is altered by the valleys of M\u016b\u0161a and its tributaries Ma\u017eup\u0117, Tatula, L\u0117vuo, Pyvesa, and Jie\u0161muo. There are no lakes in the area, only a few small ponds. Ice ages brought huge boulders, from which the stones of Petrai\u010diai (in Dauj\u0117nai Eldership) and Banioniai (in Pump\u0117nai Eldership) have survived to this day. The legacy of the ice ages is also layers of gravel, sand, clay soils, as it is romantically said &#8211; the land of oaks and wheat.<\/p>\n\n\n\n<p>It is one of the most urbanized and cultured districts in Lithuania with developed agriculture and forestry. Instead of grasslands and swamps rich with animal and plant species that once laid here, today we find drained plains converted into agricultural land.<\/p>\n\n\n\n<h4>Territory<\/h4>\n\n\n\n<p>Pasvalys District occupies 2 % of the Territory of Lithuania<br>The District is divided into 11 elderships: Dauj\u0117nai, Joni\u0161k\u0117lis Region, Joni\u0161k\u0117lis City, Krin\u010dinas, Nami\u0161iai, Pasvalys Region, Pasvalys city, Pump\u0117nai, Pu\u0161alotas, Salo\u010diai, Va\u0161kai.<\/p>\n\n\n\n<h4>Residents<\/h4>\n\n\n\n<p>According to the Statistics Department, 22,339 residents lived in the municipality of Pasvalys District as of 01 January 2021.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Pasvalys Pasvalis District is located in northern Lithuania. &nbsp;It is a typical district of the plains of the northern part of Lithuania (lowlands of \u017diemgala and M\u016b\u0161a-Nemun\u0117lis). The reason for the appearance of the plains characteristic of the region is a water basin that was formed as early as 350 million years ago &#8211; an ancient shallow lagoon, which, due to the accumulation of sediments, became more and more shallow. Layers of gypsum formed at the bottom, were covered by other sediments, and the water had to \u201cretreat\u201d.&nbsp; Karst phenomena characteristic to Pasvalys District are sinkholes, also known as \u201cliving&#8230;<\/p>\n","protected":false},"author":1,"featured_media":375,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":[],"translation":{"provider":"WPGlobus","version":"2.10.7","language":"en","enabled_languages":["lt","en"],"languages":{"lt":{"title":true,"content":true,"excerpt":false},"en":{"title":true,"content":true,"excerpt":false}}},"_links":{"self":[{"href":"https:\/\/tic.visitpasvalys.lt\/en\/wp-json\/wp\/v2\/pages\/62"}],"collection":[{"href":"https:\/\/tic.visitpasvalys.lt\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/tic.visitpasvalys.lt\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/tic.visitpasvalys.lt\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/tic.visitpasvalys.lt\/en\/wp-json\/wp\/v2\/comments?post=62"}],"version-history":[{"count":21,"href":"https:\/\/tic.visitpasvalys.lt\/en\/wp-json\/wp\/v2\/pages\/62\/revisions"}],"predecessor-version":[{"id":394,"href":"https:\/\/tic.visitpasvalys.lt\/en\/wp-json\/wp\/v2\/pages\/62\/revisions\/394"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/tic.visitpasvalys.lt\/en\/wp-json\/wp\/v2\/media\/375"}],"wp:attachment":[{"href":"https:\/\/tic.visitpasvalys.lt\/en\/wp-json\/wp\/v2\/media?parent=62"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}